Nothing Special   »   [go: up one dir, main page]

You seem to have javascript disabled. Please note that many of the page functionalities won't work as expected without javascript enabled.
 
 
Sign in to use this feature.

Years

Between: -

Subjects

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Journals

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Article Types

Countries / Regions

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Search Results (297)

Search Parameters:
Keywords = anthropogenic heat

Order results
Result details
Results per page
Select all
Export citation of selected articles as:
26 pages, 5323 KiB  
Article
An Urban Climate Paradox of Anthropogenic Heat Flux and Urban Cool Island in a Semi-Arid Urban Environment
by Asfa Siddiqui, Ambadas B. Maske, Ansar Khan, Ananya Kar, Manushi Bhatt, Vinamra Bharadwaj, Yogesh Kant and Rafiq Hamdi
Atmosphere 2025, 16(2), 151; https://doi.org/10.3390/atmos16020151 - 29 Jan 2025
Viewed by 520
Abstract
The rapid urbanization of Jaipur has profoundly altered its urban climate, driven by anthropogenic heat flux (AF) and shifts in surface energy dynamics. This study leverages remote sensing techniques, utilizing Landsat data, to quantify AF and assess its influence [...] Read more.
The rapid urbanization of Jaipur has profoundly altered its urban climate, driven by anthropogenic heat flux (AF) and shifts in surface energy dynamics. This study leverages remote sensing techniques, utilizing Landsat data, to quantify AF and assess its influence on the city’s climate. The findings reveal a striking paradox; despite a significant rise in AF from 127.31 W/m2 in 1993 to 201.82 W/m2 in 2020, Jaipur exhibits an anomalous urban cool island (UCI) effect during the daytime. In this phenomenon, surrounding fallow lands experience higher land surface temperatures (LSTs) than the urban core, defying the typical urban heat island (UHI) effect observed in most cities worldwide. This paradox is especially pronounced in semi-arid urban environments, where factors such as limited vegetation, arid conditions, and water scarcity intricately shape peculiar thermal behaviour. This study further highlights the role of urban expansion, with built-up areas growing from 11.95% in 1993 to 19% in 2020, intensifying AF. Notably, the latent heat flux was highest in vegetated areas, significantly reducing LSTs by facilitating evapotranspiration. Daytime surface temperatures have surged significantly, with temperatures ranging from 26–46.9 °C in 1993 to 31–56.5 °C in 2020, indicating an overall increase in surface heat intensity. Despite these increases, the UCI effect remains observable, further illustrating the cooling potential of urban vegetation. This study offers novel insights into the intricate dynamics of urban heat in semi-arid cities, providing refined perspectives on urban heat mitigation strategies and climate adaptation, with implications for future sustainable urban planning and environmental management. Full article
(This article belongs to the Section Biometeorology and Bioclimatology)
Show Figures

Graphical abstract

Graphical abstract
Full article ">Figure 1
<p>Land Use and Land Cover (LULC) changes in Jaipur (1993 and 2020). The LULC maps illustrating changes in key land cover categories over 27 years, including forest and bare field, built-up areas, agricultural land, fallow land, barren land, and water bodies. The maps highlight the expansion of built-up areas, reduction in forest cover, and shifts in agricultural and barren land, providing insights into the dynamic transformation of Jaipur city.</p>
Full article ">Figure 2
<p>Land Surface Temperature (LST) of Jaipur (1993 and 2020). The LST maps displaying spatial variations in LST (°C) over time, highlighting changes between 1993 and 2020. Cooler areas are shown in blue, while hotter areas are depicted in red, providing insights into the thermal dynamics and urbanization impacts on Jaipur city.</p>
Full article ">Figure 3
<p>Surface Urban Heat Island Intensity (SUHII) in Jaipur for 1993 and 2020. Maps illustrating the spatial distribution and magnitude of SUHII (°C) during 1993 and 2020. Positive SUHII values, indicating urban areas warmer than their rural surroundings, are shown in red, while negative SUHII values, representing the Urban Cool Island (UCI) effect, are depicted in blue. The maps highlight temporal changes in urban thermal patterns, driven by land use transformations and urbanization processes.</p>
Full article ">Figure 4
<p>Anthropogenic Heat Flux (<math display="inline"><semantics> <mrow> <msub> <mrow> <mi>A</mi> </mrow> <mrow> <mi>F</mi> </mrow> </msub> </mrow> </semantics></math>) for Jaipur in 1993 and 2020. Maps illustrating the spatial patterns of <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>A</mi> </mrow> <mrow> <mi>F</mi> </mrow> </msub> </mrow> </semantics></math> (W/m<sup>2</sup>) across Jaipur, reflecting heat emissions from human activities such as transportation, industrial processes, and energy consumption. The maps reveal significant changes in <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>A</mi> </mrow> <mrow> <mi>F</mi> </mrow> </msub> </mrow> </semantics></math> intensity over time, driven by urban expansion and increased energy.</p>
Full article ">
18 pages, 6356 KiB  
Article
Modelling Backward Trajectories of Air Masses for Identifying Sources of Particulate Matter Originating from Coal Combustion in a Combined Heat and Power Plant
by Maciej Ciepiela, Wiktoria Sobczyk and Eugeniusz Jacek Sobczyk
Energies 2025, 18(3), 493; https://doi.org/10.3390/en18030493 - 22 Jan 2025
Viewed by 494
Abstract
The paper analyzes the processes of emission and dispersion of particulate contaminants from a large point source emitter: a hard coal-fired power plant. Reference is made to the European Green Deal and its main objective of reducing anthropogenic particulate and greenhouse gas emissions. [...] Read more.
The paper analyzes the processes of emission and dispersion of particulate contaminants from a large point source emitter: a hard coal-fired power plant. Reference is made to the European Green Deal and its main objective of reducing anthropogenic particulate and greenhouse gas emissions. CHPP, Krakow Combined Heat and Power Plant, Poland, as described in the article, has a strong impact on the mechanisms that shape the microclimatic factors of the Krakow agglomeration. This combined heat and power plant provides heat and electricity for the city, while simultaneously emitting significant amounts of suspended particulate matter into the atmosphere. Due to the adverse impact of non-conventional energy sources on the natural environment and the increasing effects of climate warming, radical changes need to be implemented. The HYSPLIT (Hybrid Single-Particles Lagrangian Integrated Trajectories) model was used to track the movement of contaminated air masses. A 5-day episode of increased hourly concentrations of PM2.5 particulate matter contamination was selected to analyze the backward trajectories of air mass displacement. From 15 August 2022 to 19 August 2022, high 24-h particulate matter concentrations were recorded, measuring around 20 µg/m3. The HYSPLIT model, a unique tool in the precise identification of point sources of pollution and their impact on the air quality of the region, was used to analyze the influx of polluted air masses. A 5-day episode of increased hourly concentrations of PM2.5 pollutants was selected for the study, with values of approximately 20 µg/m3. It was found that low-pressure systems over the North Atlantic brought wet and variable weather conditions, while high-pressure systems in southern and eastern Europe, including Poland, provided stable and dry weather conditions. The simulation results were verified by analyzing synoptic maps of the study area. The image of the displacement of contaminated air masses obtained from the HYSPLIT model was found to be consistent with the synoptic maps, confirming the accuracy of the applied model. This means that the HYSPLIT model can be used to create maps of contaminant dispersion directions. Consequently, it was confirmed that modeling using the HYSPLIT model is an effective method for predicting the displacement directions of particulate contamination originating from coal combustion in a combined heat and power plant. Identifying circulation patterns and front zones during episodes of increased contaminant concentrations is strategic for effective weather monitoring, air quality management, and alerting the public to episodes of increased health risk in a large agglomeration. Full article
(This article belongs to the Collection Feature Papers in Energy, Environment and Well-Being)
Show Figures

Figure 1

Figure 1
<p>Structure of energy carriers in Poland in 2021 and 2023 [<a href="#B15-energies-18-00493" class="html-bibr">15</a>].</p>
Full article ">Figure 2
<p>Krakow Metropolitan Area (dark blue) in the context of the Malopolskie Voivodeship (blue) [<a href="#B36-energies-18-00493" class="html-bibr">36</a>].</p>
Full article ">Figure 3
<p>City physiognomy contrast—Nowa Huta meadows in Krakow (photo M. Ciepiela).</p>
Full article ">Figure 4
<p>CHPP, Krakow Combined Heat and Power Plant, Poland (photo M. Ciepiela).</p>
Full article ">Figure 5
<p>HYSPLIT model for reverse trajectories at the measurement point of the CHPP, Krakow Combined Heat, and Power Plant, Poland, in 2022 for: (<b>a</b>) 15 August, (<b>b</b>) 16 August, (<b>c</b>) 17 August, (<b>d</b>) 18 August, (<b>e</b>) 19 August [<a href="#B48-energies-18-00493" class="html-bibr">48</a>].</p>
Full article ">Figure 5 Cont.
<p>HYSPLIT model for reverse trajectories at the measurement point of the CHPP, Krakow Combined Heat, and Power Plant, Poland, in 2022 for: (<b>a</b>) 15 August, (<b>b</b>) 16 August, (<b>c</b>) 17 August, (<b>d</b>) 18 August, (<b>e</b>) 19 August [<a href="#B48-energies-18-00493" class="html-bibr">48</a>].</p>
Full article ">Figure 6
<p>Synoptic maps for 12:00 UTC: (<b>a</b>) 15 August 2022; (<b>b</b>) 16 August 2022; (<b>c</b>) 17 August 2022; (<b>d</b>) 18 August 2022; (<b>e</b>) 19 August 2022 [<a href="#B53-energies-18-00493" class="html-bibr">53</a>].</p>
Full article ">Figure 6 Cont.
<p>Synoptic maps for 12:00 UTC: (<b>a</b>) 15 August 2022; (<b>b</b>) 16 August 2022; (<b>c</b>) 17 August 2022; (<b>d</b>) 18 August 2022; (<b>e</b>) 19 August 2022 [<a href="#B53-energies-18-00493" class="html-bibr">53</a>].</p>
Full article ">Figure 6 Cont.
<p>Synoptic maps for 12:00 UTC: (<b>a</b>) 15 August 2022; (<b>b</b>) 16 August 2022; (<b>c</b>) 17 August 2022; (<b>d</b>) 18 August 2022; (<b>e</b>) 19 August 2022 [<a href="#B53-energies-18-00493" class="html-bibr">53</a>].</p>
Full article ">
25 pages, 14621 KiB  
Article
Thermal Environmental Impact of Urban Development Scenarios from a Low Carbon Perspective: A Case Study of Wuhan
by Kai Lin, Qingming Zhan, Wei Xue, Yulong Shu and Yixiao Lu
Buildings 2025, 15(2), 208; https://doi.org/10.3390/buildings15020208 - 12 Jan 2025
Viewed by 761
Abstract
Amidst the increasingly escalating global concern regarding climate change, adopting a low-carbon approach has become crucial for charting the future developmental trajectory of urban areas. It also offers a novel angle for cities to avoid high-temperature risks. This paper estimates carbon emissions in [...] Read more.
Amidst the increasingly escalating global concern regarding climate change, adopting a low-carbon approach has become crucial for charting the future developmental trajectory of urban areas. It also offers a novel angle for cities to avoid high-temperature risks. This paper estimates carbon emissions in Wuhan City from both direct and indirect aspects. Then, the ANN (artificial neural network)–CA (Cellular Automata) model is employed to establish three distinct development scenarios (Ecological Priority, Tight Growth, and Natural Growth) to predict future urban expansion. Additionally, the WRF (Weather Research and Forecasting Model)—UCM (Urban Canopy Model) model is used to investigate the thermal environmental impacts of varying urban development scenarios. This study uses a low-carbon perspective to explore how cities can develop scientifically sound urban strategies to meet climate change challenges and achieve sustainable development goals. The conclusions are as follows: (1) The net carbon emission for Wuhan in 2022 is estimated to be approximately 20.8353 million tonnes. Should the city maintain an average annual emission reduction rate of 10%, the carbon sink capacity of Wuhan would need to be enhanced by 382,200 tonnes by 2060. (2) In the absence of anthropogenic influence, there is a propensity for the urban construction zone of Wuhan to expand primarily towards the southeast and western sectors. (3) The Ecological Priority (EP) and Tight Growth (TG) scenarios are effective in alleviating the urban thermal environment, achieving a reduction of 0.88% and 2.48%, respectively, in the urban heat island index during afternoon hours. In contrast, the Natural Growth (NG) scenario results in a degradation of the urban thermal environment, with a significant increase of over 4% in the urban heat island index during the morning and evening periods. (4) An overabundance of urban green spaces and water bodies could exacerbate the urban heat island effect during the early morning and at night. The findings of this study enhance the comprehension of the climatic implications associated with various urban development paradigms and are instrumental in delineating future trajectories for low-carbon sustainable urban development models. Full article
(This article belongs to the Special Issue New Challenges in Digital City Planning)
Show Figures

Figure 1

Figure 1
<p>Location of Wuhan City and distribution of urban thermal environment. Areas within the urban built-up area where the temperature difference is greater than 2 °C compared to the suburbs are considered heat island areas. Areas with a temperature difference of less than 2 °C are considered cold island areas.</p>
Full article ">Figure 2
<p>Research framework and technical route of this study.</p>
Full article ">Figure 3
<p>Spatial constraint factors used for scenario prediction.</p>
Full article ">Figure 4
<p>The range and location relationship of the three domains. Urban blue-green spaces are areas within cities that include water bodies and vegetation. Domain refers to the specific geographical area and the grid system defined for numerical weather prediction simulations.</p>
Full article ">Figure 5
<p>Comparison of daily temperature change and WRF-UCM simulation in Wuhan Meteorological Station (Jiangxia, Caidian and Huangpi). This figure verifies the error between simulation results and observation results by presenting the trend of temperature changes.</p>
Full article ">Figure 6
<p>Measurement and prediction results of carbon emission in Wuhan. (<b>a</b>) Correlation analysis of carbon emissions in land use type. (<b>b</b>) Carbon emission measurement results in historical years. (<b>c</b>) Forecast results of carbon emission in future years.</p>
Full article ">Figure 7
<p>Comparison of land use distribution and scale in 2015 and future scenarios. (<b>a</b>) Land use distribution in various development scenarios; (<b>b</b>) the quantitative structure of land use in various development scenarios.</p>
Full article ">Figure 8
<p>Temperature curve and temperature difference curve. (<b>a</b>) Air temperature, (<b>b</b>) air temperature difference, (<b>c</b>) surface temperature, (<b>d</b>) surface temperature difference.</p>
Full article ">Figure 9
<p>Temperature difference field and wind difference field at 6:00.</p>
Full article ">Figure 10
<p>Temperature difference field and wind difference field at 16:00.</p>
Full article ">Figure 11
<p>Urban heat island intensity in the simulated region. This figure is obtained by processing the surface temperature data output by WRF-UCM through the NCAR Command Language (NCL). It shows the heat island intensity of various urban scenarios at four different times throughout the day: early morning, morning, afternoon, and night.</p>
Full article ">Figure 12
<p>The energy curves and difference curves of SWDOWN, HFX, LH, and GRDFLX.</p>
Full article ">
22 pages, 6364 KiB  
Review
Review on the Application of Remote Sensing Data and Machine Learning to the Estimation of Anthropogenic Heat Emissions
by Lingyun Feng, Danyang Ma, Min Xie and Mengzhu Xi
Remote Sens. 2025, 17(2), 200; https://doi.org/10.3390/rs17020200 - 8 Jan 2025
Cited by 1 | Viewed by 712
Abstract
Anthropogenic heat is the heat generated by human activities such as industry, construction, transport, and metabolism. Accurate estimates of anthropogenic heat are essential for studying the impacts of human activities on the climate and atmospheric environment. Commonly applied methods for estimating anthropogenic heat [...] Read more.
Anthropogenic heat is the heat generated by human activities such as industry, construction, transport, and metabolism. Accurate estimates of anthropogenic heat are essential for studying the impacts of human activities on the climate and atmospheric environment. Commonly applied methods for estimating anthropogenic heat include the inventory method, the energy balance equation method, and the building model simulation method. In recent years, the rapid development of computer technology and the availability of massive data have made machine learning a powerful tool for estimating anthropogenic heat fluxes and assessing its effects. Multi-source remote sensing data have also been widely used to obtain more details of the spatial and temporal distribution characteristics of anthropogenic heat. This paper reviews the main approaches for estimating anthropogenic heat emissions. The typical algorithms of the abovementioned three methods are introduced, and their advantages and limitations are also evaluated. Moreover, the recent progress in the application of remote sensing data and machine learning are discussed as well. Based on big data and machine learning techniques, the research on feature engineering and model fusion will bring about major changes in data analysis and modeling of anthropogenic heat. More in-depth research of this issue is recommended to provide important support for curbing global warming, mitigating air pollution, and achieving the national goals of carbon peak and a carbon neutrality strategy. Full article
Show Figures

Figure 1

Figure 1
<p>Time series graph of keywords and top articles of anthropogenic heat articles [<a href="#B4-remotesensing-17-00200" class="html-bibr">4</a>,<a href="#B6-remotesensing-17-00200" class="html-bibr">6</a>,<a href="#B9-remotesensing-17-00200" class="html-bibr">9</a>,<a href="#B10-remotesensing-17-00200" class="html-bibr">10</a>].</p>
Full article ">Figure 2
<p>Number of AH articles in the last decade (2010–2023).</p>
Full article ">Figure 3
<p>Flow chart of PRISMA for systematic review.</p>
Full article ">Figure 4
<p>Different methods and scales of AH estimation articles, 2010–2023. NCP refers to the North China Plain region. YRD refers to the Yangtze River Delta region. PRD refers to the Pearl River Delta region.</p>
Full article ">Figure 5
<p>The application of satellite remote sensing data in the inventory method.</p>
Full article ">Figure 6
<p>The process of building machine learning models.</p>
Full article ">Figure 7
<p>Flowchart of the article including regression factors and machine learning methods (Ao et al., 2024 [<a href="#B30-remotesensing-17-00200" class="html-bibr">30</a>]).</p>
Full article ">Figure 8
<p>Flowchart of the article, including regression factors and machine learning methods (Qian et al., 2024 [<a href="#B66-remotesensing-17-00200" class="html-bibr">66</a>]).</p>
Full article ">Figure 9
<p>Importance of the features for (<b>a</b>) building heat, (<b>b</b>) industrial heat, and (<b>c</b>) transportation heat (Qian et al., 2024 [<a href="#B66-remotesensing-17-00200" class="html-bibr">66</a>]).</p>
Full article ">
19 pages, 26867 KiB  
Article
Lipid Biomarkers in Urban Soils of the Alluvial Area near Sava River, Belgrade, Serbia
by Gordana Dević, Sandra Bulatović, Jelena Avdalović, Nenad Marić, Jelena Milić, Mila Ilić and Tatjana Šolević Knudsen
Molecules 2025, 30(1), 154; https://doi.org/10.3390/molecules30010154 - 3 Jan 2025
Viewed by 617
Abstract
This study focused on the investigation of soil samples from the alluvial zone of the Sava River, located near the heating plant in New Belgrade, Serbia. Using gas chromatography with flame ionization detection (GC-FID), a broad range of alkanes, including linear n-alkanes [...] Read more.
This study focused on the investigation of soil samples from the alluvial zone of the Sava River, located near the heating plant in New Belgrade, Serbia. Using gas chromatography with flame ionization detection (GC-FID), a broad range of alkanes, including linear n-alkanes (C10 to C33) and isoprenoids, was analyzed in all samples. The obtained datasets were effectively made simpler by applying multivariate statistical analysis. Various geochemical indices (CPI, ACL, AI, TAR, etc.) and ratios (S/L, Paq, Pwax, etc.) were calculated and used to distinguish between biogenic and anthropogenic contributions. This approach added a higher level of precision to the source identification of hydrocarbons and provided a detailed geochemical characterization of the investigated soil. The results showed that the topsoil had a high content of TPH (average value, 90.65 mg kg−1), potentially related to an accidental oil spill that occurred repeatedly over extended periods. The uncommon n-alkane profiles reported for the investigated soil samples are probably the result of inputs related to anthropogenic sources, emphasizing that petroleum was the main source of the short-chain n-alkanes. The methodology developed in this study was proven to be efficient for the assessment of the environmental quality of the soil in an urban part of New Belgrade, but it can also be a useful tool for soil monitoring and for a pollution assessment in other (sub)urban areas. Full article
(This article belongs to the Special Issue Environmental Analysis of Organic Pollutants, 2nd Edition)
Show Figures

Figure 1

Figure 1
<p>Investigated area—the heating plant in New Belgrade, Serbia, and the positions of sampling microlocations.</p>
Full article ">Figure 2
<p>GC-FID chromatograms of <span class="html-italic">n</span>-alkanes in some soil samples from the alluvial area of New Belgrade.</p>
Full article ">Figure 3
<p>Box and whisker plot showing the variation of geochemical indices in the investigated soil samples.</p>
Full article ">Figure 4
<p>Ternary diagram showing relative abundance of the carbon preference indices: short-chain alkane homologs, CPI1, mid-chain <span class="html-italic">n</span>-alkanes, CPI2, and all <span class="html-italic">n</span>-alkanes homologs (CPI3) of investigated soil samples.</p>
Full article ">Figure 5
<p>Relationship between the Average Chain Length and the Carbon Preference Index CPI2 in the urban soil samples.</p>
Full article ">Figure 6
<p>Cross-plots of the terrigenous/aquatic ratio, versus proxy ratios: submerged/floating aquatic macrophyte (Paq) (<b>a</b>) and terrestrial plants Pwax (<b>b</b>).</p>
Full article ">Figure 7
<p>The dendrogram was obtained by applying the Q-mode hierarchical cluster analysis on the evaluation indices calculated on the basis of the distribution of <span class="html-italic">n</span>-alkanes in OM of the urban soils analyzed in this study.</p>
Full article ">
26 pages, 8176 KiB  
Article
Evaluating Urban Heat Island Effects in the Southwestern Plateau of China: A Comparative Analysis of Nine Estimation Methods
by Ziyang Ma, Huyan Fu, Jianghai Wen and Zhiru Chen
Land 2025, 14(1), 37; https://doi.org/10.3390/land14010037 - 28 Dec 2024
Viewed by 674
Abstract
Surface urban heat island intensity (SUHII) is a critical indicator of the urban heat island (UHI) effect. However, discrepancies in estimation methods may introduce uncertainty in SUHII values. While previous studies have examined the responses of SUHII to different methods at large scales, [...] Read more.
Surface urban heat island intensity (SUHII) is a critical indicator of the urban heat island (UHI) effect. However, discrepancies in estimation methods may introduce uncertainty in SUHII values. While previous studies have examined the responses of SUHII to different methods at large scales, further analysis is needed for plateau cities in southwestern China, which have complex geographical features. This study investigates the spatiotemporal patterns and influencing factors of SUHII in 200 plateau cities across southwestern China via nine estimation methods that incorporate rural ranges and elevation-based conditions. The results show that: (1) The annual average daytime and nighttime SUHII for these cities were 0.97 ± 0.78 °C (mean ± std) and 0.21 ± 0.87 °C, respectively. For 22% of the cities during the day and 26% at night, the choice of different SUHII estimation methods resulted in the transformation between a surface urban heat island (SUHI) and a surface urban cold island (SUCI) due to the exclusion of rural pixels more than ±50 m from the median urban elevation. Compared with other regions, high-altitude plateau cities exhibited a slightly lower daytime SUHII but a significantly higher nighttime SUHII because of the lower atmospheric pressure in plateau areas, which limits the conduction and retention of heat. Consequently, heat dissipates more quickly at night, increasing SUHII values. (2) The mean ΔSUHIIAD (absolute difference in SUHII values across methods) was 0.51 ± 0.01 °C during the day and 0.44 ± 0.02 °C at night. (3) In high-altitude plateau cities, for all methods, the correlation of the SUHII with influencing factors was stronger, highlighting their sensitivity to both environmental and anthropogenic influences. These results enhance our understanding of plateau UHI dynamics and highlight the importance of considering appropriate rural definitions for cities with varying geographical characteristics. Full article
Show Figures

Figure 1

Figure 1
<p>Study area.</p>
Full article ">Figure 2
<p>Spatial distribution of rural ranges in Kunming; (<b>a</b>–<b>c</b>) correspond to rural ranges 1 (R1), 2 (R1), and 3 (R1).</p>
Full article ">Figure 3
<p>Spatial distribution of average daytime SUHII for cities in Southwest China over the last twenty years. M1–M9 correspond to the methods described in <a href="#land-14-00037-t002" class="html-table">Table 2</a>, with the black numbers below each subplot indicating the proportion of cities with SUHI.</p>
Full article ">Figure 4
<p>Spatial distribution of average nighttime SUHII for cities in Southwest China over the last twenty years. M1–M9 correspond to the methods described in <a href="#land-14-00037-t002" class="html-table">Table 2</a>, with the black numbers below each subplot indicating the proportion of cities with SUHI.</p>
Full article ">Figure 5
<p>Box plots of the average daytime (<b>a</b>) and nighttime (<b>b</b>) SUHII for cities in Southwest China over twenty years. M1–M9 correspond to the methods described in <a href="#land-14-00037-t002" class="html-table">Table 2</a>, with the black numbers indicating the average SUHII values and standard deviations (mean ± std) for the nine estimation methods. The midline of the box indicates the median, while the colored points and error bars dictate the mean values and 95% confidence intervals, respectively.</p>
Full article ">Figure 6
<p>Seasonal variations in the average daytime (<b>a</b>) and nighttime (<b>b</b>) SUHII for cities in Southwest China over the last twenty years. M1–M9 correspond to the methods described in <a href="#land-14-00037-t002" class="html-table">Table 2</a>, with the colored points indicating the mean values and the error bars indicating the 95% confidence intervals. The black dashed line indicates the average SUHII values.</p>
Full article ">Figure 7
<p>Spatial distribution of the average daytime and nighttime LST in cities of the Tibet Autonomous Region over the last twenty years, where a, b, c, and d represent the regions of Seni District in Naqu, Duilongdeqing District, Chengguan District in Lhasa, and Sangzhuzi District in Shigatse, respectively.</p>
Full article ">Figure 8
<p>Box plots of annual average daytime (<b>a</b>) and nighttime (<b>b</b>) SUHIIs for cities in Southwest China across different terrains. The box represents the interquartile range, with the line inside indicating the median. The colored points and error bars represent the mean and the 95% confidence interval, respectively.</p>
Full article ">Figure 9
<p>Seasonal variations in the annual average daytime (<b>a</b>) and nighttime (<b>b</b>) SUHIIs for cities in Southwest China across different terrains. The colored points and error bars represent the mean values and 95% confidence intervals, respectively.</p>
Full article ">Figure 10
<p>Pearson correlation coefficients (r) between annual average daytime and nighttime SUHIIs and influencing factors. Population (log(P)); urban area (UA); enhanced vegetation index (EVI); white sky albedo (WSA); monthly average temperature (MAT); monthly total precipitation (MTP); Δ represents the difference in influencing factors between urban and rural areas; A represents the difference in influencing factors between summer and winter. Asterisks (*) denote statistical significance at the 0.05 level, while double asterisks (**) denote statistical significance at the 0.01 level.</p>
Full article ">Figure 11
<p>Pearson correlation coefficients (r) between annual average daytime SUHIIs and influencing factors for cities in Southwest China across different terrains. (<b>a</b>–<b>d</b>) represent basin cities, hilly and mountainous cities, low-elevation plateau cities, and high-elevation plateau cities, respectively. Population (log(P)); urban area (UA); enhanced vegetation index (EVI); white sky albedo (WSA); monthly average temperature (MAT); monthly total precipitation (MTP); Δ represents the difference between urban and rural areas; A represents the difference between summer and winter. An asterisk (*) indicates statistical significance at the 0.05 level, and two asterisks (**) indicate statistical significance at the 0.01 level.</p>
Full article ">Figure 12
<p>Pearson correlation coefficients (r) between annual average nighttime SUHIIs and influencing factors for cities in Southwest China across different terrains. (<b>a</b>–<b>d</b>) represent basin cities, hilly and mountainous cities, low-elevation plateau cities, and high-elevation plateau cities, respectively. Population (log(P)); urban area (UA); enhanced vegetation index (EVI); white sky albedo (WSA); monthly average temperature (MAT); monthly total precipitation (MTP); Δ represents the difference between urban and rural areas; A represents the difference between summer and winter. An asterisk (*) indicates statistical significance at the 0.05 level, and two asterisks (**) indicate statistical significance at the 0.01 level.</p>
Full article ">Figure 13
<p>Correlations between daytime SUHII values for the nine estimation methods. M1–M9 refer to the methods outlined in <a href="#land-14-00037-t002" class="html-table">Table 2</a>, with the horizontal and vertical axes representing the daytime SUHII (°C) for each estimation method. The red points indicate the daytime SUHII for each city, and the green line represents the trend line. The value of r denotes the correlation, and all results are statistically significant at the 0.01 level.</p>
Full article ">Figure 14
<p>Correlation between nighttime SUHII values for the nine estimation methods. M1–M9 refer to the methods outlined in <a href="#land-14-00037-t002" class="html-table">Table 2</a>, with the horizontal and vertical axes representing the nighttime SUHII (°C) for each estimation method. The blue points indicate the nighttime SUHII for each city, and the green line represents the trend line. The value of r denotes the correlation, and all results are statistically significant at the 0.01 level.</p>
Full article ">Figure 15
<p>Overlay frequency distribution of the average daytime (<b>a</b>) and nighttime (<b>b</b>) ΔSUHII<sub>AD</sub> for cities in Southwest China over twenty years. ΔSUHII<sub>AD</sub> represents the absolute difference in SUHII between different estimation methods. The horizontal axis denotes the ΔSUHII<sub>AD</sub> between different methods (e.g., M1–M2 represents the ΔSUHII<sub>AD</sub> between method 1 and method 2, as shown in <a href="#land-14-00037-t002" class="html-table">Table 2</a>), and the vertical axis represents the proportion of each ΔSUHII<sub>AD</sub> interval.</p>
Full article ">Figure 16
<p>Box plot of the average daytime (<b>a</b>) and nighttime (<b>b</b>) ΔSUHII<sub>AD</sub> for cities in Southwest China over twenty years. ΔSUHII<sub>AD</sub> represents the absolute difference in SUHII between different estimation methods. The horizontal axis denotes the differences between various methods (e.g., M1–M2 represents the ΔSUHII<sub>AD</sub> between methods 1 and 2 as described in <a href="#land-14-00037-t002" class="html-table">Table 2</a>). The black dashed line, along with the accompanying numbers, represents the mean and standard deviation (mean ± std) of the ΔSUHII<sub>AD</sub> for all method pairs. The line inside the box indicates the median, while the colored points represent the average values.</p>
Full article ">Figure 17
<p>Relationship between the average rural LST and the number of pixels for cities in Southwest China over twenty years. Panels (<b>a</b>–<b>c</b>) correspond to R1, 2, and 3, respectively.</p>
Full article ">
15 pages, 2168 KiB  
Article
Urban Management for Building-Sector Decarbonization: Focusing on the Role of Low-Carbon Policies
by Jianxin Tang, Pengpeng Yang, Kai Tang and Sibo Wang
Buildings 2024, 14(12), 3924; https://doi.org/10.3390/buildings14123924 - 9 Dec 2024
Viewed by 724
Abstract
The building sector is a major source of anthropogenic carbon emissions worldwide. While existing studies have extensively explored the socioeconomic and technological impacts on carbon emissions generated from building operations, few have assessed the effectiveness of low-carbon policies in curbing the increasing trend [...] Read more.
The building sector is a major source of anthropogenic carbon emissions worldwide. While existing studies have extensively explored the socioeconomic and technological impacts on carbon emissions generated from building operations, few have assessed the effectiveness of low-carbon policies in curbing the increasing trend of building sector carbon emissions. This study examines the impacts of low-carbon policy intensity on building sector carbon emissions using a two-way fixed effects model on a 6-year panel (2015–2020) dataset for 286 cities in China. Our findings indicate that, on average, the aggregated intensity of low-carbon policies fails to pose any significant impacts on carbon emissions from building operations. This is partly due to the variations in different types of policy. Specifically, a 10% increase in the intensity of energy conservation policy results in a 0.05% decrease in carbon emissions, whereas capacity utilization policies are associated with an increase in building-operation carbon emissions. Moreover, these policy–emission relationships vary across building types and end-use sources. In particular, energy conservation policies are negatively associated with emissions from cooking and heating, but positively related to emissions generated from appliances and cooling. In comparison, capacity utilization policies tend to encourage additional emissions from most sources. This study highlights the partial effectiveness of energy conservation policies in curbing building sector carbon emissions and underscores the need for additional efforts in tackling the rebound effects to realize building sector decarbonization. Full article
(This article belongs to the Special Issue Energy Efficiency and Carbon Neutrality in Buildings)
Show Figures

Figure 1

Figure 1
<p>Spatial distribution of sample cities, building sector carbon emissions, and policy intensity for low-carbon policies. (<b>a</b>) Spatial distribution of sample cities; (<b>b</b>) building sector carbon emissions of sample cities; and (<b>c</b>) policy intensity for low-carbon policies of sample cities.</p>
Full article ">Figure 2
<p>City- and province-specific estimates of policy intensity impacts on building sector carbon emissions. (<b>a</b>) City-specific estimates of the PIA impact on TCE; (<b>b</b>) province-specific estimates of the PIA impact on TCE; and (<b>c</b>) number of cities with positive, negative, and not significant coefficients within each province.</p>
Full article ">Figure 3
<p>Summary of results. * 10% statistical significance; ** 5% statistical significance; *** 1% statistical significance; PICR: intensity for carbon reduction policies; PIEC: intensity for energy conservation policies; PICE: intensity for capacity utilization policies; PITEC: intensity for technology policies; TCE: total carbon emissions from building operation; PCCE: carbon emissions from public and commercial building operations; URCE: carbon emissions from urban residential building operation; RRCE: carbon emissions from rural residential building operation; ACE: carbon emissions from appliances; LCE: carbon emissions from lighting; CCE: carbon emissions from cooling; CWCE: carbon emissions from cooking and water heating; DHCE: carbon emissions from distributed heating; CHCE: carbon emissions from central heating.</p>
Full article ">
25 pages, 4754 KiB  
Article
Borehole Optical Fibre Distributed Temperature Sensing vs. Manual Temperature Logging for Geothermal Condition Assessment: Results of the OptiSGE Project
by Maciej R. Kłonowski, Anders Nermoen, Peter J. Thomas, Urszula Wyrwalska, Weronika Pratkowiecka, Agnieszka Ładocha, Kirsti Midttømme, Paweł Brytan, Anna Krzonkalla, Adrianna Maćko, Karol Zawistowski and Jolanta Duczmańska-Kłonowska
Sensors 2024, 24(23), 7419; https://doi.org/10.3390/s24237419 - 21 Nov 2024
Viewed by 841
Abstract
Geothermal energy is a crucial component contributing to the development of local thermal energy systems as a carbon-neutral and reliable energy source. Insights into its availability derive from knowledge of geology, hydrogeology and the thermal regime of the subsurface. This expertise helps to [...] Read more.
Geothermal energy is a crucial component contributing to the development of local thermal energy systems as a carbon-neutral and reliable energy source. Insights into its availability derive from knowledge of geology, hydrogeology and the thermal regime of the subsurface. This expertise helps to locate and monitor geothermal installations as well as observe diverse aspects of natural and man-made thermal effects. Temperature measurements were performed in hydrogeological boreholes in south-western Poland using two methods, i.e., manual temperature logging and optical fibre distributed temperature sensing (OF DTS). It was assumed the water column in each borehole was under thermodynamic equilibrium with the local geothermal gradient of the subsurface, meaning rocks and aquifers. Most of the acquired results show typical patterns, with the upper part of the log depending on altitude, weather and climate as well as on seasonal temperature changes. For deeper parts, the temperature normally increases depending on the local geothermal gradient. The temperature logs for some boreholes located in urban agglomerations showed anthropogenic influence caused by the presence of infrastructure, the urban heat island effect, post-mining activities, etc. The presented research methods are suitable for applications connected with studies crucial to selecting the locations of geothermal installations and to optimize their technical parameters. The observations also help to identify zones of intensified groundwater flow, groundwater inrush into wells, fractured and fissured zones and many others. Full article
(This article belongs to the Section Environmental Sensing)
Show Figures

Figure 1

Figure 1
<p>Contour maps of Europe (<b>A</b>) and Poland (<b>B</b>). Localization of the studied boreholes on the contour map (<b>C</b>) and simplified geological map (<b>D</b>) [<a href="#B25-sensors-24-07419" class="html-bibr">25</a>] of south-western Poland. Numbering of the studied boreholes according to <a href="#sensors-24-07419-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 2
<p>Field setup of temperature logging with manual recorders.</p>
Full article ">Figure 3
<p>Field setup of OF DTS.</p>
Full article ">Figure 4
<p>Connection scheme of the devices used for OF DTS measurements.</p>
Full article ">Figure 5
<p>Calculation of correction factors for two PT100s used for calibrating DTS data. The PT100s were submerged in an ice bath while logging the temperature. Curves were fitted to the resulting time series in order to give a correction factor based on the steady-state temperature.</p>
Full article ">Figure 6
<p>DTS data obtained from channel 4 (Ch. 4) for borehole no. 15 Wambierzyce 18N in the anti-Stokes and Stokes regime are shown by colorful lines. The data covered a time period of about 40 min, explaining the variability in the observed ambient air temperature. The data before and after ~410 m corresponds to Raman backscatter produced by laser pulses traveling downwards and upwards along the cable, respectively.</p>
Full article ">Figure 7
<p>Box plots showing statistical parameters for temperature measurements by manual logging and OF DTS for the individual boreholes.</p>
Full article ">Figure 8
<p>Depth-dependent temperature curves in the selected geological boreholes for manual logging and OF DTS measurements showing strong anthropogenic impact. Since the geothermal signal is overrun, these boreholes were excluded from the assessment of vertical heat flow.</p>
Full article ">Figure 9
<p>Depth-dependent temperature values with calculation intervals and thermal conductivity values of the rock types for the selected boreholes. Values of thermal conductivities were set up according to Earth Energy Designer application [<a href="#B42-sensors-24-07419" class="html-bibr">42</a>]. Values of weighted thermal conductivities for each calculation interval are shown in <a href="#sensors-24-07419-t006" class="html-table">Table 6</a>.</p>
Full article ">
19 pages, 3162 KiB  
Article
Challenges and Performance of Filter Dusts as a Supplementary Cementitious Material
by Johannes Berger, Anabella Mocciaro, Gisela Cordoba, Cecilia Martinefsky, Edgardo F. Irassar, Nancy Beuntner, Sebastian Scherb, Karl-Christian Thienel and Alejandra Tironi
Materials 2024, 17(22), 5676; https://doi.org/10.3390/ma17225676 - 20 Nov 2024
Viewed by 697
Abstract
Global industry relies on a linear approach for economic growth. One step towards transformation is the implementation of a circular economy and the reclamation of anthropogenic deposits. This study examines two filter dusts, one German and one Argentinian, from the production of calcined [...] Read more.
Global industry relies on a linear approach for economic growth. One step towards transformation is the implementation of a circular economy and the reclamation of anthropogenic deposits. This study examines two filter dusts, one German and one Argentinian, from the production of calcined clays, representing such deposits. Investigations and comparisons of untreated and calcined filter dust and the industrial base product pave the way for using waste product filter dust as supplementary cementitious material (SCM). In the future, some twenty thousand tons of contemporary waste could potentially be used annually as SCM. The results confirm the suitability of one material as a full-fledged SCM without further treatment and a measured pozzolanic reactivity on par with fly ash. Sample materials were classified into two groups: one was found to be a reactive pozzolanic material; the other was characterized as filler material with minor pozzolanic reactivity. Additionally, important insights into the physical properties of oven dust and heat-treated oven dust were obtained. For both material groups, an inversely proportional relationship with rising calcination temperatures was found for the specific surface area and water demand. The impact of the calcination temperature on both the particle size distribution and the potential to optimize the reactivity performance is presented. Full article
(This article belongs to the Special Issue Advances in Natural Building and Construction Materials)
Show Figures

Figure 1

Figure 1
<p>XRD assessment of swellable clay minerals in D-CIC through glycol vapor treatment. D-CIC—AD represents the air-dried and D-CIC—Glycol the glycol vapor-treated D-CIC sample.</p>
Full article ">Figure 2
<p>XRD segment of the XRD quantification showing the different phyllosilicates present in the D-CIC.</p>
Full article ">Figure 3
<p>TG and DTG curves of the two dusts D-CCC and D-CIC with marked calcination temperatures.</p>
Full article ">Figure 4
<p>FTIR spectra, comparing German filter dust before and after treatment.</p>
Full article ">Figure 5
<p>FTIR spectra, comparing Argentinian filter dust before and after treatment.</p>
Full article ">Figure 6
<p>Visualization of the inverse proportional relationship between the BET surface area and the water demand determined with the Puntke method with qualitatively increasing temperatures for both of the investigated sample groups.</p>
Full article ">Figure 7
<p>R<sup>3</sup> test for evolved heat; German samples with reference curves and inert threshold band according to [<a href="#B9-materials-17-05676" class="html-bibr">9</a>].</p>
Full article ">Figure 8
<p>R<sup>3</sup> test for evolved heat; Argentinian samples with reference curves and inert threshold band according to [<a href="#B9-materials-17-05676" class="html-bibr">9</a>].</p>
Full article ">
20 pages, 10246 KiB  
Article
Investigation into the Mechanism of the Impact of Sunlight Exposure Area of Urban Artificial Structures and Human Activities on Land Surface Temperature Based on Point of Interest Data
by Yuchen Wang, Yu Zhang and Nan Ding
Land 2024, 13(11), 1879; https://doi.org/10.3390/land13111879 - 10 Nov 2024
Viewed by 948
Abstract
With rapid urbanization, the urban heat island (UHI) effect has intensified, posing challenges to human health and ecosystems. This study explores the impact of sunlight exposure areas of artificial structures and human activities on land surface temperature (LST) in Hefei and Xuzhou, using [...] Read more.
With rapid urbanization, the urban heat island (UHI) effect has intensified, posing challenges to human health and ecosystems. This study explores the impact of sunlight exposure areas of artificial structures and human activities on land surface temperature (LST) in Hefei and Xuzhou, using Landsat 9 data, Google imagery, nighttime light data, and Point of Interest (POI) data. Building shadow distributions and urban road surface areas were derived, and geospatial analysis methods were applied to assess their impact on LST. The results indicate that the sunlight exposure areas of roofs and roads are the primary factors affecting LST, with a more pronounced effect in Xuzhou, while anthropogenic heat plays a more prominent role in Hefei. The influence of sunlight exposure on building facades is relatively weak, and population density shows a limited impact on LST. The geographical detector model reveals that interactions between roof and road sunlight exposure and anthropogenic heat are key drivers of LST increases. Based on these findings, urban planning should focus on optimizing building layouts and heights, enhancing greening on roofs and roads, and reducing the sunlight exposure areas of artificial structures. Additionally, strategically utilizing building shadows and minimizing anthropogenic heat emissions can help lower local temperatures and improve the urban thermal environment. Full article
(This article belongs to the Special Issue Geospatial Data in Land Suitability Assessment: 2nd Edition)
Show Figures

Figure 1

Figure 1
<p>Geographical location and land cover of the study areas: (<b>a</b>) location of Anhui and Jiangsu in China; (<b>b</b>) location and land cover of Hefei’s built-up area; and (<b>c</b>) location and land cover of Xuzhou’s built-up area.</p>
Full article ">Figure 2
<p>POI data for (<b>a</b>,<b>d</b>) buildings, roads, and (<b>b</b>,<b>e</b>) real-time population distribution, along with (<b>c</b>,<b>f</b>) NTL imagery for Hefei and Xuzhou.</p>
Full article ">Figure 3
<p>(<b>a</b>) The relationship between the spatial distribution of building shadows and solar illumination; (<b>b</b>) solar azimuth and solar elevation angle.</p>
Full article ">Figure 4
<p>Methodology flow for extracting sunlight exposure area of artificial structures.</p>
Full article ">Figure 5
<p>(<b>a</b>) Building roof sunlight exposure area extraction; (<b>b</b>) sunlit building facade sunlight exposure area extraction; (<b>c</b>) road sunlight exposure area extraction.</p>
Full article ">Figure 6
<p>LST inversion results of (<b>a</b>) Hefei and (<b>b</b>) Xuzhou with 300 × 300 m grids.</p>
Full article ">Figure 7
<p>Spatial distribution map of all influencing factors on 300 × 300 m grids in Hefei and Xuzhou.</p>
Full article ">Figure 8
<p>The matrix scatter plot between LST and each impact factor: (<b>a</b>) Hefei and (<b>b</b>) Xuzhou.</p>
Full article ">Figure 9
<p>Moran’s I and LISA results for the spatial correlation between LST and influencing factors in Hefei and Xuzhou.</p>
Full article ">Figure 10
<p>Interaction detection results for LST and influencing factors: (<b>a</b>) Hefei, (<b>b</b>) Xuzhou.</p>
Full article ">
28 pages, 14767 KiB  
Article
Trends in CO, CO2, CH4, BC, and NOx during the First 2020 COVID-19 Lockdown: Source Insights from the WMO/GAW Station of Lamezia Terme (Calabria, Southern Italy)
by Francesco D’Amico, Ivano Ammoscato, Daniel Gullì, Elenio Avolio, Teresa Lo Feudo, Mariafrancesca De Pino, Paolo Cristofanelli, Luana Malacaria, Domenico Parise, Salvatore Sinopoli, Giorgia De Benedetto and Claudia Roberta Calidonna
Sustainability 2024, 16(18), 8229; https://doi.org/10.3390/su16188229 - 21 Sep 2024
Cited by 4 | Viewed by 1215
Abstract
In 2020, the COVID-19 outbreak led many countries across the globe to introduce lockdowns (LDs) that effectively caused most anthropic activities to either stop completely or be significantly reduced. In Europe, Italy played a pioneeristic role via the early introduction of a strict [...] Read more.
In 2020, the COVID-19 outbreak led many countries across the globe to introduce lockdowns (LDs) that effectively caused most anthropic activities to either stop completely or be significantly reduced. In Europe, Italy played a pioneeristic role via the early introduction of a strict nationwide LD on March 9th. This study was aimed at evaluating, using both chemical and meteorological data, the environmental response to that occurrence as observed by the Lamezia Terme (LMT) GAW/WMO station in Calabria, Southern Italy. The first 2020 lockdown was therefore used as a “proving ground” to assess CO, CO2, CH4, BC, and NOx concentrations in a rather unique context by exploiting the location of LMT in the context of the Mediterranean Basin. In fact, its location on the Tyrrhenian coast of Calabria and local wind circulation both lead to daily cycles where western-seaside winds depleted in anthropogenic pollutants can be easily differentiated from northeastern-continental winds, enriched in anthropogenic outputs. In addition to this, the first Italian LD occurred during the seasonal transition from winter to spring and, consequently, summer, thus providing new insights on emission outputs correlated with seasons. The findings clearly indicated BC and, in particular, CO as strongly correlated with average daily temperatures, as well as possibly domestic heating. CO2’s reduction during the lockdown and consequent increase in the post-lockdown period, combined with wind data, allowed us to constrain the local source of emissions located northeast from LMT. NOx reductions during specific circumstances were consistent with hypotheses from previous research, which linked them to rush hour traffic and other forms of transportation emissions. CH4’s stable patterns were consistent with livestock, landfills, and other sources assumed to be nearly constant during LD periods. Full article
(This article belongs to the Special Issue Sustainable Climate Action for Global Health)
Show Figures

Figure 1

Figure 1
<p>(<b>A</b>): MapChart of Italy highlighting the region of Calabria. (<b>B</b>): Location of LMT in Calabria itself. (<b>C</b>) Details of the Lamezia Terme area with a highlight on notable emission sources in the area. The “Highway” mark refers to a point where the distance between the A2 highway and LMT is approximately 4.3 km. Farms are spread over the area. “Lamezia Terme” points to the most densely populated areas of the municipality.</p>
Full article ">Figure 1 Cont.
<p>(<b>A</b>): MapChart of Italy highlighting the region of Calabria. (<b>B</b>): Location of LMT in Calabria itself. (<b>C</b>) Details of the Lamezia Terme area with a highlight on notable emission sources in the area. The “Highway” mark refers to a point where the distance between the A2 highway and LMT is approximately 4.3 km. Farms are spread over the area. “Lamezia Terme” points to the most densely populated areas of the municipality.</p>
Full article ">Figure 2
<p>(<b>A</b>): Total hourly wind speeds and directions observed between 1 February and 31 July 2020 at LMT, plotted in a wind rose highlighting the main W (seaside) and NE (continental) corridors described in <a href="#sec2dot1-sustainability-16-08229" class="html-sec">Section 2.1</a>. Each bar covers an angle of 8 degrees (1/45 of 360°). (<b>B</b>): Average hourly wind directions during the ALD (ante-lockdown), LD (lockdown), and PLD (post-lockdown) periods, with shaded areas covering the average ± σ (standard deviation) range.</p>
Full article ">Figure 3
<p>Daily averaged temperatures (°C) throughout the entire FEB–JUL 2020 study period. The vertical dotted lines mark the beginning and the end of the first Italian nationwide LD, respectively. These periods are also marked by the horizontal ALD, LD, and PLD labels. The color pattern was set to mark the difference between typical Mediterranean winter temperatures (dark blue) and temperatures closer to summertime averages (red).</p>
Full article ">Figure 4
<p>Correlations between daily temperatures and each parameter, differentiated by period of observation (ALD, LD, PLD). Data ellipses refer to a 90% confidence interval. (<b>A</b>): CO; (<b>B</b>): CO<sub>2</sub>; (<b>C</b>): CH<sub>4</sub>; (<b>D</b>): eBC; (<b>E</b>): NO<sub>x</sub>.</p>
Full article ">Figure 4 Cont.
<p>Correlations between daily temperatures and each parameter, differentiated by period of observation (ALD, LD, PLD). Data ellipses refer to a 90% confidence interval. (<b>A</b>): CO; (<b>B</b>): CO<sub>2</sub>; (<b>C</b>): CH<sub>4</sub>; (<b>D</b>): eBC; (<b>E</b>): NO<sub>x</sub>.</p>
Full article ">Figure 5
<p>Hourly trends observed between February and July 2020, differentiated by period (ALD, LD, PLD). The smoothed black line was computed using the “loess” method to estimate trends through time. (<b>A</b>): CO; (<b>B</b>): CO<sub>2</sub>; (<b>C</b>): CH<sub>4</sub>; (<b>D</b>): eBC; (<b>E</b>): NO<sub>x</sub>.</p>
Full article ">Figure 5 Cont.
<p>Hourly trends observed between February and July 2020, differentiated by period (ALD, LD, PLD). The smoothed black line was computed using the “loess” method to estimate trends through time. (<b>A</b>): CO; (<b>B</b>): CO<sub>2</sub>; (<b>C</b>): CH<sub>4</sub>; (<b>D</b>): eBC; (<b>E</b>): NO<sub>x</sub>.</p>
Full article ">Figure 6
<p>Averaged daily cycles of all observed parameters, differentiated by ALD, LD, and PLD periods. Shaded areas show ±σ (standard deviation) ranges. To ease visualization, the legend is shown in (<b>A</b>) alone. (<b>A</b>): CO; (<b>B</b>): CO<sub>2</sub>; (<b>C</b>): CH<sub>4</sub>; (<b>D</b>): eBC; (<b>E</b>): NO<sub>x</sub>.</p>
Full article ">Figure 6 Cont.
<p>Averaged daily cycles of all observed parameters, differentiated by ALD, LD, and PLD periods. Shaded areas show ±σ (standard deviation) ranges. To ease visualization, the legend is shown in (<b>A</b>) alone. (<b>A</b>): CO; (<b>B</b>): CO<sub>2</sub>; (<b>C</b>): CH<sub>4</sub>; (<b>D</b>): eBC; (<b>E</b>): NO<sub>x</sub>.</p>
Full article ">Figure 7
<p>Correlation between hourly averaged data and wind speeds, differentiated by sector (#1 plots for the NE-continental corridor; #2 plots for the W-seaside corridor; and #3 plots for all wind directions, including those falling outside the two main corridors). The color scheme differentiates periods of observation (ALD, LD, PLD) following the same pattern used in other graphs. (<b>A1</b>–<b>A3</b>): CO; (<b>B1</b>–<b>B3</b>): CO<sub>2</sub>; (<b>C1</b>–<b>C3</b>): CH<sub>4</sub>; (<b>D1</b>–<b>D3</b>): eBC; (<b>E1</b>–<b>E3</b>): NO<sub>x</sub>.</p>
Full article ">Figure 7 Cont.
<p>Correlation between hourly averaged data and wind speeds, differentiated by sector (#1 plots for the NE-continental corridor; #2 plots for the W-seaside corridor; and #3 plots for all wind directions, including those falling outside the two main corridors). The color scheme differentiates periods of observation (ALD, LD, PLD) following the same pattern used in other graphs. (<b>A1</b>–<b>A3</b>): CO; (<b>B1</b>–<b>B3</b>): CO<sub>2</sub>; (<b>C1</b>–<b>C3</b>): CH<sub>4</sub>; (<b>D1</b>–<b>D3</b>): eBC; (<b>E1</b>–<b>E3</b>): NO<sub>x</sub>.</p>
Full article ">Figure 7 Cont.
<p>Correlation between hourly averaged data and wind speeds, differentiated by sector (#1 plots for the NE-continental corridor; #2 plots for the W-seaside corridor; and #3 plots for all wind directions, including those falling outside the two main corridors). The color scheme differentiates periods of observation (ALD, LD, PLD) following the same pattern used in other graphs. (<b>A1</b>–<b>A3</b>): CO; (<b>B1</b>–<b>B3</b>): CO<sub>2</sub>; (<b>C1</b>–<b>C3</b>): CH<sub>4</sub>; (<b>D1</b>–<b>D3</b>): eBC; (<b>E1</b>–<b>E3</b>): NO<sub>x</sub>.</p>
Full article ">Figure 7 Cont.
<p>Correlation between hourly averaged data and wind speeds, differentiated by sector (#1 plots for the NE-continental corridor; #2 plots for the W-seaside corridor; and #3 plots for all wind directions, including those falling outside the two main corridors). The color scheme differentiates periods of observation (ALD, LD, PLD) following the same pattern used in other graphs. (<b>A1</b>–<b>A3</b>): CO; (<b>B1</b>–<b>B3</b>): CO<sub>2</sub>; (<b>C1</b>–<b>C3</b>): CH<sub>4</sub>; (<b>D1</b>–<b>D3</b>): eBC; (<b>E1</b>–<b>E3</b>): NO<sub>x</sub>.</p>
Full article ">Figure 7 Cont.
<p>Correlation between hourly averaged data and wind speeds, differentiated by sector (#1 plots for the NE-continental corridor; #2 plots for the W-seaside corridor; and #3 plots for all wind directions, including those falling outside the two main corridors). The color scheme differentiates periods of observation (ALD, LD, PLD) following the same pattern used in other graphs. (<b>A1</b>–<b>A3</b>): CO; (<b>B1</b>–<b>B3</b>): CO<sub>2</sub>; (<b>C1</b>–<b>C3</b>): CH<sub>4</sub>; (<b>D1</b>–<b>D3</b>): eBC; (<b>E1</b>–<b>E3</b>): NO<sub>x</sub>.</p>
Full article ">Figure 8
<p>Weekly trends observed at LMT between February and July 2020. The dotted horizontal lines show average values per category. ALD (dark blue), LD (yellow), PLD (dark green). (<b>A</b>): CO; (<b>B</b>): CO<sub>2</sub>; (<b>C</b>): CH<sub>4</sub>; (<b>D</b>): eBC; (<b>E</b>): NO<sub>x</sub>.</p>
Full article ">Figure 8 Cont.
<p>Weekly trends observed at LMT between February and July 2020. The dotted horizontal lines show average values per category. ALD (dark blue), LD (yellow), PLD (dark green). (<b>A</b>): CO; (<b>B</b>): CO<sub>2</sub>; (<b>C</b>): CH<sub>4</sub>; (<b>D</b>): eBC; (<b>E</b>): NO<sub>x</sub>.</p>
Full article ">
22 pages, 27897 KiB  
Article
Evaluation of the Urban Canopy Scheme TERRA-URB in the ICON Model at Hectometric Scale over the Naples Metropolitan Area
by Davide Cinquegrana, Myriam Montesarchio, Alessandra Lucia Zollo and Edoardo Bucchignani
Atmosphere 2024, 15(9), 1119; https://doi.org/10.3390/atmos15091119 - 14 Sep 2024
Viewed by 936
Abstract
The present work is focused on the validation of the urban canopy scheme TERRA-URB, implemented in ICON weather forecast model. TERRA-URB is used to capture the behavior of urbanized areas as sources of heat fluxes, mainly due to anthropogenic activities that can influence [...] Read more.
The present work is focused on the validation of the urban canopy scheme TERRA-URB, implemented in ICON weather forecast model. TERRA-URB is used to capture the behavior of urbanized areas as sources of heat fluxes, mainly due to anthropogenic activities that can influence temperature, humidity, and other atmospheric variables of the surrounding areas. Heat fluxes occur especially during the nighttime in large urbanized areas, characterized by poor vegetation, and are responsible for the formation of Urban Heat and Dry Island, i.e., higher temperatures and lower humidity compared to rural areas. They can be exacerbated under severe conditions, with dangerous consequences for people living in these urban areas. For these reasons, the need of accurately forecasting these phenomena is particularly felt. The present work represents one of the first attempts of using a very high resolution (about 600 m) in a Numerical Weather Prediction model. Performances of this advanced version of ICON have been investigated over a domain located in southern Italy, including the urban metropolitan area of Naples, considering a week characterized by extremely high temperatures. Results highlight that the activation of TERRA-URB scheme entails a better representation of temperature, relative humidity, and wind speed in urban areas, especially during nighttime, also allowing a proper reproduction of Urban Heat and Dry Island effects. Over rural areas, instead, no significant differences are found in model results when the urban canopy scheme is used. Full article
(This article belongs to the Section Meteorology)
Show Figures

Figure 1

Figure 1
<p>An overview of the urban–atmosphere interactions resolved by TERRA-URB, from Wouters et al. [<a href="#B35-atmosphere-15-01119" class="html-bibr">35</a>].</p>
Full article ">Figure 2
<p>The orography of the computational domain simulated, located in southern Italy.</p>
Full article ">Figure 3
<p>Surface air temperature anomaly for July 2022 over Europe, from <a href="https://www.copernicus.eu/en/media/image-day-gallery/surface-air-temperature-anomaly-july-2022" target="_blank">https://www.copernicus.eu/en/media/image-day-gallery/surface-air-temperature-anomaly-july-2022</a> (accessed on 13 September 2024).</p>
Full article ">Figure 4
<p>ICON urban paved fraction values (fr_paved), over a zoomed domain considered for the model validation.</p>
Full article ">Figure 5
<p>Location of ground stations (<b>a</b>) and corresponding values of ICON urban paved fraction (<b>b</b>).</p>
Full article ">Figure 6
<p>Diurnal cycles for the variables analyzed, averaged over the considered week, with standard deviations: comparison of ICON output against ground station data.</p>
Full article ">Figure 7
<p>Diurnal cycles of T2m, Rh2m, Ws10m, and Wd10m, averaged over the considered week, with standard deviations: comparison of ICON output against rural and urban stations data.</p>
Full article ">Figure 8
<p>Taylor Diagram of T2m, Rh2m, Ws10m, and Wd10m for urban and rural stations: comparison between TU on and off.</p>
Full article ">Figure 8 Cont.
<p>Taylor Diagram of T2m, Rh2m, Ws10m, and Wd10m for urban and rural stations: comparison between TU on and off.</p>
Full article ">Figure 9
<p>Diurnal cycle of transfer coefficients for heat in rural (<b>a</b>) and urban (<b>b</b>) stations.</p>
Full article ">Figure 10
<p>Diurnal cycle of Sensible Surface heat fluxes in rural (<b>a</b>) and urban (<b>b</b>) stations.</p>
Full article ">Figure 11
<p>Diurnal cycle of Latent Surface heat fluxes in rural (<b>a</b>) and urban (<b>b</b>) stations.</p>
Full article ">Figure 12
<p>Time series of T2m over the considered week, for selected stations (observational data and model output with TU on and off).</p>
Full article ">Figure 12 Cont.
<p>Time series of T2m over the considered week, for selected stations (observational data and model output with TU on and off).</p>
Full article ">Figure 13
<p>Time series of Rh2m over the considered week, for selected stations (observational data and model output with TU on and off).</p>
Full article ">Figure 14
<p>Map of temperature differences provided by ICON, assuming TU on and off, over the Naples Metropolitan Area.</p>
Full article ">Figure 15
<p>Map of relative humidity differences provided by ICON assuming TU on and off, over the Naples Metropolitan Area.</p>
Full article ">Figure 16
<p>Diurnal cycle of an Urban Heat Island (<b>a</b>) and an Urban Dry Island (<b>b</b>), assuming TU is switched on and off.</p>
Full article ">Figure 17
<p>Diurnal cycle of an Urban Heat Island and an Urban Dry Island: ICON vs. Observed.</p>
Full article ">
22 pages, 3944 KiB  
Article
Insulating Innovative Geopolymer Foams with Natural Fibers and Phase-Change Materials—A Review of Solutions and Research Results
by Agnieszka Przybek and Michał Łach
Materials 2024, 17(18), 4503; https://doi.org/10.3390/ma17184503 - 13 Sep 2024
Viewed by 1703
Abstract
Geopolymers are synthesized using anthropogenic raw materials and waste from the energy industry. Their preparation necessitates an alkaline activator, which facilitates the dissolution of raw materials and their subsequent binding. At present, geopolymers are considered a promising material with the potential to replace [...] Read more.
Geopolymers are synthesized using anthropogenic raw materials and waste from the energy industry. Their preparation necessitates an alkaline activator, which facilitates the dissolution of raw materials and their subsequent binding. At present, geopolymers are considered a promising material with the potential to replace conventional cement-based products. This research investigates foamed geopolymer materials based on fly ash, natural fibers, and phase-change materials. The study utilized three distinct types of fibers and two phase-change materials manufactured by Rubitherm Technologies GmbH of Germany. This paper presents the results of the thermal conductivity coefficient and specific heat tests on the finished foams. Additionally, compressive strength tests were conducted on the samples after 28 days. Natural fibers decreased the insulation parameter by 12%, while PCM enhanced it by up to 6%. The addition of fibers increased the compressive strength by nearly 30%, whereas PCM reduced this by as little as 14%. Natural fibers and phase-change materials had an increased heat capacity by up to 35%. The results demonstrated the material’s potential in various industrial sectors, with the primary areas of application being building materials and insulations. The findings illustrate the significant potential of these composites as energetically and environmentally sustainable materials. Full article
Show Figures

Figure 1

Figure 1
<p>The bonding scheme of geopolymer materials.</p>
Full article ">Figure 2
<p>The essence of phase-change materials (permission from Microtek Laboratories Inc.).</p>
Full article ">Figure 3
<p>Fibers of natural origin: (<b>a</b>) flax, (<b>b</b>) sisal, (<b>c</b>) cotton, (<b>d</b>) bamboo, (<b>e</b>) hemp, (<b>f</b>) coconut, (<b>g</b>) jute, (<b>h</b>) sugar cane, (<b>i</b>) banana.</p>
Full article ">Figure 4
<p>Materials used for the fabrication of the samples (<b>a</b>–<b>e</b>) and additives (<b>f</b>–<b>j</b>): (<b>a</b>) fly ash, (<b>b</b>) sand, (<b>c</b>) cement, (<b>d</b>) fly ash microspheres, (<b>e</b>) Syringaldehyde, (<b>f</b>) hay, (<b>g</b>) wood shavings, (<b>h</b>) coconut fibers, (<b>i</b>) GR42, (<b>j</b>) PX25.</p>
Full article ">Figure 5
<p>Diagram of geopolymer foams manufacturing. Indication of the various processes from multi-step mixing of ingredients to curing and sample molding.</p>
Full article ">Figure 6
<p>Compressive strength of samples with the addition of natural fibers and phase-change materials. Confirmation of the positive effect of fiber addition on compressive strength.</p>
Full article ">Figure 7
<p>Thermal conductivity of samples with the addition of natural fibers and phase-change materials.</p>
Full article ">Figure 8
<p>Porous structure morphology: (<b>a</b>) reference fly ash, (<b>b</b>) 1% of hay, (<b>c</b>) 1% of wood shavings, (<b>d</b>) 1% of coconut fibers (<b>e</b>) 2.5% GR42 (<b>f</b>) 7.5% GR42 (<b>g</b>) 2.5% PX25 (<b>h</b>) 7.5% PX25.</p>
Full article ">Figure 9
<p>Microstructure of the sample: (<b>a</b>) reference fly ash, (<b>b</b>) 1% of hay, (<b>c</b>) 1% of wood shavings, (<b>d</b>) 1% of coconut fibers (<b>e</b>) 2.5% GR42 (<b>f</b>) 7.5% GR42 (<b>g</b>) 2.5% PX25 (<b>h</b>) 7.5% PX25.</p>
Full article ">
13 pages, 12208 KiB  
Article
Weekday–Holiday Differences in Urban Wind Speed in Japan
by Fumiaki Fujibe
Urban Sci. 2024, 8(3), 141; https://doi.org/10.3390/urbansci8030141 - 13 Sep 2024
Viewed by 850
Abstract
Wind speed differences between weekdays and holidays at urban sites in Japan were investigated in search of the influence of urban anthropogenic heat on surface wind speed using data from the Automated Meteorological Data Acquisition System (AMeDAS) of the Japan Meteorological Agency (JMA) [...] Read more.
Wind speed differences between weekdays and holidays at urban sites in Japan were investigated in search of the influence of urban anthropogenic heat on surface wind speed using data from the Automated Meteorological Data Acquisition System (AMeDAS) of the Japan Meteorological Agency (JMA) for 44 years. The wind speed was found to be lower on holidays than on weekdays, not only in large cities but also in areas with medium degrees of urbanization, which is interpreted to be due to the stronger stability of the surface boundary layer under lower temperatures with smaller amounts of anthropogenic heat. The rate of decrease is about −3% in central Tokyo, and about −0.5% for the average over stations with population densities between 1000 and 3000 km−2. Additionally, an analysis using the spatially dense data on the Air Pollution Monitoring System of Tokyo Metropolis for 28 years showed that negative anomalies in wind speed on holidays were detected at many stations in the Tokyo Wards Area, although negative temperature anomalies were limited to a few stations in the central area or near big roads, suggesting different spatial scales in the response of temperature and wind speed to anthropogenic heat. Full article
Show Figures

Figure 1

Figure 1
<p>Map showing (<b>a</b>) the topography of East Asia, (<b>b</b>) locations of the AMeDAS stations used for analysis, and (<b>c</b>) the APMS and AMeDAS stations in the Tokyo Wards Area (TWA). The square in (<b>a</b>) indicates the region shown in (<b>b</b>), and the square in (<b>b</b>) indicates the region shown in (<b>c</b>). In (<b>c</b>), the boundaries of prefectures and the Tokyo Metropolis are shown in green solid lines, and the western border of the TWA is shown in a green dotted line.</p>
Full article ">Figure 2
<p>Weekly variations of daily mean values of <span class="html-italic">∆T</span> and <span class="html-italic">∆v</span> for April 1979 to March 2023. Vertical bars indicate the 95% confidence ranges, and symbols at the bottom of each panel indicate the degree of statistical significance, in red and blue for positive and negative values, respectively (the same in the following figures).</p>
Full article ">Figure 3
<p>Diurnal variations of <span class="html-italic">∆T</span> and <span class="html-italic">∆v</span> for holidays. The values on Sundays only are shown in dashed green lines without confidence ranges.</p>
Full article ">Figure 4
<p>Same as <a href="#urbansci-08-00141-f003" class="html-fig">Figure 3</a>, but for Saturdays.</p>
Full article ">Figure 5
<p>Seasonal variation of daily mean values of <span class="html-italic">∆T</span> and <span class="html-italic">∆v</span> on holidays.</p>
Full article ">Figure 6
<p>Daily mean values of <span class="html-italic">∆T</span> and <span class="html-italic">∆v</span> on holidays for each subperiod.</p>
Full article ">Figure 7
<p>Distribution of <span class="html-italic">∆T</span> and <span class="html-italic">∆v</span> on holidays in TWA for April 1995 to March 2023. Open and closed squares indicate positive and negative values, respectively.</p>
Full article ">Figure 8
<p>Diurnal variations of <span class="html-italic">∆T</span> and <span class="html-italic">∆v</span> for holidays at APMS stations in TWA.</p>
Full article ">Figure 9
<p>Daily mean values of <span class="html-italic">∆T</span> and <span class="html-italic">∆v</span> on holidays at each level on Tokyo Tower, and their diurnal variations at three levels on the tower.</p>
Full article ">
33 pages, 13344 KiB  
Article
Presenting a Long-Term, Reprocessed Dataset of Global Sea Surface Temperature Produced Using the OSTIA System
by Mark Worsfold, Simon Good, Chris Atkinson and Owen Embury
Remote Sens. 2024, 16(18), 3358; https://doi.org/10.3390/rs16183358 - 10 Sep 2024
Cited by 2 | Viewed by 1303
Abstract
Over the past few decades, the oceans have stored the majority of the excess heat in the climate system resulting from anthropogenic emissions. An accurate, long-term sea surface temperature (SST) dataset is essential for monitoring and researching the changes to the global oceans. [...] Read more.
Over the past few decades, the oceans have stored the majority of the excess heat in the climate system resulting from anthropogenic emissions. An accurate, long-term sea surface temperature (SST) dataset is essential for monitoring and researching the changes to the global oceans. A variety of SST datasets have been produced by various institutes over the years, and here, we present a new SST data record produced originally within the Copernicus Marine Environment Monitoring Service (which is therefore named CMEMS v2.0) and assess: (1) its accuracy compared to independent observations; (2) how it compares with the previous version (named CMEMS v1.2); and (3) its performance during two major volcanic eruptions. By comparing both versions of the CMEMS datasets using independent in situ observations, we show that both datasets are within the target accuracy of 0.1 K, but that CMEMS v2.0 is closer to the ground truth. The uncertainty fields generated by the two analyses were also compared, and CMEMS v2.0 was found to provide a more accurate estimate of its own uncertainties. Frequency and vector analysis of the SST fields determined that CMEMS v2.0 feature resolution and horizontal gradients were also superior, indicating that it resolved oceanic features with greater clarity. The behavior of the two analyses during two volcanic eruption events (Mt. Pinatubo and El Chichón) was examined. A comparison with the HadSST4 gridded in situ dataset suggested a cool bias in the CMEMS v2.0 dataset versus the v1.2 dataset following the Pinatubo eruption, although a comparison with sparser buoy-only observations yielded less clear results. No clear impact of the El Chichón eruption (which was a smaller event than Mt. Pinatubo) on CMEMS v2.0 was found. Overall, with the exception of a few specific and extreme events early in the time series, CMEMS v2.0 possesses high accuracy, resolution, and stability and is recommended to users. Full article
(This article belongs to the Section Ocean Remote Sensing)
Show Figures

Graphical abstract

Graphical abstract
Full article ">Figure 1
<p>Timeline of satellite and reference sensors. The reference sensor timeline is below the blue line.</p>
Full article ">Figure 2
<p>Monthly count of the number of SIRDS observations used for validating each of the analyses. There are slight differences between the two because of differences in the locations of the edges of the ice sheet.</p>
Full article ">Figure 3
<p>Analysis vs. in situ statistics plots of CMEMS v1.2 and v2.0. (<b>top</b>) Analysis–in situ mean difference; (<b>bottom</b>) analysis–in situ standard deviation. Shaded areas are 5th and 95th percentiles.</p>
Full article ">Figure 4
<p>Analysis vs. in situ statistics (same as <a href="#remotesensing-16-03358-f003" class="html-fig">Figure 3</a>, but with reduced scale) plots of CMEMS v1.2 and v2.0. (<b>top</b>) Analysis–in situ mean difference; (<b>bottom</b>) analysis–in situ standard deviation. Shaded areas are 5th and 95th percentiles.</p>
Full article ">Figure 5
<p>Analysis − Argo in situ mean difference and standard deviation for trial using AMSR2 as a reference sensor versus the AVHRR-MTA and SLSTR-A reference sensors used in CMEMS v2.0. Shaded areas are 95th-percentile confidence intervals calculated using a bootstrap method. The dashed line is zero.</p>
Full article ">Figure 6
<p>Binned analysis: in situ mean difference, averaged over August 2012 to December 2020. Top row—spatial bias maps with 2.5° bins: (<b>a</b>): CMEMS v2.0. (<b>b</b>): AMSR2 as reference sensor. Bottom row—longitudinal average plots with 2° bins: (<b>c</b>): CMEMS v2.0. (<b>d</b>): AMSR2 as reference sensor.</p>
Full article ">Figure 7
<p>Top row—global Argo data, 2000–2007. (<b>a</b>) CMEMS v1.2, (<b>b</b>) CMEMS v2.0. Bottom row—global buoy data, 1985–2007. (<b>c</b>) CMEMS v1.2 (<b>d</b>) CMEMS v2.0.</p>
Full article ">Figure 8
<p>Power spectrum plots of three regions of Interest (ROI) for the time period 1985–2007. (<b>a</b>) Gulf Stream. (<b>b</b>) Agulhas Current Retroreflection. (<b>c</b>) Kuroshio Current.</p>
Full article ">Figure 9
<p>ROI horizontal gradients for 2007. Units: mk/km. (<b>Left</b>) CMEMS v1.2. (<b>Right</b>) CMEMS v2.0. (<b>Top</b>) Gulf Stream. (<b>Middle</b>) Agulhas Current Retroreflection. (<b>Bottom</b>) Kuroshio Current.</p>
Full article ">Figure 10
<p>CMEMS v1.2 monthly average obs-background field bias plots for June–August 1991. AVHRR (<b>top row</b>); ATSR-1: (<b>bottom row</b>).</p>
Full article ">Figure 11
<p>CMEMS v2.0 AVHRR monthly average obs-background bias plots. ATSR1 data were not used in CMEMS v2.0 during this time period.</p>
Full article ">Figure 12
<p>Number of drifting and moored buoy observations for 1991 in 2.5-degree bins. Black lines are 20°S and 30°N latitudes to demonstrate the Mt. Pinatubo study region.</p>
Full article ">Figure 13
<p>Spatially averaged L4 analysis minus median HadSST4 in situ difference for latitudes 20°S to 30°N.</p>
Full article ">Figure 14
<p>Spatially averaged L4 analysis minus median HadSST4 in situ difference for latitudes 0–30°N and longitudes 60–150°W.</p>
Full article ">
Back to TopTop