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Keywords = Oum Er Rabia

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26 pages, 6374 KiB  
Article
Multi-Index Approach to Assess and Monitor Meteorological and Agricultural Drought in the Mediterranean Region: Case of the Upper Oum Er Rabia Watershed, Morocco
by Mohammed Mouad Mliyeh, Yassine Ait Brahim, Eleni-Ioanna Koutsovili, Ourania Tzoraki, Ahmed Zian, Mourad Aqnouy and Lahcen Benaabidate
Water 2024, 16(21), 3104; https://doi.org/10.3390/w16213104 - 29 Oct 2024
Viewed by 737
Abstract
Drought is a severe disaster, increasingly exacerbated by climate change, and poses significant challenges worldwide, particularly in arid and semi-arid regions like Morocco. This study aims to assess and monitor drought using a multi-index approach to provide a comprehensive understanding of its spatio-temporal [...] Read more.
Drought is a severe disaster, increasingly exacerbated by climate change, and poses significant challenges worldwide, particularly in arid and semi-arid regions like Morocco. This study aims to assess and monitor drought using a multi-index approach to provide a comprehensive understanding of its spatio-temporal dynamics at both meteorological and agricultural levels. The research focuses on the Upper Oum Er Rabia watershed, which spans 35,000 km2 and contributes approximately a quarter of Morocco’s renewable water resources. We propose a methodology that combines ERA5 temperature data from remote sensing with ground-based precipitation data to analyze drought characteristics. Three meteorological indices were utilized: the Standardized Precipitation Index (SPI), the Standardized Precipitation Evapotranspiration Index (SPEI), and the Reconnaissance Drought Index (RDI). Additionally, three remote-sensing indices were employed to capture agricultural drought: the Normalized Difference Vegetation Index (NDVI), the Enhanced Vegetation Index (EVI), and the Crop Water Stress Index (CWSI), with a total of 528 NDVI and EVI images and 1016 CWSI images generated through Google Earth Engine (GEE), using machine-learning techniques. Trend analyses were conducted to monitor drought patterns spatio-temporally. Our results reveal that the three-month interval is critical for effective drought monitoring and evaluation. Among the indices, SPEI emerged as the most effective for capturing drought in combination with remote-sensing data, while CWSI exhibited the highest correlation with SPEI over the three-month period, outperforming NDVI and EVI. The trend analysis indicates a significant precipitation deficit, alongside increasing trends in temperature and evapotranspiration over both the short and long term. Furthermore, all drought indices (SPI, SPEI, and RDI) demonstrate an intensification of drought conditions. Adaptation strategies are essential for managing water resources in the Upper Oum Er Rabia watershed under these evolving climate conditions. Continuous monitoring of climate variables and drought indices will be crucial for tracking changes and informing future water management strategies. Full article
(This article belongs to the Section Water and Climate Change)
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Figure 1
<p>Location of study area.</p>
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<p>Average annual precipitation (1979-2022).</p>
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<p>Average monthly temperatures and potential evapotranspiration.</p>
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<p>Flowchart of the adopted methodology.</p>
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<p>Correlation graphs between observed temperatures and ERA5 product temperatures: (<b>a</b>–<b>d</b>) Ahmed El Hansali station and (<b>e</b>,<b>f</b>) Tarhat station.</p>
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<p>Graph of monthly SPEI (3 months) and CWSI.</p>
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<p>Graph of SPEI (3 months) and CWSI in the spring season.</p>
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<p>(<b>a</b>) Annual precipitation, SPEI, RDI and SPI, (<b>b</b>) annual, (<b>c</b>) 12 months, (<b>d</b>) 6 months, (<b>e</b>) 3 months, and (<b>f</b>) 1 month.</p>
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30 pages, 27337 KiB  
Article
Nested Cross-Validation for HBV Conceptual Rainfall–Runoff Model Spatial Stability Analysis in a Semi-Arid Context
by Mohamed El Garnaoui, Abdelghani Boudhar, Karima Nifa, Yousra El Jabiri, Ismail Karaoui, Abdenbi El Aloui, Abdelbasset Midaoui, Morad Karroum, Hassan Mosaid and Abdelghani Chehbouni
Remote Sens. 2024, 16(20), 3756; https://doi.org/10.3390/rs16203756 - 10 Oct 2024
Viewed by 1288
Abstract
Accurate and efficient streamflow simulations are necessary for sustainable water management and conservation in arid and semi-arid contexts. Conceptual hydrological models often underperform in these catchments due to the high climatic variability and data scarcity, leading to unstable parameters and biased results. This [...] Read more.
Accurate and efficient streamflow simulations are necessary for sustainable water management and conservation in arid and semi-arid contexts. Conceptual hydrological models often underperform in these catchments due to the high climatic variability and data scarcity, leading to unstable parameters and biased results. This study evaluates the stability of the HBV model across seven sub-catchments of the Oum Er Rabia river basin (OERB), focusing on the HBV model regionalization process and the effectiveness of Earth Observation data in enhancing predictive capability. Therefore, we developed a nested cross-validation framework for spatiotemporal stability assessment, using optimal parameters from a donor-single-site calibration (DSSC) to inform target-multi-site calibration (TMSC). The results show that the HBV model remains spatially transferable from one basin to another with moderate to high performances (KGE (0.1~0.9 NSE (0.5~0.8)). Furthermore, calibration using KGE improves model stability over NSE. Some parameter sets exhibit spatial instability, but inter-annual parameter behavior remains stable, indicating potential climate change impacts. Model performance declines over time (18–124%) with increasing dryness. As a conclusion, this study presents a framework for analyzing parameter stability in hydrological models and highlights the need for more research on spatial and temporal factors affecting hydrological response variability. Full article
(This article belongs to the Special Issue Multi-Source Remote Sensing Data in Hydrology and Water Management)
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<p>Location of the seven study catchments in the Oum Er Rabia river basin. Land use and Land cover of the study area.</p>
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<p>HBV (Hydrologiska Byråns Vattenbalansavedelning) model scheme, modified from [<a href="#B83-remotesensing-16-03756" class="html-bibr">83</a>].</p>
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<p>Work modeling flowchart. Note that the warm-up year (2000–2001) is not included in the original modeling time series.</p>
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<p>Hydrograph of observed against simulated streamflow in AOCH (donor catchment) and the six target catchments calibrated and validated in the year 2009–2010 (as example).</p>
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<p>Hydrograph of observed against simulated streamflow in AOCH (donor catchment) and the six target catchments calibrated and validated in the year 2009–2010 (as example).</p>
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<p>Resume of optimal parameter sets versus performance metrics during spatiotemporal cross validation process.</p>
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<p>Best parameter set variation over seven sub-catchments of the study area.</p>
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<p>Variation of long-term trend of KGE performance metric across study catchments between 2001 and 2019 (mean: blue line, median: red line, standard deviation: orange line, trend: black line).</p>
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<p>Variation of long-term trend of NSE performance metric across study catchments between 2001 and 2019 (mean: blue line, median: red line, standard deviation: orange line, trend: black line).</p>
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<p>Variation of long-term trend of RMSE performance metric across study catchments between 2001 and 2019 (mean: blue line, median: red line, standard deviation: orange line, trend: black line).</p>
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<p>KGE, NSE, R<sup>2</sup>, and RMSE metric variations for different catchments across years.</p>
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<p>Variation of long-term trend of optimal parameters, across study catchments over time between 2001 and 2019 (mean: blue line, median: red line, standard deviation: orange line, trend: black line).</p>
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<p>Variation of long-term trend of optimal parameters, across study catchments over time between 2001 and 2019 (mean: blue line, median: red line, standard deviation: orange line, trend: black line).</p>
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<p>HBV model performance loss assessment over time and space using MRC criterion [<a href="#B98-remotesensing-16-03756" class="html-bibr">98</a>]. Green icon: No performance loss (or performance gain), yellow icon: low performance loss, and red icon: high performance loss (model crash).</p>
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<p>HBV model performance loss trend over time and space ((<b>A</b>) KGE, (<b>B</b>) NSE, (<b>C</b>) R<sup>2</sup>).</p>
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<p>Variation of long-term trend of R<sup>2</sup> performance metric across study catchments between 2001 and 2019 (mean: blue line, median: red line, standard deviation: orange line, trend: black line).</p>
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<p>Variation of long-term trend of RVE performance metric across study catchments between 2001 and 2019 (mean: blue line, median: red line, standard deviation: orange line, trend: black line).</p>
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<p>RVE metric variation for different catchments across years.</p>
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