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

Dunkerley, 2010 - Google Patents

How do the rain rates of sub‐event intervals such as the maximum 5‐and 15‐min rates (I5 or I30) relate to the properties of the enclosing rainfall event?

Dunkerley, 2010

Document ID
16731130321495113238
Author
Dunkerley D
Publication year
Publication venue
Hydrological Processes

External Links

Snippet

The intensity‐duration properties of rain have been explored using various approaches, including daily or hourly data, IDF and event‐based analyses, and the study of rain properties across intra‐event durations such as the widely used I30 indicator of peak event …
Continue reading at onlinelibrary.wiley.com (other versions)

Classifications

    • GPHYSICS
    • G01MEASURING; TESTING
    • G01WMETEOROLOGY
    • G01W1/00Meteorology
    • G01W1/10Devices for predicting weather conditions
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01WMETEOROLOGY
    • G01W1/00Meteorology
    • G01W1/14Rainfall or precipitation gauges
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01WMETEOROLOGY
    • G01W1/00Meteorology
    • G01W1/02Instruments for indicating weather conditions by measuring two or more variables, e.g. humidity, pressure, temperature, cloud cover, wind speed
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01WMETEOROLOGY
    • G01W1/00Meteorology
    • G01W1/08Adaptations of balloons, missiles, or aircraft for meteorological purposes; Radiosondes

Similar Documents

Publication Publication Date Title
Safeeq et al. Coupling snowpack and groundwater dynamics to interpret historical streamflow trends in the western United States
Yan et al. Next‐generation intensity‐duration‐frequency curves for hydrologic design in snow‐dominated environments
Costa et al. Temperature signal in suspended sediment export from an Alpine catchment
Merz et al. A process typology of regional floods
Dunkerley How do the rain rates of sub‐event intervals such as the maximum 5‐and 15‐min rates (I5 or I30) relate to the properties of the enclosing rainfall event?
Tennant et al. Elevation‐dependent responses of streamflow to climate warming
Eum et al. Inter‐comparison of high‐resolution gridded climate data sets and their implication on hydrological model simulation over the Athabasca Watershed, Canada
Krakauer et al. Stream recession curves and storage variability in small watersheds
Camici et al. Design soil moisture estimation by comparing continuous and storm‐based rainfall‐runoff modeling
Rogger et al. Step changes in the flood frequency curve: Process controls
Wright et al. Critical examination of area reduction factors
Cosgrove et al. NOAA's National Water Model: Advancing operational hydrology through continental‐scale modeling
Shayeghi et al. Reliability of reanalysis and remotely sensed precipitation products for hydrological simulation over the Sefidrood River Basin, Iran
Lam et al. Reducing uncertainty with flood frequency analysis: The contribution of paleoflood and historical flood information
Crawford et al. Capturing season‐specific precipitation signals in the northern Rocky Mountains, USA, using earlywood and latewood tree rings
Lewis et al. From months to minutes–exploring the value of high‐resolution rainfall observation and prediction during the UK winter storms of 2013/2014
Kim et al. Assessment of antecedent moisture condition on flood frequency: An experimental study in Napa River Basin, CA
Knight et al. A bimillennial-length tree-ring reconstruction of precipitation for the Tavaputs Plateau, Northeastern Utah
Bloomfield et al. Analysis of groundwater drought using a variant of the Standardised Precipitation Index
Shepherd et al. Climate change and future flows of Rocky Mountain rivers: converging forecasts from empirical trend projection and down‐scaled global circulation modelling
Mascaro et al. Temporal downscaling and statistical analysis of rainfall across a topographic transect in northwest Mexico
Jomelli et al. Respective influence of geomorphologic and climate conditions on debris-flow occurrence in the Northern French Alps
Yoon et al. Flood flow simulation using CMAX radar rainfall estimates in orographic basins
Rawat et al. Rainfall variability analysis using Precipitation Concentration Index: A case study of the western agro-climatic zone of Punjab, India
Bayat-Afshary et al. Are the magnitude and frequency of floods increasing in Iran due to climate change? Implications from a 50-year analysis