2013
DOI: 10.2172/1091096
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THE APPLICATION OF A STATISTICAL DOWNSCALING PROCESS TO DERIVE 21{sup ST} CENTURY RIVER FLOW PREDICTIONS USING A GLOBAL CLIMATE SIMULATION

Abstract: Executive SummaryThe ability of water managers to maintain adequate supplies in coming decades depends, in part, on future weather conditions, as climate change has the potential to alter river flows from their current values, possibly rendering them unable to meet demand. Reliable climate projections are therefore critical to predicting the future water supply for the United States. These projections cannot be provided solely by global climate models (GCMs), however, as their resolution is too coarse to resol… Show more

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Cited by 1 publication
(2 citation statements)
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“…In this study, the watershed runoff model parameters were developed from Section 2. The runoff flows (hydrography) for the period 2040-2049 were calculated using downscaled meteorological data (Werth, 2011). The downscaling was performed using three GCMs i.e., the Goddard Institute of Space Studies (GISS) Model E, the Meteorological Research Institute (MRI) of Japan's model, and the Canadian Climate Center (CCC) model to provide hourly precipitation and temperature data for NWS Dalton, GA, Jasper, GA and Rome, GA.…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…In this study, the watershed runoff model parameters were developed from Section 2. The runoff flows (hydrography) for the period 2040-2049 were calculated using downscaled meteorological data (Werth, 2011). The downscaling was performed using three GCMs i.e., the Goddard Institute of Space Studies (GISS) Model E, the Meteorological Research Institute (MRI) of Japan's model, and the Canadian Climate Center (CCC) model to provide hourly precipitation and temperature data for NWS Dalton, GA, Jasper, GA and Rome, GA.…”
Section: Resultsmentioning
confidence: 99%
“…The process for this study is discussed in two reports. In the first report (Part 1), future weather conditions are predicted by using a statistical technique to downscale future climate produced by Global Climate Models (GCMs) to a regional/local area (Werth, 2011). This second part (Part 2) estimates the watershed runoff flow based on the future climate generated in Part 1.…”
Section: Introductionmentioning
confidence: 99%