THE ROLE OF CLIMATE VARIABILITY IN OPERATIONAL WATER SUPPLY FORECASTING FOR THE WESTERN UNITED STATES

The single greatest uncertainty in seasonal water supply forecasts is the amount of precipitation falling after the forecast issue date. There has been a long history of attempting to incorporate seasonal climate forecasts into operational water supply forecasts. The skill of these precipitation for...

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Main Author: Pagano, Thomas Christopher
Other Authors: Sorooshian, Soroosh
Language:EN
Published: The University of Arizona. 2005
Subjects:
Online Access:http://hdl.handle.net/10150/194261
http://arizona.openrepository.com/arizona/handle/10150/194261
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spelling ndltd-arizona.edu-oai-arizona.openrepository.com-10150-1942612017-09-10T03:00:26Z THE ROLE OF CLIMATE VARIABILITY IN OPERATIONAL WATER SUPPLY FORECASTING FOR THE WESTERN UNITED STATES Pagano, Thomas Christopher Pagano, Thomas Christopher Sorooshian, Soroosh Sorooshian, Soroosh Valdez, Juan Shuttleworth, James Davis, Don Mullen, Steven Water Forecasting El Nino Climatology Hydroclimatology The single greatest uncertainty in seasonal water supply forecasts is the amount of precipitation falling after the forecast issue date. There has been a long history of attempting to incorporate seasonal climate forecasts into operational water supply forecasts. The skill of these precipitation forecasts remains low especially compared to highly confident snow-based streamflow forecasts. Early in the season (e.g., September-December), however, large-scale climate indices are the best available predictors of future water supplies. This dissertation suggests practical methods for issuing climate-based operational streamflow forecasts.This study also documents the existence of strong decadal trends in water supply forecast skill. Across the Western US, 1 April forecast skill peaked in the 1960-1970s and has been on the decline more recently. The high skill period was a very calm period in the Western US, with a near absence of extreme (wet or dry) spring precipitation events. In contrast, the period after 1980 has had the most variable, persistent, and skewed spring and summer streamflows in the modern record. Spring precipitation is also now more variable than it has been since at least the 1930s. This rise in spring precipitation variability in the Colorado/Rio Grande Basins and the Pacific Northwest is the likely cause behind the recent decline in water supply forecast skill. 2005 text Electronic Dissertation http://hdl.handle.net/10150/194261 http://arizona.openrepository.com/arizona/handle/10150/194261 137353541 1022 EN Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. The University of Arizona.
collection NDLTD
language EN
sources NDLTD
topic Water
Forecasting
El Nino
Climatology
Hydroclimatology
spellingShingle Water
Forecasting
El Nino
Climatology
Hydroclimatology
Pagano, Thomas Christopher
Pagano, Thomas Christopher
THE ROLE OF CLIMATE VARIABILITY IN OPERATIONAL WATER SUPPLY FORECASTING FOR THE WESTERN UNITED STATES
description The single greatest uncertainty in seasonal water supply forecasts is the amount of precipitation falling after the forecast issue date. There has been a long history of attempting to incorporate seasonal climate forecasts into operational water supply forecasts. The skill of these precipitation forecasts remains low especially compared to highly confident snow-based streamflow forecasts. Early in the season (e.g., September-December), however, large-scale climate indices are the best available predictors of future water supplies. This dissertation suggests practical methods for issuing climate-based operational streamflow forecasts.This study also documents the existence of strong decadal trends in water supply forecast skill. Across the Western US, 1 April forecast skill peaked in the 1960-1970s and has been on the decline more recently. The high skill period was a very calm period in the Western US, with a near absence of extreme (wet or dry) spring precipitation events. In contrast, the period after 1980 has had the most variable, persistent, and skewed spring and summer streamflows in the modern record. Spring precipitation is also now more variable than it has been since at least the 1930s. This rise in spring precipitation variability in the Colorado/Rio Grande Basins and the Pacific Northwest is the likely cause behind the recent decline in water supply forecast skill.
author2 Sorooshian, Soroosh
author_facet Sorooshian, Soroosh
Pagano, Thomas Christopher
Pagano, Thomas Christopher
author Pagano, Thomas Christopher
Pagano, Thomas Christopher
author_sort Pagano, Thomas Christopher
title THE ROLE OF CLIMATE VARIABILITY IN OPERATIONAL WATER SUPPLY FORECASTING FOR THE WESTERN UNITED STATES
title_short THE ROLE OF CLIMATE VARIABILITY IN OPERATIONAL WATER SUPPLY FORECASTING FOR THE WESTERN UNITED STATES
title_full THE ROLE OF CLIMATE VARIABILITY IN OPERATIONAL WATER SUPPLY FORECASTING FOR THE WESTERN UNITED STATES
title_fullStr THE ROLE OF CLIMATE VARIABILITY IN OPERATIONAL WATER SUPPLY FORECASTING FOR THE WESTERN UNITED STATES
title_full_unstemmed THE ROLE OF CLIMATE VARIABILITY IN OPERATIONAL WATER SUPPLY FORECASTING FOR THE WESTERN UNITED STATES
title_sort role of climate variability in operational water supply forecasting for the western united states
publisher The University of Arizona.
publishDate 2005
url http://hdl.handle.net/10150/194261
http://arizona.openrepository.com/arizona/handle/10150/194261
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