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Title: The Water‐Year Water Balance of the Colorado River Basin

Abstract

Abstract Model‐estimated monthly water balance components (i.e., potential evapotranspiration, actual evapotranspiration, and runoff ( R )) for 146 United States (U.S.) Geological Survey 8‐digit hydrologic units located in the Colorado River Basin (CRB) are used to examine the temporal and spatial variability of the CRB water balance for water years 1901 through 2014 (a water year is the period from October 1 of one year through September 30 of the following year). Results indicate that the CRB can be divided into six subregions with similar temporal variability in monthly R . The water balance analyses indicated that approximately 75% of total water‐year R is generated by just one CRB subregion and that most of the R in the basin is derived from surplus ( S ) water generated during the months of October through April. Furthermore, the analyses show that temporal variability in S is largely controlled by the occurrence of negative atmospheric pressure anomalies over the northwestern conterminous U.S. (CONUS) and positive atmospheric pressure anomalies over the southeastern CONUS. This combination of atmospheric pressure anomalies results in an anomalous flow of moist air from the North Pacific Ocean into the CRB, particularly the Upper CRB. Additionally, the occurrence ofmore » extreme dry and wet periods in the CRB appears to be related to variability of the Atlantic Multidecadal Oscillation and the Pacific Decadal Oscillation.« less

Authors:
 [1];  [2]
  1. U.S. Geological Survey Denver Colorado USA
  2. U.S. Geological Survey Lawrence Kansas USA
Publication Date:
Sponsoring Org.:
USDOE
OSTI Identifier:
1630254
Resource Type:
Publisher's Accepted Manuscript
Journal Name:
Journal of the American Water Resources Association
Additional Journal Information:
Journal Name: Journal of the American Water Resources Association Journal Volume: 56 Journal Issue: 4; Journal ID: ISSN 1093-474X
Publisher:
Wiley-Blackwell
Country of Publication:
United States
Language:
English

Citation Formats

McCabe, Gregory J., and Wolock, David M. The Water‐Year Water Balance of the Colorado River Basin. United States: N. p., 2020. Web. doi:10.1111/1752-1688.12848.
McCabe, Gregory J., & Wolock, David M. The Water‐Year Water Balance of the Colorado River Basin. United States. https://doi.org/10.1111/1752-1688.12848
McCabe, Gregory J., and Wolock, David M. Wed . "The Water‐Year Water Balance of the Colorado River Basin". United States. https://doi.org/10.1111/1752-1688.12848.
@article{osti_1630254,
title = {The Water‐Year Water Balance of the Colorado River Basin},
author = {McCabe, Gregory J. and Wolock, David M.},
abstractNote = {Abstract Model‐estimated monthly water balance components (i.e., potential evapotranspiration, actual evapotranspiration, and runoff ( R )) for 146 United States (U.S.) Geological Survey 8‐digit hydrologic units located in the Colorado River Basin (CRB) are used to examine the temporal and spatial variability of the CRB water balance for water years 1901 through 2014 (a water year is the period from October 1 of one year through September 30 of the following year). Results indicate that the CRB can be divided into six subregions with similar temporal variability in monthly R . The water balance analyses indicated that approximately 75% of total water‐year R is generated by just one CRB subregion and that most of the R in the basin is derived from surplus ( S ) water generated during the months of October through April. Furthermore, the analyses show that temporal variability in S is largely controlled by the occurrence of negative atmospheric pressure anomalies over the northwestern conterminous U.S. (CONUS) and positive atmospheric pressure anomalies over the southeastern CONUS. This combination of atmospheric pressure anomalies results in an anomalous flow of moist air from the North Pacific Ocean into the CRB, particularly the Upper CRB. Additionally, the occurrence of extreme dry and wet periods in the CRB appears to be related to variability of the Atlantic Multidecadal Oscillation and the Pacific Decadal Oscillation.},
doi = {10.1111/1752-1688.12848},
journal = {Journal of the American Water Resources Association},
number = 4,
volume = 56,
place = {United States},
year = {Wed May 20 00:00:00 EDT 2020},
month = {Wed May 20 00:00:00 EDT 2020}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record
https://doi.org/10.1111/1752-1688.12848

Citation Metrics:
Cited by: 8 works
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