TY - JOUR
T1 - Upper Colorado River Basin 20th century droughts under 21st century warming
T2 - Plausible scenarios for the future
AU - Woodhouse, Connie A.
AU - Smith, Rebecca M.
AU - McAfee, Stephanie A.
AU - Pederson, Gregory T.
AU - McCabe, Gregory J.
AU - Miller, W. Paul
AU - Csank, Adam
N1 - Funding Information:
We thank our water manager partners from Denver Water, Southern Nevada Water Authority, Bureau of Reclamation, Colorado River District, and Salt River Project who have been the driving force in this study. We also appreciate the comments and suggestions of Jeremy Littell and two anonymous reviewers who helped us improve the quality of the paper. This research was funded by the Department of the Interior Southwest Climate Adaptation Science Center. The project described in this publication was supported by Grant No. G17AP00099 from the U.S. Geological Survey. Its contents are those of the authors and do not necessarily represent the views of the Southwest Climate Adaptation Science Center. This article has been peer reviewed and approved for publication consistent with USGS Fundamental Science Practices (https://pubs.usgs.gov/circ/1367/). This manuscript is submitted for publication with the understanding that the U.S. Government is authorized to reproduce and distribute reprints for Governmental purposes. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
Publisher Copyright:
© 2020 The Author(s)
PY - 2021/1
Y1 - 2021/1
N2 - This study builds on a collaboration with a water resource management community of practice in the Upper Colorado River Basin to develop scenarios of future drought and assess impacts on water supply reliability. Water managers are concerned with the impacts of warming on water year streamflow, but uncertainties in projections of climate make the application of these projections to planning a challenge. Instead, water managers considered a plausible scenario for future drought to be historical droughts to which warming is added. We used a simple statistical model of water year streamflow with temperatures increased by 1 °C to 4 °C, and then examined reductions in flow and runoff efficiency (RE) with each degree of warming for the six droughts defined in the observed streamflow record. In order to place these results into a management context, we employed an existing framework for system reliability, and in particular, a vulnerability assessment for water delivery metrics. Using modeled streamflow resulting from 1 °C to 4 °C warming, we found vulnerable condition thresholds for the two water delivery metrics assessed, Upper Basin Shortage and Lees Ferry Deficit, were crossed relatively infrequently at +1 °C, but with a substantially increased frequency under additional warming. Results are more relevant to resource management because the impacts of warming on Upper Colorado River streamflow were assessed in the context of management metrics and vulnerability thresholds, in collaboration with members of the water management community of practice.
AB - This study builds on a collaboration with a water resource management community of practice in the Upper Colorado River Basin to develop scenarios of future drought and assess impacts on water supply reliability. Water managers are concerned with the impacts of warming on water year streamflow, but uncertainties in projections of climate make the application of these projections to planning a challenge. Instead, water managers considered a plausible scenario for future drought to be historical droughts to which warming is added. We used a simple statistical model of water year streamflow with temperatures increased by 1 °C to 4 °C, and then examined reductions in flow and runoff efficiency (RE) with each degree of warming for the six droughts defined in the observed streamflow record. In order to place these results into a management context, we employed an existing framework for system reliability, and in particular, a vulnerability assessment for water delivery metrics. Using modeled streamflow resulting from 1 °C to 4 °C warming, we found vulnerable condition thresholds for the two water delivery metrics assessed, Upper Basin Shortage and Lees Ferry Deficit, were crossed relatively infrequently at +1 °C, but with a substantially increased frequency under additional warming. Results are more relevant to resource management because the impacts of warming on Upper Colorado River streamflow were assessed in the context of management metrics and vulnerability thresholds, in collaboration with members of the water management community of practice.
KW - Climate warming
KW - Drought
KW - Runoff efficiency
KW - Streamflow
KW - Upper Colorado River Basin
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U2 - 10.1016/j.cliser.2020.100206
DO - 10.1016/j.cliser.2020.100206
M3 - Article
AN - SCOPUS:85099514158
SN - 2405-8807
VL - 21
JO - Climate Services
JF - Climate Services
M1 - 100206
ER -