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Title: Interactions between Climate Change and Complex Topography Drive Observed Streamflow Changes in the Colorado River Basin

Abstract

Abstract The Colorado River basin (CRB) is one of the most important watersheds for energy, water, and food security in the United States. CRB water supports 15% of U.S. food production, more than 50 GW of electricity capacity, and one of the fastest growing populations in the United States. Energy–water–food nexus impacts from climate change are projected to increase in the CRB. These include a higher incidence of extreme events, widespread snow-to-rain regime shifts, and a higher frequency and magnitude of climate-driven disturbances. Here, we empirically show how the historical annual streamflow maximum and hydrograph centroid timing relate to temperature, precipitation, and snow. In addition, we show how these hydroclimatic relationships vary with elevation and how the elevation dependence has changed over this historical observational record. We find temperature and precipitation have a relatively weak relation (|r| < 0.3) to interannual variations in streamflow timing and extremes at low elevations (<1500 m), but a relatively strong relation (|r| > 0.5) at high elevations (>2300 m) where more snow occurs in the CRB. The threshold elevation where this relationship is strongest (|r| > 0.5) is moving uphill at a rate of up to 4.8 m yr−1 (p = 0.11) and 6.1more » m yr−1 (p = 0.01) for temperature and precipitation, respectively. Based on these findings, we hypothesize where warming and precipitation-related streamflow changes are likely to be most severe using a watershed-scale vulnerability map to prioritize areas for further research and to inform energy, water, and food resource management in the CRB.« less

Authors:
 [1];  [1];  [2];  [3];  [1];  [1]
  1. Los Alamos National Laboratory, Los Alamos, New Mexico
  2. White Rabbit R&D LLC, and Oregon State University, Corvallis, Oregon, and University of British Columbia, Vancouver, British Columbia, Canada, and Los Alamos National Laboratory, Los Alamos, New Mexico
  3. Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico
Publication Date:
Research Org.:
Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
Sponsoring Org.:
USDOE; LANL Laboratory Directed Research and Development (LDRD) Program
OSTI Identifier:
1580197
Alternate Identifier(s):
OSTI ID: 1511224
Report Number(s):
LA-UR-17-27512
Journal ID: ISSN 1525-755X
Grant/Contract Number:  
20150397DR; 89233218CNA000001
Resource Type:
Published Article
Journal Name:
Journal of Hydrometeorology
Additional Journal Information:
Journal Name: Journal of Hydrometeorology Journal Volume: 19 Journal Issue: 10; Journal ID: ISSN 1525-755X
Publisher:
American Meteorological Society
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; climate change; hydrology; hydrometeorology; regression analysis; time series; climate variability

Citation Formats

Solander, Kurt C., Bennett, Katrina E., Fleming, Sean W., Gutzler, David S., Hopkins, Emily M., and Middleton, Richard S. Interactions between Climate Change and Complex Topography Drive Observed Streamflow Changes in the Colorado River Basin. United States: N. p., 2018. Web. doi:10.1175/JHM-D-18-0012.1.
Solander, Kurt C., Bennett, Katrina E., Fleming, Sean W., Gutzler, David S., Hopkins, Emily M., & Middleton, Richard S. Interactions between Climate Change and Complex Topography Drive Observed Streamflow Changes in the Colorado River Basin. United States. https://doi.org/10.1175/JHM-D-18-0012.1
Solander, Kurt C., Bennett, Katrina E., Fleming, Sean W., Gutzler, David S., Hopkins, Emily M., and Middleton, Richard S. Fri . "Interactions between Climate Change and Complex Topography Drive Observed Streamflow Changes in the Colorado River Basin". United States. https://doi.org/10.1175/JHM-D-18-0012.1.
@article{osti_1580197,
title = {Interactions between Climate Change and Complex Topography Drive Observed Streamflow Changes in the Colorado River Basin},
author = {Solander, Kurt C. and Bennett, Katrina E. and Fleming, Sean W. and Gutzler, David S. and Hopkins, Emily M. and Middleton, Richard S.},
abstractNote = {Abstract The Colorado River basin (CRB) is one of the most important watersheds for energy, water, and food security in the United States. CRB water supports 15% of U.S. food production, more than 50 GW of electricity capacity, and one of the fastest growing populations in the United States. Energy–water–food nexus impacts from climate change are projected to increase in the CRB. These include a higher incidence of extreme events, widespread snow-to-rain regime shifts, and a higher frequency and magnitude of climate-driven disturbances. Here, we empirically show how the historical annual streamflow maximum and hydrograph centroid timing relate to temperature, precipitation, and snow. In addition, we show how these hydroclimatic relationships vary with elevation and how the elevation dependence has changed over this historical observational record. We find temperature and precipitation have a relatively weak relation (|r| < 0.3) to interannual variations in streamflow timing and extremes at low elevations (<1500 m), but a relatively strong relation (|r| > 0.5) at high elevations (>2300 m) where more snow occurs in the CRB. The threshold elevation where this relationship is strongest (|r| > 0.5) is moving uphill at a rate of up to 4.8 m yr−1 (p = 0.11) and 6.1 m yr−1 (p = 0.01) for temperature and precipitation, respectively. Based on these findings, we hypothesize where warming and precipitation-related streamflow changes are likely to be most severe using a watershed-scale vulnerability map to prioritize areas for further research and to inform energy, water, and food resource management in the CRB.},
doi = {10.1175/JHM-D-18-0012.1},
journal = {Journal of Hydrometeorology},
number = 10,
volume = 19,
place = {United States},
year = {Fri Oct 19 00:00:00 EDT 2018},
month = {Fri Oct 19 00:00:00 EDT 2018}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record
https://doi.org/10.1175/JHM-D-18-0012.1

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Cited by: 2 works
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Figures / Tables:

Figure 1 Figure 1: Map of the Colorado River Basin showing the streamflow gages that were used in the analysis with corresponding record length of 30-years (1985-2014), 40-years (1975-2014), 50- years (1965-2014) and 60-years (1955-2014). White borders show boundaries of HUC-4 watersheds located within the basin.

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