Projections of Potential Flood Regime Changes in California

Floods have been a recurring theme in California’s climatology, hydrology, and politics throughout its history. Today, California's aging water supply and flood protection infrastructures are challenged by major floods and increased standards for urban flood protection. With warming in the twenty-fi...

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Authors: Dettinger, Michael D.; Hidalgo León, Hugo G.; Das, Tapash; Cayan, Daniel R.; Knowles, Noah
Format: Report
Publication date:2009
Country:Costa Rica
Institution:UCR
Repository:Kérwá
OAI Identifier:oai:kerwa.ucr.ac.cr:10669/29857
Online Access:http://www.energy.ca.gov/2009publications/CEC-500-2009-050/CEC-500-2009-050-D.PDF
https://hdl.handle.net/10669/29857
Access Level:Open access
Keyword:California
Floods
Climate Change
Hydrologic change
Simulations
Atmospheric rivers
Sea-level rise
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author Dettinger, Michael D.
author2 Hidalgo León, Hugo G.
Das, Tapash
Cayan, Daniel R.
Knowles, Noah
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author_browse Cayan, Daniel R.
Das, Tapash
Dettinger, Michael D.
Hidalgo León, Hugo G.
Knowles, Noah
author_facet Dettinger, Michael D.
Hidalgo León, Hugo G.
Das, Tapash
Cayan, Daniel R.
Knowles, Noah
author_role author
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description Floods have been a recurring theme in California’s climatology, hydrology, and politics throughout its history. Today, California's aging water supply and flood protection infrastructures are challenged by major floods and increased standards for urban flood protection. With warming in the twenty-first century, some changes in California’s flood regimes seem likely: Higher snowlines may well increase the frequency of flooding; occasional larger than historical flood magnitudes are likely to follow—especially from the higher southern parts of the Sierra Nevada; potentials for floods may be exacerbated by wetter winter soils in high-altitude catchments; and opportunities for estuarine and coastal flooding may increase as sea-level rise and flood frequencies converge. Other changes are more difficult to project, and simulation models are used here to weigh competing influences that might either increase or diminish future floods. Both the Variable Infiltration Capacity (VIC) and Bay-Delta Watershed Model (BDWM) hydrologic models responded to downscaled climate-change projections with increases in flood frequencies and magnitudes, but neither yielded large changes in that regard, especially in the northern parts of the state. Future characteristics of major storms, in particular pineapple express or atmospheric river storms, by global climate models indicated changes mostly at the extremes: Years with many atmospheric river storms become more frequent in most climate models analyzed here, but the average number of such storms per year did not change much. Likewise, although the average intensity of storms was not projected to increase much in most climate models, occasional much-larger-than-historical-range storm intensities were simulated
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spelling Projections of Potential Flood Regime Changes in California Dettinger, Michael D. Hidalgo León, Hugo G. Das, Tapash Cayan, Daniel R. Knowles, Noah California Floods Climate Change Hydrologic change Simulations Atmospheric rivers Sea-level rise Floods have been a recurring theme in California’s climatology, hydrology, and politics throughout its history. Today, California's aging water supply and flood protection infrastructures are challenged by major floods and increased standards for urban flood protection. With warming in the twenty-first century, some changes in California’s flood regimes seem likely: Higher snowlines may well increase the frequency of flooding; occasional larger than historical flood magnitudes are likely to follow—especially from the higher southern parts of the Sierra Nevada; potentials for floods may be exacerbated by wetter winter soils in high-altitude catchments; and opportunities for estuarine and coastal flooding may increase as sea-level rise and flood frequencies converge. Other changes are more difficult to project, and simulation models are used here to weigh competing influences that might either increase or diminish future floods. Both the Variable Infiltration Capacity (VIC) and Bay-Delta Watershed Model (BDWM) hydrologic models responded to downscaled climate-change projections with increases in flood frequencies and magnitudes, but neither yielded large changes in that regard, especially in the northern parts of the state. Future characteristics of major storms, in particular pineapple express or atmospheric river storms, by global climate models indicated changes mostly at the extremes: Years with many atmospheric river storms become more frequent in most climate models analyzed here, but the average number of such storms per year did not change much. Likewise, although the average intensity of storms was not projected to increase much in most climate models, occasional much-larger-than-historical-range storm intensities were simulated California Energy Commissionfunded California Climate Change Center, United States CALFED Bay-Delta Program-funded Computational Assessments of Scenarios of Change in the Delta Ecosystem (CASCaDE) Project, California, United States Universidad de Costa Rica//UCR/Costa Rica UCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias Básicas::Centro de Investigaciones Geofísicas (CIGEFI) http://www.energy.ca.gov/2009publications/CEC-500-2009-050/CEC-500-2009-050-D.PDF CEC-500-2009-050-D https://hdl.handle.net/10669/29857
spellingShingle Projections of Potential Flood Regime Changes in California
Dettinger, Michael D.
California
Floods
Climate Change
Hydrologic change
Simulations
Atmospheric rivers
Sea-level rise
title Projections of Potential Flood Regime Changes in California
title_full Projections of Potential Flood Regime Changes in California
title_fullStr Projections of Potential Flood Regime Changes in California
title_full_unstemmed Projections of Potential Flood Regime Changes in California
title_short Projections of Potential Flood Regime Changes in California
title_sort Projections of Potential Flood Regime Changes in California
topic California
Floods
Climate Change
Hydrologic change
Simulations
Atmospheric rivers
Sea-level rise
topic_facet California
Floods
Climate Change
Hydrologic change
Simulations
Atmospheric rivers
Sea-level rise
url http://www.energy.ca.gov/2009publications/CEC-500-2009-050/CEC-500-2009-050-D.PDF
https://hdl.handle.net/10669/29857