Simulating and Evaluating Atmospheric River‐Induced Precipitation Extremes Along the U.S. Pacific Coast: Case Studies From 1980–2017
Atmospheric rivers (ARs) are responsible for a majority of extreme precipitation and flood events along the U.S. West Coast. To better understand the present‐day characteristics of AR‐related precipitation extremes, a selection of nine most intense historical AR events during 1980–2017 is simulated...
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Veröffentlicht in: | Journal of geophysical research. Atmospheres 2020-02, Vol.125 (4), p.n/a |
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description | Atmospheric rivers (ARs) are responsible for a majority of extreme precipitation and flood events along the U.S. West Coast. To better understand the present‐day characteristics of AR‐related precipitation extremes, a selection of nine most intense historical AR events during 1980–2017 is simulated using a dynamical downscaling modeling framework based on the Weather Research and Forecasting Model. We find that the chosen framework and Weather Research and Forecasting Model configuration reproduces both large‐scale atmospheric features—including parent synoptic‐scale cyclones—as well as the filamentary corridors of integrated vapor transport associated with the ARs themselves. The accuracy of simulated extreme precipitation maxima, relative to in situ and interpolated gridded observations, improves notably with increasing model resolution, with improvements as large as 40–60% for fine scale (3 km) relative to coarse‐scale (27 km) simulations. A separate set of simulations using smoothed topography suggests that much of these gains stem from the improved representation of complex terrain. Additionally, using the 12 December 1995 storm in Northern California as an example, we demonstrate that only the highest‐resolution simulations resolve important fine‐scale features—such as localized orographically forced vertical motion and powerful near hurricane‐force boundary layer winds. Given the demonstrated ability of a targeted dynamical downscaling framework to capture both local extreme precipitation and key fine‐scale characteristics of the most intense ARs in the historical record, we argue that such a configuration may be highly conducive to understanding AR‐related extremes and associated changes in a warming climate.
Key Points
High‐resolution modeling captures key physical characteristics of extreme atmospheric rivers
Fine scale is needed to well reproduce precipitation extremes and associated meteorological features
Targeted simulations can advance the studying of atmospheric rivers changes to a warming climate |
doi_str_mv | 10.1029/2019JD031554 |
format | Article |
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Key Points
High‐resolution modeling captures key physical characteristics of extreme atmospheric rivers
Fine scale is needed to well reproduce precipitation extremes and associated meteorological features
Targeted simulations can advance the studying of atmospheric rivers changes to a warming climate</description><identifier>ISSN: 2169-897X</identifier><identifier>EISSN: 2169-8996</identifier><identifier>DOI: 10.1029/2019JD031554</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Atmospheric models ; Boundary layer winds ; Boundary layers ; Climate change ; Climate models ; Computer simulation ; Configurations ; Cyclones ; Extreme weather ; Frameworks ; Geophysics ; Global warming ; Hurricanes ; Precipitation ; Resolution ; Simulation ; Storms ; Transportation corridors ; Vertical motion ; Weather forecasting ; Winds</subject><ispartof>Journal of geophysical research. Atmospheres, 2020-02, Vol.125 (4), p.n/a</ispartof><rights>2020. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3723-9b567a7c5716eccfdc550ea0b0871c84a69064859ec6ab52f0e1559d3d9f453e3</citedby><cites>FETCH-LOGICAL-c3723-9b567a7c5716eccfdc550ea0b0871c84a69064859ec6ab52f0e1559d3d9f453e3</cites><orcidid>0000-0003-4973-8500 ; 0000-0003-4276-3092 ; 0000-0002-1223-8521 ; 0000-0003-2494-9897 ; 0000000342763092 ; 0000000324949897 ; 0000000349738500 ; 0000000212238521</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2019JD031554$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2019JD031554$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>230,314,776,780,881,1411,1427,27903,27904,45553,45554,46387,46811</link.rule.ids><backlink>$$Uhttps://www.osti.gov/biblio/1599527$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Huang, Xingying</creatorcontrib><creatorcontrib>Swain, Daniel L.</creatorcontrib><creatorcontrib>Walton, Daniel B.</creatorcontrib><creatorcontrib>Stevenson, Samantha</creatorcontrib><creatorcontrib>Hall, Alex D.</creatorcontrib><title>Simulating and Evaluating Atmospheric River‐Induced Precipitation Extremes Along the U.S. Pacific Coast: Case Studies From 1980–2017</title><title>Journal of geophysical research. Atmospheres</title><description>Atmospheric rivers (ARs) are responsible for a majority of extreme precipitation and flood events along the U.S. West Coast. To better understand the present‐day characteristics of AR‐related precipitation extremes, a selection of nine most intense historical AR events during 1980–2017 is simulated using a dynamical downscaling modeling framework based on the Weather Research and Forecasting Model. We find that the chosen framework and Weather Research and Forecasting Model configuration reproduces both large‐scale atmospheric features—including parent synoptic‐scale cyclones—as well as the filamentary corridors of integrated vapor transport associated with the ARs themselves. The accuracy of simulated extreme precipitation maxima, relative to in situ and interpolated gridded observations, improves notably with increasing model resolution, with improvements as large as 40–60% for fine scale (3 km) relative to coarse‐scale (27 km) simulations. A separate set of simulations using smoothed topography suggests that much of these gains stem from the improved representation of complex terrain. Additionally, using the 12 December 1995 storm in Northern California as an example, we demonstrate that only the highest‐resolution simulations resolve important fine‐scale features—such as localized orographically forced vertical motion and powerful near hurricane‐force boundary layer winds. Given the demonstrated ability of a targeted dynamical downscaling framework to capture both local extreme precipitation and key fine‐scale characteristics of the most intense ARs in the historical record, we argue that such a configuration may be highly conducive to understanding AR‐related extremes and associated changes in a warming climate.
Key Points
High‐resolution modeling captures key physical characteristics of extreme atmospheric rivers
Fine scale is needed to well reproduce precipitation extremes and associated meteorological features
Targeted simulations can advance the studying of atmospheric rivers changes to a warming climate</description><subject>Atmospheric models</subject><subject>Boundary layer winds</subject><subject>Boundary layers</subject><subject>Climate change</subject><subject>Climate models</subject><subject>Computer simulation</subject><subject>Configurations</subject><subject>Cyclones</subject><subject>Extreme weather</subject><subject>Frameworks</subject><subject>Geophysics</subject><subject>Global warming</subject><subject>Hurricanes</subject><subject>Precipitation</subject><subject>Resolution</subject><subject>Simulation</subject><subject>Storms</subject><subject>Transportation corridors</subject><subject>Vertical motion</subject><subject>Weather forecasting</subject><subject>Winds</subject><issn>2169-897X</issn><issn>2169-8996</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp90c1KxDAQAOAiCop68wGCXt01aZq08bas6x-C4ip4C9l06kbaZk3SVW8ePQq-oU9ipCKezGUy8M0wzCTJDsFDglNxkGIizo8wJYxlK8lGSrgYFELw1d9_freebHv_gOMrMM1YtpG8TU3T1SqY9h6ptkSTpaq7Ph2FxvrFHJzR6NoswX2-vp-1ZaehRFcOtFmYEKVt0eQ5OGjAo1FtY2GYA7odTofoSmlTxeqxVT4corHygKahK02kx842iIgCf75-xNHzrWStUrWH7Z-4mdweT27Gp4OLy5Oz8ehioGme0oGYMZ6rXLOccNC6KjVjGBSe4SInusgUF5hnBROguZqxtMIQFyJKWooqYxToZrLb97U-GOm1CaDn2rYt6CAJE4KleUR7PVo4-9iBD_LBdq6Nc8mUckpoJrCIar9X2lnvHVRy4Uyj3IskWH7fRP69SeS050-mhpd_rTw_uT5iHGeUfgFdFI1B</recordid><startdate>20200227</startdate><enddate>20200227</enddate><creator>Huang, Xingying</creator><creator>Swain, Daniel L.</creator><creator>Walton, Daniel B.</creator><creator>Stevenson, Samantha</creator><creator>Hall, Alex D.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union (AGU)</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><scope>OTOTI</scope><orcidid>https://orcid.org/0000-0003-4973-8500</orcidid><orcidid>https://orcid.org/0000-0003-4276-3092</orcidid><orcidid>https://orcid.org/0000-0002-1223-8521</orcidid><orcidid>https://orcid.org/0000-0003-2494-9897</orcidid><orcidid>https://orcid.org/0000000342763092</orcidid><orcidid>https://orcid.org/0000000324949897</orcidid><orcidid>https://orcid.org/0000000349738500</orcidid><orcidid>https://orcid.org/0000000212238521</orcidid></search><sort><creationdate>20200227</creationdate><title>Simulating and Evaluating Atmospheric River‐Induced Precipitation Extremes Along the U.S. Pacific Coast: Case Studies From 1980–2017</title><author>Huang, Xingying ; Swain, Daniel L. ; Walton, Daniel B. ; Stevenson, Samantha ; Hall, Alex D.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3723-9b567a7c5716eccfdc550ea0b0871c84a69064859ec6ab52f0e1559d3d9f453e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Atmospheric models</topic><topic>Boundary layer winds</topic><topic>Boundary layers</topic><topic>Climate change</topic><topic>Climate models</topic><topic>Computer simulation</topic><topic>Configurations</topic><topic>Cyclones</topic><topic>Extreme weather</topic><topic>Frameworks</topic><topic>Geophysics</topic><topic>Global warming</topic><topic>Hurricanes</topic><topic>Precipitation</topic><topic>Resolution</topic><topic>Simulation</topic><topic>Storms</topic><topic>Transportation corridors</topic><topic>Vertical motion</topic><topic>Weather forecasting</topic><topic>Winds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Huang, Xingying</creatorcontrib><creatorcontrib>Swain, Daniel L.</creatorcontrib><creatorcontrib>Walton, Daniel B.</creatorcontrib><creatorcontrib>Stevenson, Samantha</creatorcontrib><creatorcontrib>Hall, Alex D.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>OSTI.GOV</collection><jtitle>Journal of geophysical research. Atmospheres</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Huang, Xingying</au><au>Swain, Daniel L.</au><au>Walton, Daniel B.</au><au>Stevenson, Samantha</au><au>Hall, Alex D.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Simulating and Evaluating Atmospheric River‐Induced Precipitation Extremes Along the U.S. Pacific Coast: Case Studies From 1980–2017</atitle><jtitle>Journal of geophysical research. Atmospheres</jtitle><date>2020-02-27</date><risdate>2020</risdate><volume>125</volume><issue>4</issue><epage>n/a</epage><issn>2169-897X</issn><eissn>2169-8996</eissn><abstract>Atmospheric rivers (ARs) are responsible for a majority of extreme precipitation and flood events along the U.S. West Coast. To better understand the present‐day characteristics of AR‐related precipitation extremes, a selection of nine most intense historical AR events during 1980–2017 is simulated using a dynamical downscaling modeling framework based on the Weather Research and Forecasting Model. We find that the chosen framework and Weather Research and Forecasting Model configuration reproduces both large‐scale atmospheric features—including parent synoptic‐scale cyclones—as well as the filamentary corridors of integrated vapor transport associated with the ARs themselves. The accuracy of simulated extreme precipitation maxima, relative to in situ and interpolated gridded observations, improves notably with increasing model resolution, with improvements as large as 40–60% for fine scale (3 km) relative to coarse‐scale (27 km) simulations. A separate set of simulations using smoothed topography suggests that much of these gains stem from the improved representation of complex terrain. Additionally, using the 12 December 1995 storm in Northern California as an example, we demonstrate that only the highest‐resolution simulations resolve important fine‐scale features—such as localized orographically forced vertical motion and powerful near hurricane‐force boundary layer winds. Given the demonstrated ability of a targeted dynamical downscaling framework to capture both local extreme precipitation and key fine‐scale characteristics of the most intense ARs in the historical record, we argue that such a configuration may be highly conducive to understanding AR‐related extremes and associated changes in a warming climate.
Key Points
High‐resolution modeling captures key physical characteristics of extreme atmospheric rivers
Fine scale is needed to well reproduce precipitation extremes and associated meteorological features
Targeted simulations can advance the studying of atmospheric rivers changes to a warming climate</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2019JD031554</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0003-4973-8500</orcidid><orcidid>https://orcid.org/0000-0003-4276-3092</orcidid><orcidid>https://orcid.org/0000-0002-1223-8521</orcidid><orcidid>https://orcid.org/0000-0003-2494-9897</orcidid><orcidid>https://orcid.org/0000000342763092</orcidid><orcidid>https://orcid.org/0000000324949897</orcidid><orcidid>https://orcid.org/0000000349738500</orcidid><orcidid>https://orcid.org/0000000212238521</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Atmospheric models Boundary layer winds Boundary layers Climate change Climate models Computer simulation Configurations Cyclones Extreme weather Frameworks Geophysics Global warming Hurricanes Precipitation Resolution Simulation Storms Transportation corridors Vertical motion Weather forecasting Winds |
title | Simulating and Evaluating Atmospheric River‐Induced Precipitation Extremes Along the U.S. Pacific Coast: Case Studies From 1980–2017 |
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