Relationships between Gulf of California Moisture Surges and Tropical Cyclones in the Eastern Pacific Basin
Relationships between Gulf of California moisture surges and tropical cyclones (TCs) in the eastern Pacific basin are examined. Standard surface observations are used to identify gulf surge events at Yuma, Arizona, for a multiyear (July–August 1979–2001) period. The surges are related to TCs using N...
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| Veröffentlicht in: | Journal of climate 2005-11, Vol.18 (22), p.4601-4620 |
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| creator | Higgins, R. W. Shi, W. |
| description | Relationships between Gulf of California moisture surges and tropical cyclones (TCs) in the eastern Pacific basin are examined. Standard surface observations are used to identify gulf surge events at Yuma, Arizona, for a multiyear (July–August 1979–2001) period. The surges are related to TCs using National Hurricane Center 6-hourly track data for the eastern Pacific basin. Climate Prediction Center (CPC)-observed daily precipitation analyses and the NCEP Regional Reanalysis are used to examine the relative differences in the precipitation, atmospheric circulation, and moisture fields for several categories of surge events, including those that are directly related to TCs, indirectly related to TCs, and not related to TCs.
It is shown that the response to the surge in the southwestern United States and northwestern Mexico is strongly discriminated by the presence or absence of TCs. Surges related to TCs tend to be associated with much stronger and deeper low-level southerly flow, deeper plumes of tropical moisture, and wetter conditions over the core monsoon region than surges that are unrelated to TCs. The response to the surge is also strongly influenced by the proximity of the TC to the Gulf of California (GOC) region. Tropical cyclones that track toward the GOC region exert a stronger, more direct influence on Yuma surges than those that track away from the GOC. |
| doi_str_mv | 10.1175/JCLI3551.1 |
| format | Article |
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It is shown that the response to the surge in the southwestern United States and northwestern Mexico is strongly discriminated by the presence or absence of TCs. Surges related to TCs tend to be associated with much stronger and deeper low-level southerly flow, deeper plumes of tropical moisture, and wetter conditions over the core monsoon region than surges that are unrelated to TCs. The response to the surge is also strongly influenced by the proximity of the TC to the Gulf of California (GOC) region. Tropical cyclones that track toward the GOC region exert a stronger, more direct influence on Yuma surges than those that track away from the GOC.</description><identifier>ISSN: 0894-8755</identifier><identifier>EISSN: 1520-0442</identifier><identifier>DOI: 10.1175/JCLI3551.1</identifier><language>eng</language><publisher>Boston, MA: American Meteorological Society</publisher><subject>Atmospheric circulation ; Atmospheric moisture ; Climate ; Climate prediction ; Cyclones ; Daily precipitation ; Datasets ; Dew point ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Hurricane tracking ; Hurricanes ; Marine ; Meteorology ; Moisture ; Moisture effects ; Monsoons ; Plumes ; Precipitation ; Rain ; Sea level ; Storms, hurricanes, tornadoes, thunderstorms ; Surges ; Tropical cyclones ; Tropical regions ; Weather analysis and prediction ; Weather forecasting ; Wind</subject><ispartof>Journal of climate, 2005-11, Vol.18 (22), p.4601-4620</ispartof><rights>2005 American Meteorological Society</rights><rights>2006 INIST-CNRS</rights><rights>Copyright American Meteorological Society Nov 15, 2005</rights><rights>Copyright American Meteorological Society 2005</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c405t-35a779ccf20a457bc9879794eb09452e6a9de21b4d0d68f6a2cf210ea8eaa3483</citedby><cites>FETCH-LOGICAL-c405t-35a779ccf20a457bc9879794eb09452e6a9de21b4d0d68f6a2cf210ea8eaa3483</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/26253744$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/26253744$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,3668,27903,27904,57995,58228</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=17366535$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Higgins, R. W.</creatorcontrib><creatorcontrib>Shi, W.</creatorcontrib><title>Relationships between Gulf of California Moisture Surges and Tropical Cyclones in the Eastern Pacific Basin</title><title>Journal of climate</title><description>Relationships between Gulf of California moisture surges and tropical cyclones (TCs) in the eastern Pacific basin are examined. Standard surface observations are used to identify gulf surge events at Yuma, Arizona, for a multiyear (July–August 1979–2001) period. The surges are related to TCs using National Hurricane Center 6-hourly track data for the eastern Pacific basin. Climate Prediction Center (CPC)-observed daily precipitation analyses and the NCEP Regional Reanalysis are used to examine the relative differences in the precipitation, atmospheric circulation, and moisture fields for several categories of surge events, including those that are directly related to TCs, indirectly related to TCs, and not related to TCs.
It is shown that the response to the surge in the southwestern United States and northwestern Mexico is strongly discriminated by the presence or absence of TCs. Surges related to TCs tend to be associated with much stronger and deeper low-level southerly flow, deeper plumes of tropical moisture, and wetter conditions over the core monsoon region than surges that are unrelated to TCs. The response to the surge is also strongly influenced by the proximity of the TC to the Gulf of California (GOC) region. Tropical cyclones that track toward the GOC region exert a stronger, more direct influence on Yuma surges than those that track away from the GOC.</description><subject>Atmospheric circulation</subject><subject>Atmospheric moisture</subject><subject>Climate</subject><subject>Climate prediction</subject><subject>Cyclones</subject><subject>Daily precipitation</subject><subject>Datasets</subject><subject>Dew point</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Hurricane tracking</subject><subject>Hurricanes</subject><subject>Marine</subject><subject>Meteorology</subject><subject>Moisture</subject><subject>Moisture effects</subject><subject>Monsoons</subject><subject>Plumes</subject><subject>Precipitation</subject><subject>Rain</subject><subject>Sea level</subject><subject>Storms, hurricanes, tornadoes, thunderstorms</subject><subject>Surges</subject><subject>Tropical cyclones</subject><subject>Tropical regions</subject><subject>Weather analysis and prediction</subject><subject>Weather forecasting</subject><subject>Wind</subject><issn>0894-8755</issn><issn>1520-0442</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp10d9rFDEQB_AgFbxWX3wXQsU-FLYm2fzaR136S04Urc_LXG7S5twmZ7JL6X9vyrUKgk-BySdfZjKEvObshHOj3n_ql5etUvyEPyMLrgRrmJRijyyY7WRjjVIvyH4pG8a40IwtyM9vOMIUUiw3YVvoCqc7xEjP59HT5GkPY_ApxwD0cwplmjPS73O-xkIhrulVTtvgYKT9vRtTrNUQ6XSD9BTKhDnSr-CCD45-hBLiS_Lcw1jw1eN5QH6cnV71F83yy_ll_2HZOMnU1LQKjOmc84KBVGblOms600lcsU4qgRq6NQq-kmu21tZrEJVyhmARoJW2PSBHu9xtTr9mLNNwG4rDcYSIaS4DN1JaYU2Fb_-BmzTnWHsbhOWd0JIZWdXhf5UQVhvGH6KOd8jlVEpGP2xzuIV8P3A2PKxmeFrNwCt-95gIpf6ezxBdKH9fmFZr1arq3uzcpkwp_7kXWqi2ztD-BsDHloM</recordid><startdate>20051115</startdate><enddate>20051115</enddate><creator>Higgins, R. 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W. ; Shi, W.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c405t-35a779ccf20a457bc9879794eb09452e6a9de21b4d0d68f6a2cf210ea8eaa3483</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>Atmospheric circulation</topic><topic>Atmospheric moisture</topic><topic>Climate</topic><topic>Climate prediction</topic><topic>Cyclones</topic><topic>Daily precipitation</topic><topic>Datasets</topic><topic>Dew point</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Hurricane tracking</topic><topic>Hurricanes</topic><topic>Marine</topic><topic>Meteorology</topic><topic>Moisture</topic><topic>Moisture effects</topic><topic>Monsoons</topic><topic>Plumes</topic><topic>Precipitation</topic><topic>Rain</topic><topic>Sea level</topic><topic>Storms, hurricanes, tornadoes, thunderstorms</topic><topic>Surges</topic><topic>Tropical cyclones</topic><topic>Tropical regions</topic><topic>Weather analysis and prediction</topic><topic>Weather forecasting</topic><topic>Wind</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Higgins, R. 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W.</au><au>Shi, W.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Relationships between Gulf of California Moisture Surges and Tropical Cyclones in the Eastern Pacific Basin</atitle><jtitle>Journal of climate</jtitle><date>2005-11-15</date><risdate>2005</risdate><volume>18</volume><issue>22</issue><spage>4601</spage><epage>4620</epage><pages>4601-4620</pages><issn>0894-8755</issn><eissn>1520-0442</eissn><abstract>Relationships between Gulf of California moisture surges and tropical cyclones (TCs) in the eastern Pacific basin are examined. Standard surface observations are used to identify gulf surge events at Yuma, Arizona, for a multiyear (July–August 1979–2001) period. The surges are related to TCs using National Hurricane Center 6-hourly track data for the eastern Pacific basin. Climate Prediction Center (CPC)-observed daily precipitation analyses and the NCEP Regional Reanalysis are used to examine the relative differences in the precipitation, atmospheric circulation, and moisture fields for several categories of surge events, including those that are directly related to TCs, indirectly related to TCs, and not related to TCs.
It is shown that the response to the surge in the southwestern United States and northwestern Mexico is strongly discriminated by the presence or absence of TCs. Surges related to TCs tend to be associated with much stronger and deeper low-level southerly flow, deeper plumes of tropical moisture, and wetter conditions over the core monsoon region than surges that are unrelated to TCs. The response to the surge is also strongly influenced by the proximity of the TC to the Gulf of California (GOC) region. Tropical cyclones that track toward the GOC region exert a stronger, more direct influence on Yuma surges than those that track away from the GOC.</abstract><cop>Boston, MA</cop><pub>American Meteorological Society</pub><doi>10.1175/JCLI3551.1</doi><tpages>20</tpages><oa>free_for_read</oa></addata></record> |
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| source | Jstor Complete Legacy; American Meteorological Society; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals |
| subjects | Atmospheric circulation Atmospheric moisture Climate Climate prediction Cyclones Daily precipitation Datasets Dew point Earth, ocean, space Exact sciences and technology External geophysics Hurricane tracking Hurricanes Marine Meteorology Moisture Moisture effects Monsoons Plumes Precipitation Rain Sea level Storms, hurricanes, tornadoes, thunderstorms Surges Tropical cyclones Tropical regions Weather analysis and prediction Weather forecasting Wind |
| title | Relationships between Gulf of California Moisture Surges and Tropical Cyclones in the Eastern Pacific Basin |
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