Dependence of Global Monsoon Response to Volcanic Eruptions on the Background Oceanic States
Both proxy data and climate modeling show divergent responses of global monsoon precipitation to volcanic eruptions. The reason is, however, unknown. Here, based on analysis of the Community Earth System Model (CESM) Last Millennium Ensemble simulation, we show evidence that the divergent responses...
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Veröffentlicht in: | Journal of climate 2021-10, Vol.34 (20), p.8273-8289 |
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description | Both proxy data and climate modeling show divergent responses of global monsoon precipitation to volcanic eruptions. The reason is, however, unknown. Here, based on analysis of the Community Earth System Model (CESM) Last Millennium Ensemble simulation, we show evidence that the divergent responses are dominated by the pre-eruption background oceanic states. We found that under El Niño–Southern Oscillation (ENSO) neutral and warm-phase initial conditions, the Pacific favors an El Niño–like anomaly after volcanic eruptions, whereas La Niña–like SST anomalies tend to occur following eruptions under ENSO cold-phase initial conditions, especially after southern eruptions. The cold initial condition is associated with stronger upper-ocean temperature stratification and a shallower thermocline over the eastern Pacific Ocean than is normal. The easterly anomalies triggered by surface cooling over the tropical South American continent can generate changes in SST through anomalous advection and the ocean subsurface upwelling more efficiently, causing La Niña–like SST anomalies. Under a warm initial condition, in contrast, the easterly anomalies fail to develop and the westerly anomalies still play a dominant role, thus forming an El Niño–like SST anomaly. This SST response further regulates the monsoon precipitation changes through atmospheric teleconnection. The contribution of direct radiative forcing and indirect SST response to precipitation changes shows regional differences that will further affect the intensity and sign of precipitation response in submonsoon regions. Our results imply that attention should be paid to the background oceanic state when predicting the global monsoon precipitation responses to volcanic eruptions. |
doi_str_mv | 10.1175/jcli-d-20-0891.1 |
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The reason is, however, unknown. Here, based on analysis of the Community Earth System Model (CESM) Last Millennium Ensemble simulation, we show evidence that the divergent responses are dominated by the pre-eruption background oceanic states. We found that under El Niño–Southern Oscillation (ENSO) neutral and warm-phase initial conditions, the Pacific favors an El Niño–like anomaly after volcanic eruptions, whereas La Niña–like SST anomalies tend to occur following eruptions under ENSO cold-phase initial conditions, especially after southern eruptions. The cold initial condition is associated with stronger upper-ocean temperature stratification and a shallower thermocline over the eastern Pacific Ocean than is normal. The easterly anomalies triggered by surface cooling over the tropical South American continent can generate changes in SST through anomalous advection and the ocean subsurface upwelling more efficiently, causing La Niña–like SST anomalies. Under a warm initial condition, in contrast, the easterly anomalies fail to develop and the westerly anomalies still play a dominant role, thus forming an El Niño–like SST anomaly. This SST response further regulates the monsoon precipitation changes through atmospheric teleconnection. The contribution of direct radiative forcing and indirect SST response to precipitation changes shows regional differences that will further affect the intensity and sign of precipitation response in submonsoon regions. Our results imply that attention should be paid to the background oceanic state when predicting the global monsoon precipitation responses to volcanic eruptions.</description><identifier>ISSN: 0894-8755</identifier><identifier>EISSN: 1520-0442</identifier><identifier>DOI: 10.1175/jcli-d-20-0891.1</identifier><language>eng</language><publisher>Boston: American Meteorological Society</publisher><subject>Advection ; Anomalies ; Atmospheric models ; Climate models ; El Nino ; El Nino phenomena ; El Nino-Southern Oscillation event ; Initial conditions ; La Nina ; Monsoon forecasting ; Monsoon precipitation ; Monsoons ; Ocean circulation ; Ocean models ; Ocean temperature ; Oceans ; Precipitation ; Radiative forcing ; Sea surface ; Sea surface temperature anomalies ; Southern Oscillation ; Stratification ; Surface cooling ; Thermocline ; Tropical climate ; Upwelling ; Volcanic eruptions ; Wind</subject><ispartof>Journal of climate, 2021-10, Vol.34 (20), p.8273-8289</ispartof><rights>2021 American Meteorological Society</rights><rights>Copyright American Meteorological Society Oct 2021</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c359t-9c313b3350b196d96a55247604c12013f1fc7ad2747a4ecfab3b23a47c88f90f3</citedby><cites>FETCH-LOGICAL-c359t-9c313b3350b196d96a55247604c12013f1fc7ad2747a4ecfab3b23a47c88f90f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/27182457$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/27182457$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,3681,27924,27925,58017,58250</link.rule.ids></links><search><creatorcontrib>Zuo, Meng</creatorcontrib><creatorcontrib>Man, Wenmin</creatorcontrib><creatorcontrib>Zhou, Tianjun</creatorcontrib><title>Dependence of Global Monsoon Response to Volcanic Eruptions on the Background Oceanic States</title><title>Journal of climate</title><description>Both proxy data and climate modeling show divergent responses of global monsoon precipitation to volcanic eruptions. The reason is, however, unknown. Here, based on analysis of the Community Earth System Model (CESM) Last Millennium Ensemble simulation, we show evidence that the divergent responses are dominated by the pre-eruption background oceanic states. We found that under El Niño–Southern Oscillation (ENSO) neutral and warm-phase initial conditions, the Pacific favors an El Niño–like anomaly after volcanic eruptions, whereas La Niña–like SST anomalies tend to occur following eruptions under ENSO cold-phase initial conditions, especially after southern eruptions. The cold initial condition is associated with stronger upper-ocean temperature stratification and a shallower thermocline over the eastern Pacific Ocean than is normal. The easterly anomalies triggered by surface cooling over the tropical South American continent can generate changes in SST through anomalous advection and the ocean subsurface upwelling more efficiently, causing La Niña–like SST anomalies. Under a warm initial condition, in contrast, the easterly anomalies fail to develop and the westerly anomalies still play a dominant role, thus forming an El Niño–like SST anomaly. This SST response further regulates the monsoon precipitation changes through atmospheric teleconnection. The contribution of direct radiative forcing and indirect SST response to precipitation changes shows regional differences that will further affect the intensity and sign of precipitation response in submonsoon regions. Our results imply that attention should be paid to the background oceanic state when predicting the global monsoon precipitation responses to volcanic eruptions.</description><subject>Advection</subject><subject>Anomalies</subject><subject>Atmospheric models</subject><subject>Climate models</subject><subject>El Nino</subject><subject>El Nino phenomena</subject><subject>El Nino-Southern Oscillation event</subject><subject>Initial conditions</subject><subject>La Nina</subject><subject>Monsoon forecasting</subject><subject>Monsoon precipitation</subject><subject>Monsoons</subject><subject>Ocean circulation</subject><subject>Ocean models</subject><subject>Ocean temperature</subject><subject>Oceans</subject><subject>Precipitation</subject><subject>Radiative forcing</subject><subject>Sea surface</subject><subject>Sea surface temperature anomalies</subject><subject>Southern Oscillation</subject><subject>Stratification</subject><subject>Surface cooling</subject><subject>Thermocline</subject><subject>Tropical climate</subject><subject>Upwelling</subject><subject>Volcanic eruptions</subject><subject>Wind</subject><issn>0894-8755</issn><issn>1520-0442</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNo9kM1LxDAQxYMouK7evQgBz13z2bRHXdd1ZWXBr5MQ0jTR1trUJD3435t1xcMwM4_fm4EHwClGM4wFv2h112R1RlCGihLP8B6YYL7dGCP7YJJElhWC80NwFEKLECY5QhPwem0G09em1wY6C5edq1QH710fnOvhgwlDGg2MDr64Tqu-0XDhxyE2SYaJiO8GXin98ebd2Ndwo80v8xhVNOEYHFjVBXPy16fg-WbxNL_N1pvlan65zjTlZcxKTTGtKOWowmVel7ninDCRI6YxQZhabLVQNRFMKGa0VRWtCFVM6KKwJbJ0Cs53dwfvvkYTomzd6Pv0UpJc8FwUqRKFdpT2LgRvrBx886n8t8RIbjOUd_P1Sl5LguQ2Q4mT5WxnaUN0_p8nAheEcUF_AGWvbnI</recordid><startdate>20211015</startdate><enddate>20211015</enddate><creator>Zuo, Meng</creator><creator>Man, Wenmin</creator><creator>Zhou, Tianjun</creator><general>American Meteorological Society</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20211015</creationdate><title>Dependence of Global Monsoon Response to Volcanic Eruptions on the Background Oceanic States</title><author>Zuo, Meng ; Man, Wenmin ; Zhou, Tianjun</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c359t-9c313b3350b196d96a55247604c12013f1fc7ad2747a4ecfab3b23a47c88f90f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Advection</topic><topic>Anomalies</topic><topic>Atmospheric models</topic><topic>Climate models</topic><topic>El Nino</topic><topic>El Nino phenomena</topic><topic>El Nino-Southern Oscillation event</topic><topic>Initial conditions</topic><topic>La Nina</topic><topic>Monsoon forecasting</topic><topic>Monsoon precipitation</topic><topic>Monsoons</topic><topic>Ocean circulation</topic><topic>Ocean models</topic><topic>Ocean temperature</topic><topic>Oceans</topic><topic>Precipitation</topic><topic>Radiative forcing</topic><topic>Sea surface</topic><topic>Sea surface temperature anomalies</topic><topic>Southern Oscillation</topic><topic>Stratification</topic><topic>Surface cooling</topic><topic>Thermocline</topic><topic>Tropical climate</topic><topic>Upwelling</topic><topic>Volcanic eruptions</topic><topic>Wind</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zuo, Meng</creatorcontrib><creatorcontrib>Man, Wenmin</creatorcontrib><creatorcontrib>Zhou, Tianjun</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of climate</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zuo, Meng</au><au>Man, Wenmin</au><au>Zhou, Tianjun</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Dependence of Global Monsoon Response to Volcanic Eruptions on the Background Oceanic States</atitle><jtitle>Journal of climate</jtitle><date>2021-10-15</date><risdate>2021</risdate><volume>34</volume><issue>20</issue><spage>8273</spage><epage>8289</epage><pages>8273-8289</pages><issn>0894-8755</issn><eissn>1520-0442</eissn><abstract>Both proxy data and climate modeling show divergent responses of global monsoon precipitation to volcanic eruptions. The reason is, however, unknown. Here, based on analysis of the Community Earth System Model (CESM) Last Millennium Ensemble simulation, we show evidence that the divergent responses are dominated by the pre-eruption background oceanic states. We found that under El Niño–Southern Oscillation (ENSO) neutral and warm-phase initial conditions, the Pacific favors an El Niño–like anomaly after volcanic eruptions, whereas La Niña–like SST anomalies tend to occur following eruptions under ENSO cold-phase initial conditions, especially after southern eruptions. The cold initial condition is associated with stronger upper-ocean temperature stratification and a shallower thermocline over the eastern Pacific Ocean than is normal. The easterly anomalies triggered by surface cooling over the tropical South American continent can generate changes in SST through anomalous advection and the ocean subsurface upwelling more efficiently, causing La Niña–like SST anomalies. Under a warm initial condition, in contrast, the easterly anomalies fail to develop and the westerly anomalies still play a dominant role, thus forming an El Niño–like SST anomaly. This SST response further regulates the monsoon precipitation changes through atmospheric teleconnection. The contribution of direct radiative forcing and indirect SST response to precipitation changes shows regional differences that will further affect the intensity and sign of precipitation response in submonsoon regions. Our results imply that attention should be paid to the background oceanic state when predicting the global monsoon precipitation responses to volcanic eruptions.</abstract><cop>Boston</cop><pub>American Meteorological Society</pub><doi>10.1175/jcli-d-20-0891.1</doi><tpages>17</tpages></addata></record> |
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subjects | Advection Anomalies Atmospheric models Climate models El Nino El Nino phenomena El Nino-Southern Oscillation event Initial conditions La Nina Monsoon forecasting Monsoon precipitation Monsoons Ocean circulation Ocean models Ocean temperature Oceans Precipitation Radiative forcing Sea surface Sea surface temperature anomalies Southern Oscillation Stratification Surface cooling Thermocline Tropical climate Upwelling Volcanic eruptions Wind |
title | Dependence of Global Monsoon Response to Volcanic Eruptions on the Background Oceanic States |
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