Matches in SemOpenAlex for { <https://semopenalex.org/work/W2144092365> ?p ?o ?g. }
- W2144092365 endingPage "6208" @default.
- W2144092365 startingPage "6195" @default.
- W2144092365 abstract "Abstract Insolation forcing related to the earth’s orbital parameters is known to play an important role in regulating variations of the South Asian monsoon on geological time scales. The influence of insolation forcing on the Indian Ocean and Asian monsoon is studied in this paper by isolating the Northern and Southern Hemispheric insolation changes in several numerical experiments with a coupled ocean–atmosphere model. The focus is on the response of South Asian summer rainfall (monsoon strength) with emphasis on impacts of the local versus remote forcing and possible mechanisms. The model results show that both Northern Hemisphere (NH) and Southern Hemisphere (SH) summer insolation changes affect the Indian Ocean and Asian monsoon as a local forcing (in the same hemisphere), but only the SH changes result in remote (in the other hemisphere) forcing. The NH insolation change has a local and immediate impact on NH summer monsoons from North Africa to South and East Asia, while the SH insolation change has a remote and seasonal-scale delayed effect on the South Asian summer monsoon rainfall. When the SH insolation is increased from December to April, the sea surface temperature (SST) in the southern tropical Indian Ocean remains high from January to July. The increased SST produces more atmospheric precipitable water over the southern tropical Indian Ocean by promoting evaporation from the ocean. The enhanced precipitable water over the southern Indian Ocean is transported northward to the South Asian monsoon region by the lower-tropospheric mean cross-equatorial flows with the onset of the Asian monsoon increasing precipitable water over South Asia, eventually leading to the increase of Indian summer monsoon precipitation. Thus, these model experiments, while idealized and not fully representing actual orbitally forced insolation changes, confirm the broadscale response of northern monsoons to NH summer insolation increases and also illustrate how SH summer insolation increases can have a delayed influence on the Indian summer monsoon." @default.
- W2144092365 created "2016-06-24" @default.
- W2144092365 creator A5001545889 @default.
- W2144092365 creator A5003161142 @default.
- W2144092365 creator A5024396336 @default.
- W2144092365 creator A5035168940 @default.
- W2144092365 creator A5045780350 @default.
- W2144092365 date "2006-12-01" @default.
- W2144092365 modified "2023-09-30" @default.
- W2144092365 title "Hemispheric Insolation Forcing of the Indian Ocean and Asian Monsoon: Local versus Remote Impacts*" @default.
- W2144092365 cites W1501100918 @default.
- W2144092365 cites W1546175236 @default.
- W2144092365 cites W1650939803 @default.
- W2144092365 cites W1973977063 @default.
- W2144092365 cites W1979763416 @default.
- W2144092365 cites W1983256425 @default.
- W2144092365 cites W1995900578 @default.
- W2144092365 cites W2003926579 @default.
- W2144092365 cites W2012237835 @default.
- W2144092365 cites W2013878295 @default.
- W2144092365 cites W2014981382 @default.
- W2144092365 cites W2016499349 @default.
- W2144092365 cites W2016919420 @default.
- W2144092365 cites W2017125056 @default.
- W2144092365 cites W2024150465 @default.
- W2144092365 cites W2026413084 @default.
- W2144092365 cites W2026739367 @default.
- W2144092365 cites W2030174121 @default.
- W2144092365 cites W2034106128 @default.
- W2144092365 cites W2037799531 @default.
- W2144092365 cites W2042241171 @default.
- W2144092365 cites W2062265267 @default.
- W2144092365 cites W2063837723 @default.
- W2144092365 cites W2064759564 @default.
- W2144092365 cites W2068207047 @default.
- W2144092365 cites W2072470725 @default.
- W2144092365 cites W2073313709 @default.
- W2144092365 cites W2076865763 @default.
- W2144092365 cites W2077972705 @default.
- W2144092365 cites W2078721910 @default.
- W2144092365 cites W2081241122 @default.
- W2144092365 cites W2083601283 @default.
- W2144092365 cites W2086731985 @default.
- W2144092365 cites W2093367625 @default.
- W2144092365 cites W2113580664 @default.
- W2144092365 cites W2119440619 @default.
- W2144092365 cites W2134289299 @default.
- W2144092365 cites W2144892623 @default.
- W2144092365 cites W2151784978 @default.
- W2144092365 cites W2155558849 @default.
- W2144092365 cites W2162339007 @default.
- W2144092365 cites W2173391861 @default.
- W2144092365 cites W2173796985 @default.
- W2144092365 cites W2176874196 @default.
- W2144092365 cites W2179023634 @default.
- W2144092365 cites W25765940 @default.
- W2144092365 doi "https://doi.org/10.1175/jcli3965.1" @default.
- W2144092365 hasPublicationYear "2006" @default.
- W2144092365 type Work @default.
- W2144092365 sameAs 2144092365 @default.
- W2144092365 citedByCount "49" @default.
- W2144092365 countsByYear W21440923652012 @default.
- W2144092365 countsByYear W21440923652014 @default.
- W2144092365 countsByYear W21440923652015 @default.
- W2144092365 countsByYear W21440923652016 @default.
- W2144092365 countsByYear W21440923652017 @default.
- W2144092365 countsByYear W21440923652018 @default.
- W2144092365 countsByYear W21440923652019 @default.
- W2144092365 countsByYear W21440923652020 @default.
- W2144092365 countsByYear W21440923652021 @default.
- W2144092365 countsByYear W21440923652022 @default.
- W2144092365 countsByYear W21440923652023 @default.
- W2144092365 crossrefType "journal-article" @default.
- W2144092365 hasAuthorship W2144092365A5001545889 @default.
- W2144092365 hasAuthorship W2144092365A5003161142 @default.
- W2144092365 hasAuthorship W2144092365A5024396336 @default.
- W2144092365 hasAuthorship W2144092365A5035168940 @default.
- W2144092365 hasAuthorship W2144092365A5045780350 @default.
- W2144092365 hasBestOaLocation W21440923651 @default.
- W2144092365 hasConcept C107054158 @default.
- W2144092365 hasConcept C111368507 @default.
- W2144092365 hasConcept C127313418 @default.
- W2144092365 hasConcept C134097258 @default.
- W2144092365 hasConcept C136996986 @default.
- W2144092365 hasConcept C146213904 @default.
- W2144092365 hasConcept C153294291 @default.
- W2144092365 hasConcept C156008332 @default.
- W2144092365 hasConcept C197115733 @default.
- W2144092365 hasConcept C205649164 @default.
- W2144092365 hasConcept C23095489 @default.
- W2144092365 hasConcept C2777252438 @default.
- W2144092365 hasConcept C2778835443 @default.
- W2144092365 hasConcept C39432304 @default.
- W2144092365 hasConcept C49204034 @default.
- W2144092365 hasConcept C68818249 @default.
- W2144092365 hasConcept C91586092 @default.
- W2144092365 hasConceptScore W2144092365C107054158 @default.
- W2144092365 hasConceptScore W2144092365C111368507 @default.