FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2059229322> ?p ?o ?g. }

• W2059229322 abstract "[1] Lower-tropospheric southerly surges occurring at submonthly timescales over the eastern Indian Ocean (EIO) during Southern Hemisphere (SH) winter are extratropical-tropical interaction phenomena involving various processes. This study examined the physical mechanism driving equatorial wave disturbances associated with surge-induced cross-equatorial flow over the EIO. Japanese 25-Year Reanalysis (JRA25) and Tropical Rainfall Measuring Mission Satellite (TRMM) 3B42 data products from June to August for the 7 years from 1998 to 2004 were analyzed. Composite analyses of low-level wind and vorticity fields reveal that an equatorial clockwise gyre develops just after cross-equatorial penetration of southerly surge winds. This gyre is interpreted as an equatorially trapped Rossby wave that develops asymmetrically around the equator in response to surge-induced cross-equatorial flow. Eddy vorticity budget analysis demonstrates the dynamic role of the southerly surge in the genesis of the equatorial clockwise gyre. The result indicates that an injection of negative absolute vorticity into the equatorial tropics due to both advective and convergent processes associated with the surge winds is primarily responsible for the gyre genesis. Cross-equatorial advection of basic state absolute vorticity by the surge (eddy) winds and vortex stretching by surge wind convergence are most effective in spinning up the equatorial clockwise gyre. Wave activity flux analysis further emphasizes that Rossby wave energy propagation from the SH extratropics into the equatorial EIO region is caused by the southerly surge. These dynamic diagnostics suggest that the southerly surge plays a lateral forcing role in exciting the equatorial wave disturbance over the EIO. Composite analyses of moisture flux and precipitation anomalies characterize the equatorial clockwise gyre as a convectively coupled equatorial Rossby wave. Enhanced cross-equatorial moisture transport due to the southerly surge appears to be linked to precipitation along the west coast of the southern Indo-China Peninsula. A case study of the southerly surge event during August 2000 illustrates the formation of the equatorial clockwise gyre and its convectively coupled equatorial Rossby wave signature." @default.
• W2059229322 created "2016-06-24" @default.
• W2059229322 creator A5030250659 @default.
• W2059229322 creator A5038567365 @default.
• W2059229322 date "2009-10-31" @default.
• W2059229322 modified "2023-10-14" @default.
• W2059229322 title "Cross-equatorial influences of submonthly scale southerly surges over the eastern Indian Ocean during Southern Hemisphere winter" @default.
• W2059229322 cites W116486345 @default.
• W2059229322 cites W1433273814 @default.
• W2059229322 cites W1498891724 @default.
• W2059229322 cites W1965350141 @default.
• W2059229322 cites W1967250722 @default.
• W2059229322 cites W1971577532 @default.
• W2059229322 cites W1992652001 @default.
• W2059229322 cites W1996446184 @default.
• W2059229322 cites W1996447882 @default.
• W2059229322 cites W2008796783 @default.
• W2059229322 cites W2012288042 @default.
• W2059229322 cites W2016243669 @default.
• W2059229322 cites W2030155570 @default.
• W2059229322 cites W2031442459 @default.
• W2059229322 cites W2041591286 @default.
• W2059229322 cites W2044690762 @default.
• W2059229322 cites W2049445425 @default.
• W2059229322 cites W2054053231 @default.
• W2059229322 cites W2054732355 @default.
• W2059229322 cites W2055354093 @default.
• W2059229322 cites W2064229792 @default.
• W2059229322 cites W2064994665 @default.
• W2059229322 cites W2065656298 @default.
• W2059229322 cites W2065724545 @default.
• W2059229322 cites W2074067229 @default.
• W2059229322 cites W2082519714 @default.
• W2059229322 cites W2097519212 @default.
• W2059229322 cites W2102017249 @default.
• W2059229322 cites W2102503483 @default.
• W2059229322 cites W2113085823 @default.
• W2059229322 cites W2136500905 @default.
• W2059229322 cites W2136535710 @default.
• W2059229322 cites W2140994193 @default.
• W2059229322 cites W2146357303 @default.
• W2059229322 cites W2147962971 @default.
• W2059229322 cites W2150966423 @default.
• W2059229322 cites W2157358558 @default.
• W2059229322 cites W2176392362 @default.
• W2059229322 cites W2176967258 @default.
• W2059229322 cites W2177569130 @default.
• W2059229322 cites W2177941723 @default.
• W2059229322 cites W2232101435 @default.
• W2059229322 cites W2624022819 @default.
• W2059229322 cites W8018456 @default.
• W2059229322 doi "https://doi.org/10.1029/2008jd011441" @default.
• W2059229322 hasPublicationYear "2009" @default.
• W2059229322 type Work @default.
• W2059229322 sameAs 2059229322 @default.
• W2059229322 citedByCount "6" @default.
• W2059229322 countsByYear W20592293222014 @default.
• W2059229322 countsByYear W20592293222016 @default.
• W2059229322 countsByYear W20592293222019 @default.
• W2059229322 crossrefType "journal-article" @default.
• W2059229322 hasAuthorship W2059229322A5030250659 @default.
• W2059229322 hasAuthorship W2059229322A5038567365 @default.
• W2059229322 hasConcept C111368507 @default.
• W2059229322 hasConcept C127313418 @default.
• W2059229322 hasConcept C205649164 @default.
• W2059229322 hasConcept C2777252438 @default.
• W2059229322 hasConcept C2778755073 @default.
• W2059229322 hasConcept C2778835443 @default.
• W2059229322 hasConcept C2985189572 @default.
• W2059229322 hasConcept C39432304 @default.
• W2059229322 hasConcept C49204034 @default.
• W2059229322 hasConcept C58640448 @default.
• W2059229322 hasConcept C91586092 @default.
• W2059229322 hasConceptScore W2059229322C111368507 @default.
• W2059229322 hasConceptScore W2059229322C127313418 @default.
• W2059229322 hasConceptScore W2059229322C205649164 @default.
• W2059229322 hasConceptScore W2059229322C2777252438 @default.
• W2059229322 hasConceptScore W2059229322C2778755073 @default.
• W2059229322 hasConceptScore W2059229322C2778835443 @default.
• W2059229322 hasConceptScore W2059229322C2985189572 @default.
• W2059229322 hasConceptScore W2059229322C39432304 @default.
• W2059229322 hasConceptScore W2059229322C49204034 @default.
• W2059229322 hasConceptScore W2059229322C58640448 @default.
• W2059229322 hasConceptScore W2059229322C91586092 @default.
• W2059229322 hasIssue "D20" @default.
• W2059229322 hasLocation W20592293221 @default.
• W2059229322 hasOpenAccess W2059229322 @default.
• W2059229322 hasPrimaryLocation W20592293221 @default.
• W2059229322 hasRelatedWork W156163635 @default.
• W2059229322 hasRelatedWork W1984804586 @default.
• W2059229322 hasRelatedWork W2038475912 @default.
• W2059229322 hasRelatedWork W2051465729 @default.
• W2059229322 hasRelatedWork W2080649326 @default.
• W2059229322 hasRelatedWork W2370445157 @default.
• W2059229322 hasRelatedWork W3128677939 @default.
• W2059229322 hasRelatedWork W3194608633 @default.
• W2059229322 hasRelatedWork W4321501213 @default.
• W2059229322 hasRelatedWork W64480068 @default.
• W2059229322 hasVolume "114" @default.
• W2059229322 isParatext "false" @default.

• next