Matches in SemOpenAlex for { <https://semopenalex.org/work/W2328084110> ?p ?o ?g. }
Showing items 1 to 84 of
84
with 100 items per page.
- W2328084110 abstract "Based on monthly mean wind, geopotential height, specific humidity, and surface pressure of NCAR/NCEP reanalysis, NOAA-reconstructed sea surface temperature (SST) of the Indian Ocean, and daily precipitation data at 97 meteorological stations over the eastern NW China in the past 47 years, the threshold values for extreme precipitation events (EPE) are defined using the percentile method. Singular Value Decomposition and synthetic analysis methods are used to analyze the relationship between summer EPE in the eastern NW China and SSTA in the preceding fall, winter, spring, and the concurrent summer. The result shows that preceding spring SST anomalies (SSTA) in the Indian Ocean are clear indicators for the forecast of summer EPE in the eastern NW China, and a key area of impact is located in the equatorial Indian Ocean. When spring SST is anomalously high in the equatorial Indian Ocean, the meridional circulation averaged over 100°E-110°E will be anomalously ascending near the equator but anomalously descending near 30°N in the middle and upper troposphere from the concurrent to the subsequent summer. In the meantime, the Southwest Monsoon from the Indian Ocean will be anomalously weak and there will be no anomalous water vapor transport to the eastern NW China, resulting in a lack of EPE in the subsequent summer, and vice versa. In addition, in response to anomalously high SST in the equatorial Indian Ocean in spring, the South Asia high pressure tends to be strong in the subsequent summer and more to the west. In the anomalously low SST year, however, the South Asia high tends to be weak in the subsequent summer and more to the east. This is another possible cause of the variation of summer EPE in the eastern NW China." @default.
- W2328084110 created "2016-06-24" @default.
- W2328084110 creator A5002718976 @default.
- W2328084110 creator A5030109415 @default.
- W2328084110 date "2011-01-01" @default.
- W2328084110 modified "2023-09-26" @default.
- W2328084110 title "A STUDY ON THE EFFECT OF SPRING INDIAN OCEAN SSTA ON SUMMER EXTREME PRECIPITATION EVENTS OVER THE EASTERN NW CHINA" @default.
- W2328084110 cites W1600917725 @default.
- W2328084110 cites W2150897391 @default.
- W2328084110 cites W2164475240 @default.
- W2328084110 cites W2350016274 @default.
- W2328084110 cites W2358400938 @default.
- W2328084110 cites W2373731940 @default.
- W2328084110 cites W2375761735 @default.
- W2328084110 cites W2379578904 @default.
- W2328084110 cites W2385863179 @default.
- W2328084110 cites W2389507438 @default.
- W2328084110 cites W2390333944 @default.
- W2328084110 cites W2392097935 @default.
- W2328084110 cites W2914934494 @default.
- W2328084110 hasPublicationYear "2011" @default.
- W2328084110 type Work @default.
- W2328084110 sameAs 2328084110 @default.
- W2328084110 citedByCount "0" @default.
- W2328084110 crossrefType "journal-article" @default.
- W2328084110 hasAuthorship W2328084110A5002718976 @default.
- W2328084110 hasAuthorship W2328084110A5030109415 @default.
- W2328084110 hasConcept C107054158 @default.
- W2328084110 hasConcept C122523270 @default.
- W2328084110 hasConcept C127313418 @default.
- W2328084110 hasConcept C127413603 @default.
- W2328084110 hasConcept C12980444 @default.
- W2328084110 hasConcept C13280743 @default.
- W2328084110 hasConcept C134097258 @default.
- W2328084110 hasConcept C153294291 @default.
- W2328084110 hasConcept C192901106 @default.
- W2328084110 hasConcept C205649164 @default.
- W2328084110 hasConcept C2778712887 @default.
- W2328084110 hasConcept C39432304 @default.
- W2328084110 hasConcept C49204034 @default.
- W2328084110 hasConcept C78519656 @default.
- W2328084110 hasConcept C9075549 @default.
- W2328084110 hasConceptScore W2328084110C107054158 @default.
- W2328084110 hasConceptScore W2328084110C122523270 @default.
- W2328084110 hasConceptScore W2328084110C127313418 @default.
- W2328084110 hasConceptScore W2328084110C127413603 @default.
- W2328084110 hasConceptScore W2328084110C12980444 @default.
- W2328084110 hasConceptScore W2328084110C13280743 @default.
- W2328084110 hasConceptScore W2328084110C134097258 @default.
- W2328084110 hasConceptScore W2328084110C153294291 @default.
- W2328084110 hasConceptScore W2328084110C192901106 @default.
- W2328084110 hasConceptScore W2328084110C205649164 @default.
- W2328084110 hasConceptScore W2328084110C2778712887 @default.
- W2328084110 hasConceptScore W2328084110C39432304 @default.
- W2328084110 hasConceptScore W2328084110C49204034 @default.
- W2328084110 hasConceptScore W2328084110C78519656 @default.
- W2328084110 hasConceptScore W2328084110C9075549 @default.
- W2328084110 hasLocation W23280841101 @default.
- W2328084110 hasOpenAccess W2328084110 @default.
- W2328084110 hasPrimaryLocation W23280841101 @default.
- W2328084110 hasRelatedWork W1039778171 @default.
- W2328084110 hasRelatedWork W1479795923 @default.
- W2328084110 hasRelatedWork W2025618678 @default.
- W2328084110 hasRelatedWork W2116307015 @default.
- W2328084110 hasRelatedWork W2258309301 @default.
- W2328084110 hasRelatedWork W2289884108 @default.
- W2328084110 hasRelatedWork W2321811832 @default.
- W2328084110 hasRelatedWork W2353296739 @default.
- W2328084110 hasRelatedWork W2357672519 @default.
- W2328084110 hasRelatedWork W2359937555 @default.
- W2328084110 hasRelatedWork W2361066615 @default.
- W2328084110 hasRelatedWork W2361154067 @default.
- W2328084110 hasRelatedWork W2366529618 @default.
- W2328084110 hasRelatedWork W2367942763 @default.
- W2328084110 hasRelatedWork W2375573908 @default.
- W2328084110 hasRelatedWork W2382044112 @default.
- W2328084110 hasRelatedWork W2390333944 @default.
- W2328084110 hasRelatedWork W2567325936 @default.
- W2328084110 hasRelatedWork W3145835277 @default.
- W2328084110 hasRelatedWork W3151140141 @default.
- W2328084110 isParatext "false" @default.
- W2328084110 isRetracted "false" @default.
- W2328084110 magId "2328084110" @default.
- W2328084110 workType "article" @default.