FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3123975181> ?p ?o ?g. }

• W3123975181 abstract "The key factors affecting the variation of the ‘ozone valley’, which appears during the boreal summer in the upper troposphere and lower stratosphere (UTLS) over the South Asian High (SAH) and its adjacent areas, have not been determined. This study has performed statistical analysis to improve the understanding of the roles of the sea surface temperature (SST), tropopause height, and the West Pacific Subtropical High (WPSH) on the ozone valley. Based on the European Center for Medium-Range Weather Forecasts Interim Re-Analysis (ERA5), Modern Era Retrospective Analysis for Research and Applications dataset version 2 (MERRA2), and the Stratospheric Water and Ozone Satellite Homogenized (SWOOSH) observation dataset, we examined the principal components of the zonal deviation of the total column ozone (TCO*) in the UTLS by applying the empirical orthogonal function (EOF), Liang-Kleeman information flow method, regression analysis, and composite analysis. The variations of the TCO* anomalies show three dominant modes, namely the east-west dipole mode in the low latitude region, the east-west tripole mode in the middle latitude region, and the south-north mode. According to the regression analysis and information flow, the three leading principal components of TCO* variations are related to the SST near Indonesia and the western Pacific Ocean in low latitudes, the tropopause height over the Iranian Plateau (IP), and the strength of the SAH over the eastern part of the Tibetan Plateau (TP), which is linked to the synchronousness between the SAH and the WPSH. For the east-west dipole mode in the low latitude region, composite analysis shows the interaction between the atmosphere and ocean causes the strengthening of the southern trough at 850 hPa and the divergence at 200 hPa, resulting in a decrease of the TCO* in the UTLS near the low latitude region around the TP. For the east-west tripole mode in the middle latitude region, the composite analysis shows obvious negative anomalies over the IP, where the TCO* reduces and the extent of the ozone valley over the IP increases with the rise of the tropopause. Comparatively, the south-north mode shows obvious positive anomalies over the TP, where the TCO* increases and the extent of the ozone valley over the TP decreases with a weak SAH. This mode is closely related to the location of the WPSH. In summary, the leading factors affecting the three dominant modes for the variations of the TCO* anomalies are SST, tropopause height, and the WPSH." @default.
• W3123975181 created "2021-02-01" @default.
• W3123975181 creator A5001787722 @default.
• W3123975181 creator A5012545618 @default.
• W3123975181 creator A5031606363 @default.
• W3123975181 creator A5037529473 @default.
• W3123975181 date "2021-01-22" @default.
• W3123975181 modified "2023-09-25" @default.
• W3123975181 title "Attribution of the Principal Components of the Summertime Ozone Valley in the Upper Troposphere and Lower Stratosphere" @default.
• W3123975181 cites W1841345523 @default.
• W3123975181 cites W1944123744 @default.
• W3123975181 cites W1971991115 @default.
• W3123975181 cites W2009673844 @default.
• W3123975181 cites W2019571347 @default.
• W3123975181 cites W2023258127 @default.
• W3123975181 cites W2044722291 @default.
• W3123975181 cites W2058179313 @default.
• W3123975181 cites W2059298204 @default.
• W3123975181 cites W2069857569 @default.
• W3123975181 cites W2079029547 @default.
• W3123975181 cites W2084402253 @default.
• W3123975181 cites W2090263405 @default.
• W3123975181 cites W2096239587 @default.
• W3123975181 cites W2135276541 @default.
• W3123975181 cites W2169581288 @default.
• W3123975181 cites W2312414574 @default.
• W3123975181 cites W2588787202 @default.
• W3123975181 cites W2754904600 @default.
• W3123975181 cites W2756316638 @default.
• W3123975181 cites W2758155081 @default.
• W3123975181 cites W2758632767 @default.
• W3123975181 cites W2760460242 @default.
• W3123975181 cites W2802223697 @default.
• W3123975181 cites W2888630661 @default.
• W3123975181 cites W2888904162 @default.
• W3123975181 cites W2891945631 @default.
• W3123975181 cites W2917381035 @default.
• W3123975181 cites W2946469387 @default.
• W3123975181 cites W2959085736 @default.
• W3123975181 cites W3000228423 @default.
• W3123975181 cites W3003060216 @default.
• W3123975181 cites W3005660423 @default.
• W3123975181 cites W3038746020 @default.
• W3123975181 cites W3045187307 @default.
• W3123975181 cites W643577933 @default.
• W3123975181 doi "https://doi.org/10.3389/feart.2020.605703" @default.
• W3123975181 hasPublicationYear "2021" @default.
• W3123975181 type Work @default.
• W3123975181 sameAs 3123975181 @default.
• W3123975181 citedByCount "3" @default.
• W3123975181 countsByYear W31239751812022 @default.
• W3123975181 countsByYear W31239751812023 @default.
• W3123975181 crossrefType "journal-article" @default.
• W3123975181 hasAuthorship W3123975181A5001787722 @default.
• W3123975181 hasAuthorship W3123975181A5012545618 @default.
• W3123975181 hasAuthorship W3123975181A5031606363 @default.
• W3123975181 hasAuthorship W3123975181A5037529473 @default.
• W3123975181 hasBestOaLocation W31239751811 @default.
• W3123975181 hasConcept C107054158 @default.
• W3123975181 hasConcept C122523270 @default.
• W3123975181 hasConcept C127313418 @default.
• W3123975181 hasConcept C13280743 @default.
• W3123975181 hasConcept C134306372 @default.
• W3123975181 hasConcept C13724139 @default.
• W3123975181 hasConcept C153294291 @default.
• W3123975181 hasConcept C160945548 @default.
• W3123975181 hasConcept C163861444 @default.
• W3123975181 hasConcept C171420983 @default.
• W3123975181 hasConcept C18101618 @default.
• W3123975181 hasConcept C205649164 @default.
• W3123975181 hasConcept C2780030769 @default.
• W3123975181 hasConcept C33923547 @default.
• W3123975181 hasConcept C39432304 @default.
• W3123975181 hasConcept C49204034 @default.
• W3123975181 hasConcept C9075549 @default.
• W3123975181 hasConcept C91586092 @default.
• W3123975181 hasConceptScore W3123975181C107054158 @default.
• W3123975181 hasConceptScore W3123975181C122523270 @default.
• W3123975181 hasConceptScore W3123975181C127313418 @default.
• W3123975181 hasConceptScore W3123975181C13280743 @default.
• W3123975181 hasConceptScore W3123975181C134306372 @default.
• W3123975181 hasConceptScore W3123975181C13724139 @default.
• W3123975181 hasConceptScore W3123975181C153294291 @default.
• W3123975181 hasConceptScore W3123975181C160945548 @default.
• W3123975181 hasConceptScore W3123975181C163861444 @default.
• W3123975181 hasConceptScore W3123975181C171420983 @default.
• W3123975181 hasConceptScore W3123975181C18101618 @default.
• W3123975181 hasConceptScore W3123975181C205649164 @default.
• W3123975181 hasConceptScore W3123975181C2780030769 @default.
• W3123975181 hasConceptScore W3123975181C33923547 @default.
• W3123975181 hasConceptScore W3123975181C39432304 @default.
• W3123975181 hasConceptScore W3123975181C49204034 @default.
• W3123975181 hasConceptScore W3123975181C9075549 @default.
• W3123975181 hasConceptScore W3123975181C91586092 @default.
• W3123975181 hasFunder F4320329021 @default.
• W3123975181 hasLocation W31239751811 @default.
• W3123975181 hasOpenAccess W3123975181 @default.
• W3123975181 hasPrimaryLocation W31239751811 @default.
• W3123975181 hasRelatedWork W1979199890 @default.
• W3123975181 hasRelatedWork W2006549483 @default.

• next