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1000 Titel
  • Response of the Asian summer Monsoons to a high-latitude thermal forcing: mechanisms and nonlinearities
1000 Autor/in
  1. Talento, Stefanie |
  2. Osborn, Timothy J. |
  3. Joshi, Manoj |
  4. Ratna, Satyaban B. |
  5. Luterbacher, Jürg |
1000 Erscheinungsjahr 2020
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2020-03-26
1000 Erschienen in
1000 Quellenangabe
  • 54(9-10):3927-3944
1000 Copyrightjahr
  • 2020
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1007/s00382-020-05210-9 |
1000 Publikationsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:title>Abstract</jats:title><jats:p>This study investigates mechanisms and nonlinearities in the response of the Asian Summer Monsoons (ASM) to high-latitude thermal forcings of different amplitudes. Using a suite of runs carried out with an intermediate-complexity atmospheric general circulation model, we find that the imposed forcings produce a strong precipitation response over the eastern ASM but a rather weak response over the southern ASM. The forcing also causes a precipitation dipole with wet conditions over the eastern Tibetan Plateau (TP) and dry conditions over the Bay of Bengal (BoB) and southeast Asia. A moderate increase of precipitation along the southern margin of the TP is also produced. Simulations designed to isolate the causal mechanisms show that thermodynamic interactions involving the tropical surface oceans are far less important than the water-vapour feedback for the transmission of information from the high-latitudes to the ASM. Additionally, we assess the nonlinearity of the ASM precipitation response to the forcing amplitude using a novel application of the empirical orthogonal function method. The response can be decomposed in two overlapping patterns. The first pattern represents a precipitation dipole with wet conditions over the eastern TP and dry conditions over BoB, which linearly increases with forcing amplitude becoming quasi-stationary for large forcing amplitudes (i.e. amplitudes leading to Arctic temperature anomalies larger than 10 °C). The second pattern is associated with increased precipitation over the southeastern TP and is nonlinearly dependent on forcing, being most important for intermediate forcing amplitudes (i.e. amplitudes leading to Arctic temperature anomalies between 5 and 10 °C).</jats:p>
1000 Sacherschließung
lokal Article
lokal Asian Monsoons
lokal High-latitude forcing
lokal Nonlinear
lokal Slab model
1000 Liste der Beteiligten
  1. https://orcid.org/0000-0003-0100-5033|https://frl.publisso.de/adhoc/uri/T3Nib3JuLCBUaW1vdGh5IEou|https://frl.publisso.de/adhoc/uri/Sm9zaGksIE1hbm9q|https://frl.publisso.de/adhoc/uri/UmF0bmEsIFNhdHlhYmFuIEIu|https://frl.publisso.de/adhoc/uri/THV0ZXJiYWNoZXIsIErDvHJn
1000 Hinweis
  • DeepGreen-ID: 9a99bab02cc44f3d9d33e41039f72c44 ; metadata provieded by: DeepGreen (https://www.oa-deepgreen.de/api/v1/), LIVIVO search scope life sciences (http://z3950.zbmed.de:6210/livivo), Crossref Unified Resource API (https://api.crossref.org/swagger-ui/index.html), to.science.api (https://frl.publisso.de/), ZDB JSON-API (beta) (https://zeitschriftendatenbank.de/api/), lobid - Dateninfrastruktur für Bibliotheken (https://lobid.org/resources/search)
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1000 Erstellt am 2023-11-17T03:25:25.775+0100
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1000 Zuletzt bearbeitet Fri Dec 01 04:53:09 CET 2023
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