Change in coherence of interannual variability of summer rainfall over the western Pacific around the early 2000s: Role of Indo-Pacific ocean forcing

Change in coherence of interannual variability of summer rainfall over the western Pacific around... AbstractThe observations show that the covariability between the western North Pacific (WNP) and the South China Sea (SCS) summer rainfall has experienced an obvious weakening since the early 2000s. During the period 1982-2003, the combined North Indian Ocean (NIO), central North Pacific (CNP), and central equatorial Pacific (CEP) sea surface temperature (SST) forcing results in a high coherence between the WNP and SCS summer rainfall variations via an zonally elongated anomalous lower-level cyclone over the western Pacific. During the period 2004-2016, the Indian Ocean SST contribution is largely weakened, and the WNP rainfall variability is dominated by the enhanced Pacific SST forcing with an eastward retreated lower-level wind and rainfall anomalies, whereas the SCS rainfall variability is mainly associated with local air-sea interaction processes. The results obtained from observational analysis are supported by numerical experiments with atmospheric and coupled general circulation models. The change in the coherence of interannual summer rainfall variability over the WNP and SCS has an important implication for regional climate prediction in South and East Asia. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Climate American Meteorological Society

Change in coherence of interannual variability of summer rainfall over the western Pacific around the early 2000s: Role of Indo-Pacific ocean forcing

Journal of Climate , Volume preprint (2018): 1 – Feb 28, 2018

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Publisher
American Meteorological Society
Copyright
Copyright © American Meteorological Society
ISSN
1520-0442
D.O.I.
10.1175/JCLI-D-17-0687.1
Publisher site
See Article on Publisher Site

Abstract

AbstractThe observations show that the covariability between the western North Pacific (WNP) and the South China Sea (SCS) summer rainfall has experienced an obvious weakening since the early 2000s. During the period 1982-2003, the combined North Indian Ocean (NIO), central North Pacific (CNP), and central equatorial Pacific (CEP) sea surface temperature (SST) forcing results in a high coherence between the WNP and SCS summer rainfall variations via an zonally elongated anomalous lower-level cyclone over the western Pacific. During the period 2004-2016, the Indian Ocean SST contribution is largely weakened, and the WNP rainfall variability is dominated by the enhanced Pacific SST forcing with an eastward retreated lower-level wind and rainfall anomalies, whereas the SCS rainfall variability is mainly associated with local air-sea interaction processes. The results obtained from observational analysis are supported by numerical experiments with atmospheric and coupled general circulation models. The change in the coherence of interannual summer rainfall variability over the WNP and SCS has an important implication for regional climate prediction in South and East Asia.

Journal

Journal of ClimateAmerican Meteorological Society

Published: Feb 28, 2018

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