The role of SST forcing in the interdecadal variations of the Pacific‐Japan pattern in the late 1990s
- 7 December 2022
- journal article
- research article
- Published by Wiley in International Journal of Climatology
- Vol. 43 (3) , 1514-1528
Abstract
The Pacific‐Japan (PJ) pattern is the dominant teleconnection over East Asia, closely related to the summer precipitation on various time scales. However, studies on the connection between the interdecadal variations of the PJ pattern and sea surface temperature (SST) forcing are still limited. This study indicates that the relationship between the PJ pattern and ENSO presents a pronounced interdecadal change around 1997/1998. The PJ pattern shows a baroclinic structure over the northwest Pacific and a barotropic structure near Japan during 1979–1997, while its baroclinic structure in the tropics weakens remarkably during 1998–2021, with a southward shift of its midlatitude barotropic structure. As a result, the connection between the PJ pattern and summer precipitation over East Asia exhibits an interdecadal transition in the late 1990s. In the slow La Niña decaying summer of 1979–1997, the cold SST anomalies in the tropical Indian Ocean (TIO) excite an eastward‐propagating Kelvin wave that enhances convection over the northwest Pacific, resulting in the formation of the PJ pattern. In contrast, the cold SST anomalies in the Maritime Continent rather than the TIO yield a zonally confined Kelvin wave in the rapid La Niña decaying summer of 1998–2021. The elongated Kelvin wave penetrating the central Pacific weakens convective anomalies over the northwest Pacific, thereby weakening the baroclinic structure of the PJ pattern in the tropics. Meanwhile, the warm SST anomalies in the Kuroshio Extension (KE) induce a northward shift of the East Asian subtropical westerly jet, with the anomalous anticyclonic circulation over the KE significantly affecting summer precipitation along the Meiyu belt. Therefore, the midlatitude barotropic structure of the PJ pattern shifts southward after the late 1990s.Keywords
Funding Information
- China Scholarship Council
- National Natural Science Foundation of China (41905060, 42130610, 42175071)
- Priority Academic Program Development of Jiangsu Higher Education Institutions
This publication has 56 references indexed in Scilit:
- Origin of seasonal predictability for summer climate over the Northwestern PacificProceedings of the National Academy of Sciences, 2013
- Strengthening of Tropical Indian Ocean Teleconnection to the Northwest Pacific since the Mid-1970s: An Atmospheric GCM Study*Journal of Climate, 2010
- Mechanisms of Meridional Teleconnection Observed between a Summer Monsoon System and a Subtropical Anticyclone. Part I: The Pacific–Japan PatternJournal of Climate, 2010
- Decadal Shift in El Niño Influences on Indo–Western Pacific and East Asian Climate in the 1970s*Journal of Climate, 2010
- Role of Subtropical Precipitation Anomalies in Maintaining the Summertime Meridional Teleconnection over the Western North Pacific and East AsiaJournal of Climate, 2009
- Structure and dynamics of the summertime Pacific–Japan teleconnection patternQuarterly Journal of the Royal Meteorological Society, 2006
- Associations among the Components of the East Asian Summer Monsoon System in the Meridional DirectionJournal of the Meteorological Society of Japan, 2004
- NCEP–DOE AMIP-II Reanalysis (R-2)Bulletin of the American Meteorological Society, 2002
- Some simple solutions for heat‐induced tropical circulationQuarterly Journal of the Royal Meteorological Society, 1980
- An Introduction to Dynamic MeteorologyAmerican Journal of Physics, 1973