Open AccessHow will the onset and retreat of rainy season over East Asia change in future?
Author(s) -
Kusunoki Shoji
Publication year - 2018
Publication title -
atmospheric science letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.951
H-Index - 45
ISSN - 1530-261X
DOI - 10.1002/asl.824
Subject(s) - climatology , wet season , east asia , precipitation , coupled model intercomparison project , environmental science , general circulation model , atmospheric circulation , subtropical ridge , atmospheric model , climate model , horizontal resolution , subtropics , climate change , china , atmospheric sciences , geography , meteorology , geology , oceanography , cartography , archaeology , fishery , biology
Future change of the rainy season over East Asia region is investigated using the high horizontal resolution global atmospheric model called the Meteorological Research Institute‐Atmospheric General Circulation Model (MRI‐AGCM) version 3.2S (20‐km grid) and 3.2H (60 km). Higher reproducibility of precipitation during East Asian rainy season gives reliability of future projections. For the present‐day simulations (1983–2003, 21 years), the models are forced with observed historical sea surface temperature (SST). For the future simulations (1979–2099, 21 years), the models are forced with future SST projected by Atmosphere–Ocean General Circulation Models (AOGCMs) participated to the fifth phase of the Coupled Model Intercomparison Project (CMIP5). In order to estimate the uncertainty of future change, we execute ensemble simulations with three kinds of cumulus convection schemes and four kinds of SST distributions using 60‐km version to meet the limitation of computer resources. For each grid point, the onset and retreat of rainy season are defined from time evolution of pentad mean precipitation. The onset of rainy season becomes earlier in most regions over East Asia, but onset will delay in some area of western Japan. Retreat delays over China and Korea. Duration increases in most part of East Asia especially over China and Korea. This can be caused by enhanced water vapor transport from the tropics. The delay of onset over western Japan can be attributed to the decrease of water vapor transport associated with the southward shift of the subtropical high. Future change presented in higher horizontal resolution compared with previous studies is useful for impact, adaptation and mitigation studies of global warming.