TY - JOUR
T1 - The interaction between winter monsoon activities in East Asia and sea surface temperature variations over the western Pacific Ocean
AU - Kawamura, R.
N1 - Copyright:
Copyright 2018 Elsevier B.V., All rights reserved.
PY - 1988
Y1 - 1988
N2 - First, the relationship between diabatic heating term and horizontal or vertical advection term at the lowest layer (1000-850 mb) is investigated by applying the empirical orthogonal function (EOF) analysis on heat budget components over the western Pacific Ocean. Second, the atmospheric response and forcing power on the SST anomaly are discussed based on the composite analysis of SST, outgoing longwave radiation and horizontal motion associated with the strength of winter monsoon. It is suggested that the strength of East Asian winter monsoon is partly controlled by the Matsuno-Gill type response model in which the strong convection over maritime continent acts as a heat source. -English summary
AB - First, the relationship between diabatic heating term and horizontal or vertical advection term at the lowest layer (1000-850 mb) is investigated by applying the empirical orthogonal function (EOF) analysis on heat budget components over the western Pacific Ocean. Second, the atmospheric response and forcing power on the SST anomaly are discussed based on the composite analysis of SST, outgoing longwave radiation and horizontal motion associated with the strength of winter monsoon. It is suggested that the strength of East Asian winter monsoon is partly controlled by the Matsuno-Gill type response model in which the strong convection over maritime continent acts as a heat source. -English summary
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U2 - 10.4157/grj1984a.61.6_469
DO - 10.4157/grj1984a.61.6_469
M3 - Article
AN - SCOPUS:0024194433
SN - 1347-9555
VL - 61
SP - 469
EP - 484
JO - Chirigaku Hyoron/Geographical Review of Japan
JF - Chirigaku Hyoron/Geographical Review of Japan
IS - 6
ER -