Abstract
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
| Original language | English |
|---|---|
| Pages (from-to) | 469-484 |
| Number of pages | 16 |
| Journal | Geographical Review of Japan, Series A |
| Volume | 61 |
| Issue number | 6 |
| DOIs | |
| Publication status | Published - Jan 1 1988 |
| Externally published | Yes |
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All Science Journal Classification (ASJC) codes
- Geography, Planning and Development
- Earth-Surface Processes
Cite this
The interaction between winter monsoon activities in East Asia and sea surface temperature variations over the western Pacific Ocean. / Kawamura, Ryuichi.
In: Geographical Review of Japan, Series A, Vol. 61, No. 6, 01.01.1988, p. 469-484.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - The interaction between winter monsoon activities in East Asia and sea surface temperature variations over the western Pacific Ocean
AU - Kawamura, Ryuichi
PY - 1988/1/1
Y1 - 1988/1/1
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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UR - http://www.scopus.com/inward/citedby.url?scp=0024194433&partnerID=8YFLogxK
U2 - 10.4157/grj1984a.61.6_469
DO - 10.4157/grj1984a.61.6_469
M3 - Article
VL - 61
SP - 469
EP - 484
JO - Chirigaku Hyoron/Geographical Review of Japan
JF - Chirigaku Hyoron/Geographical Review of Japan
SN - 1347-9555
IS - 6
ER -