The interaction between winter monsoon activities in East Asia and sea surface temperature variations over the western Pacific Ocean

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5 Citations (Scopus)

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 languageEnglish
Pages (from-to)469-484
Number of pages16
JournalGeographical Review of Japan, Series A
Volume61
Issue number6
DOIs
Publication statusPublished - Jan 1 1988
Externally publishedYes

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heat
monsoon
sea surface temperature
heat budget
winter
longwave radiation
ocean
heat source
heat pump
interaction
advection
budget
convection
heating
anomaly
Asia
analysis
continent
empirical orthogonal function analysis

All Science Journal Classification (ASJC) codes

  • Geography, Planning and Development
  • Earth-Surface Processes

Cite this

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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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