LONG-TERM EVOLUTION OF WAVES IN A COUPLED TMOSPHERE-OCEAN MODEL IN EQUATORIAL REGION

Article Contents

Article Navigation > Haiyang Xuebao > 1982 > 4(3): 267-282

Ji Jinjun. LONG-TERM EVOLUTION OF WAVES IN A COUPLED TMOSPHERE-OCEAN MODEL IN EQUATORIAL REGION[J]. Haiyang Xuebao, 1982, 4(3): 267-282.

Citation:

Ji Jinjun. LONG-TERM EVOLUTION OF WAVES IN A COUPLED TMOSPHERE-OCEAN MODEL IN EQUATORIAL REGION[J]. Haiyang Xuebao, 1982, 4(3): 267-282.

Ji Jinjun. LONG-TERM EVOLUTION OF WAVES IN A COUPLED TMOSPHERE-OCEAN MODEL IN EQUATORIAL REGION[J]. Haiyang Xuebao, 1982, 4(3): 267-282.

Citation:

Ji Jinjun. LONG-TERM EVOLUTION OF WAVES IN A COUPLED TMOSPHERE-OCEAN MODEL IN EQUATORIAL REGION[J]. Haiyang Xuebao, 1982, 4(3): 267-282.

Abstract

The observational facts show that there exist the quasi-periodic fluctuations with time scales of days as well as months in the atmosphere and ocean in equatorial region.To study these phenomena,a coupled atmosphere-ocean model is developed,in which the mixed process in upper layer of the ocean is considered.The non-adiabatic heating comprises Newton radiative cooling and condesation in the atmosphere and the evaporation from sea surface,upwelling in the mixed layer of ocean and short waves radiation to be mbdulated by cloud.