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Farn Parungo,Clarence Nagamoto,Cecilia M. I. R. Girz,Jeff Torgerson,Zhou Mingyu. 1995. Observation of clouds and solar radiation over the Pacific Ocean as relation to global climate. Acta Oceanologica Sinica, (2):201-207
Observation of clouds and solar radiation over the Pacific Ocean as relation to global climate
Observation of clouds and solar radiation over the Pacific Ocean as relation to global climate
Received:January 11, 1995  Revised:March 01, 1995
DOI:
Key words:Solar irradiance  cloud type  cloud cover  earth's surface insolation  global climate
中文关键词:  Solar irradiance  cloud type  cloud cover  earth's surface insolation  global climate
基金项目:
Author NameAffiliation
Farn Parungo Science and Technology Corporation, Boulder, CO, U.S.A. 
Clarence Nagamoto Air Resources Laboratory, NOAA, Boulder, CO, U.S.A. 
Cecilia M. I. R. Girz Forecast Systems Laboratory, NOAA, Boulder, CO, U.S.A. 
Jeff Torgerson Universal Weather and Aviation, White Plarins, N. Y., U.S.A. 
Zhou Mingyu National Research Center for Marine Environmental Forecasts, State Oceanic Administration, Beijing 100081, China 
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Abstract:
      During a research cruise over the Pacific Ocean in 1989, solar irradiance was measured with a broad-band pyranometer along the cruise track.Cloud cover was photographed with an all-sky time-lapse camera.Cloud types were observed and recorded.The data show that both the types and the amounts of clouds affeet radiation fluxes on the sea surface.For low-level and middle-level clouds, the correlations (r) between measured irradiance (in percent of calculated maximum irradiance) and cloud amount (in fraction of sky) were significant:r=-0.79 and -0.66, respectively.For high-level clouds, the correlation was not significant;r=-0.21.The results indicate that cloud shortwave forcing is a major modifier of the earth's surface insulation and change of cloud amount may affect global climate.
中文摘要:
      During a research cruise over the Pacific Ocean in 1989, solar irradiance was measured with a broad-band pyranometer along the cruise track.Cloud cover was photographed with an all-sky time-lapse camera.Cloud types were observed and recorded.The data show that both the types and the amounts of clouds affeet radiation fluxes on the sea surface.For low-level and middle-level clouds, the correlations (r) between measured irradiance (in percent of calculated maximum irradiance) and cloud amount (in fraction of sky) were significant:r=-0.79 and -0.66, respectively.For high-level clouds, the correlation was not significant;r=-0.21.The results indicate that cloud shortwave forcing is a major modifier of the earth's surface insulation and change of cloud amount may affect global climate.
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