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OBSERVATIONAL STUDY OF MERIDIONAL VARIATION OF UV-B RADIATION DURING VOYAGES TO THE ARCTIC AND ANTARCTIC REGIONS
作者姓名:陆龙骅  卞林根  逯昌贵  程彦杰
作者单位:Chinese Academy of Meteorological Sciences Beijing 100081,Chinese Academy of Meteorological Sciences,Beijing 100081,Chinese Academy of Meteorological Sciences,Beijing 100081,Chinese Academy of Meteorological Sciences,Beijing 100081
基金项目:Sponsored jointly by the 1996-2000 Sci./Tech.Rainstorm Project of China,the Arctic Research Program and the National Natural Science Foundation of China(No.49975006).
摘    要:Based on 1999-2000 observations made by the first Arctic and sixteenth Antactic scientificvoyages,a study is undertaken about the meridional surface UV-B (B band ultraviolet rays)variations in 75°N-70°S.It is mitigated as a function of latitudes and marked by lower radiationaveraged over the Northern Hemisphere (NH) than over the Southern Hemisphere (SH),with itsdaily course basically similar to that of total radiation.Around polar summer noon hours (localtime) and where ice albedo is maximum,the strongest UV-B irradiance on the surfaceperpendicular to sun's beams as found at equatorial latitudes is measured sometimes.In the areasnear Zhongshan Station the increase of surface UV-B radiation shows a close relation to thedecrease of ozone in the higher atmosphere but it has a less intimate relation with its concentrationat ground.


OBSERVATIONAL STUDY OF MERIDIONAL VARIATION OF UV-B RADIATION DURING VOYAGES TO THE ARCTIC AND ANTARCTIC REGIONS
LU Longhua BIAN Lingen LU Changgui CHENG Yanjie Chinese Academy of Meteorological Sciences,Beijing.OBSERVATIONAL STUDY OF MERIDIONAL VARIATION OF UV-B RADIATION DURING VOYAGES TO THE ARCTIC AND ANTARCTIC REGIONS[J].Acta Meteorologica Sinica,2002(2).
Authors:LU Longhua BIAN Lingen LU Changgui CHENG Yanjie Chinese Academy of Meteorological Sciences  Beijing
Institution:LU Longhua BIAN Lingen LU Changgui CHENG Yanjie Chinese Academy of Meteorological Sciences,Beijing 100081
Abstract:
Keywords:polar region  UV-B radiation  meridional variation  daily variation  ozone
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