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Analysis of Altimeter Wet Troposphere Range Correction
作者姓名:纪永刚  张杰  姬光荣
作者单位:[1]OceanUniversityofChina,Qingdao266003,China [2]FirstInstitutesofOceanography,StateOceanicAdministration,Qingdao266061,China
基金项目:KeyBasicResearchandDevelopmentProgramofChinaOceancirculationunderlyingdatabaseandoceanicdynamicin formationsystem (No .G19990 43 80 1)
摘    要:Wet path delay caused by tropospheric water vapor must be considered before altimeter data are used in oceanic application. This paper analyzed several methods of atmosphere water range correction (AWRC) using Seasat,Geosat, TOPEX and ERS-1 data, especially the calculated delay path using brightness temperature of TMR on TOPEX and EMR on ERS-1 ; and discussed some other problems of AWRC.

关 键 词:高度计  对流层  海洋调查  海洋资源卫星  水气
收稿时间:4 September 2002
修稿时间:13 May 2003

Analysis of altimeter wet troposphere range correction
Ji?Yonggang,Zhang?Jie,Ji?Guangrong,Zhang?Yonguang.Analysis of Altimeter Wet Troposphere Range Correction[J].Chinese Journal of Oceanology and Limnology,2004,22(2):150-156.
Authors:Ji Yonggang  Zhang Jie  Ji Guangrong  Zhang Yonguang
Institution:(1) Ocean University of China, 266003 Qingdao, China;(2) First Institutes of Oceanography, State Oceanic Administration, 266061 Qingdao, China;(3) Ocean University China, 266003 Qingdao, China
Abstract:Wet path delay caused by tropospheric water vapor must be considered before altimeter data are used in oceanic application. This paper analyzed several methods of atmosphere water range correction (AWRC) using Seasat, Geosat, TOPEX and ERS-1 data, especially the calculated delay path using brightness temperature of TMR on TOPEX and EMR on ERS-1; and discussed some other problems of AWRC.
Keywords:altimeter  atmosphere water range correction  radiometer  brightness temperature  path delay
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