{"title":"卫星雷达测高的南极东部冰盖的季节、年际和长期海拔变化","authors":"C. H. Davis, G. Feng","doi":"10.1109/IGARSS.1999.773409","DOIUrl":null,"url":null,"abstract":"Surface elevation measurements from the Seasat (1978) and Geosat (1985-88) satellite altimeters are analyzed for the East Antarctic Ice Sheet (EAIS) from 66-72/spl deg/S and 30-150/spl deg/E. The authors examined seasonal and interannual variations in surface elevation using the first two years of the Geosat-ERM dataset (Nov. 1986 to Nov. 1988). In general, the amplitude of the seasonal signal is /spl plusmn/5 cm. In addition, there is no clear periodicity in the seasonal signal as has been observed in Greenland altimeter data. Interannual variations were determined by dividing each year of the Geosat-ERM data into four 3-month seasons. The results show year-to-year variations of about /spl plusmn/3 cm. Long-term elevation change estimates from 1978-88 were measured by comparing surface elevations from the Seasat and Geosat datasets. The results show that the rate of elevation change, in general, varies spatially from -10 to +10 cm/yr. A spatial average of more than 250,000 elevation-change measurements over an area of 1.8 million km/sup 2/ yields a -3.1/spl plusmn/0.95 cm/yr rate of elevation change.","PeriodicalId":169541,"journal":{"name":"IEEE 1999 International Geoscience and Remote Sensing Symposium. IGARSS'99 (Cat. No.99CH36293)","volume":"38 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1999-06-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Seasonal, interannual, and long-term elevation change of the East Antarctic ice sheet from satellite radar altimetry\",\"authors\":\"C. H. Davis, G. Feng\",\"doi\":\"10.1109/IGARSS.1999.773409\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Surface elevation measurements from the Seasat (1978) and Geosat (1985-88) satellite altimeters are analyzed for the East Antarctic Ice Sheet (EAIS) from 66-72/spl deg/S and 30-150/spl deg/E. The authors examined seasonal and interannual variations in surface elevation using the first two years of the Geosat-ERM dataset (Nov. 1986 to Nov. 1988). In general, the amplitude of the seasonal signal is /spl plusmn/5 cm. In addition, there is no clear periodicity in the seasonal signal as has been observed in Greenland altimeter data. Interannual variations were determined by dividing each year of the Geosat-ERM data into four 3-month seasons. The results show year-to-year variations of about /spl plusmn/3 cm. Long-term elevation change estimates from 1978-88 were measured by comparing surface elevations from the Seasat and Geosat datasets. The results show that the rate of elevation change, in general, varies spatially from -10 to +10 cm/yr. A spatial average of more than 250,000 elevation-change measurements over an area of 1.8 million km/sup 2/ yields a -3.1/spl plusmn/0.95 cm/yr rate of elevation change.\",\"PeriodicalId\":169541,\"journal\":{\"name\":\"IEEE 1999 International Geoscience and Remote Sensing Symposium. IGARSS'99 (Cat. No.99CH36293)\",\"volume\":\"38 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1999-06-28\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"IEEE 1999 International Geoscience and Remote Sensing Symposium. IGARSS'99 (Cat. No.99CH36293)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/IGARSS.1999.773409\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"IEEE 1999 International Geoscience and Remote Sensing Symposium. IGARSS'99 (Cat. No.99CH36293)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/IGARSS.1999.773409","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Seasonal, interannual, and long-term elevation change of the East Antarctic ice sheet from satellite radar altimetry
Surface elevation measurements from the Seasat (1978) and Geosat (1985-88) satellite altimeters are analyzed for the East Antarctic Ice Sheet (EAIS) from 66-72/spl deg/S and 30-150/spl deg/E. The authors examined seasonal and interannual variations in surface elevation using the first two years of the Geosat-ERM dataset (Nov. 1986 to Nov. 1988). In general, the amplitude of the seasonal signal is /spl plusmn/5 cm. In addition, there is no clear periodicity in the seasonal signal as has been observed in Greenland altimeter data. Interannual variations were determined by dividing each year of the Geosat-ERM data into four 3-month seasons. The results show year-to-year variations of about /spl plusmn/3 cm. Long-term elevation change estimates from 1978-88 were measured by comparing surface elevations from the Seasat and Geosat datasets. The results show that the rate of elevation change, in general, varies spatially from -10 to +10 cm/yr. A spatial average of more than 250,000 elevation-change measurements over an area of 1.8 million km/sup 2/ yields a -3.1/spl plusmn/0.95 cm/yr rate of elevation change.