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《Chinese Journal of Geophysics》 2011-06
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Effects of glacial isostatic adjustment on the estimate of ice mass balance over Antarctica and the uncertainties

JIA Lu-Lu~(1,2),WANG Han-Sheng~(1*),XIANG Long-Wei~(1,2),WU Patrick~3,LI Fei~4,SHI Hong-Ling~(1,2)1 Key Laboratory of Dynamical Geodesy,Institute of Geodesy and Geophysics,Chinese Academy of Sciences,Wuhan 430077,China2 Graduate University of Chinese Academy of Sciences,Beijing 100049,China3 Department of Geoscience,University of Calgary,Calgary T2N 1JV4,Canada4 Chinese Antarctic Center of Surveying and Mapping,Wuhan 430079,China  
The effects of glacial isostatic adjustment (GIA)on monitoring ice mass balance over Antarctica are investigated using our newly-released GIA model ICE-4G +RF3L20 (β= 0.4)and the uncertainties are evaluated by considering the effects of differences in ice load models and reference mantle viscosities.The results and the comparison with those from GRACE timevarying gravity fields and satellite altimetry data are shown as follows.It is found that the GIA has strong effects on monitoring the changes of equivalent water height (EWH)from GRACE gravity data,significant GIA effects occur at Ross Ice Shelf,Kamb Ice Stream,Ronne Ice Shelf and Antarctic Peninsula with a maximal magnitude of ~29.8 mm/a at Kamb Ice Stream.For the whole Antarctica,the effect of GIA on total ice mass balance is 134 + 28 Gt/a.The differences in ice models account for 88.4% of the variances of uncertainties while the differences in viscosity models contribute 11.6%.In some typical regions,the changes of EWH monitored by GRACE data are given before and after GIA corrections.These are ~32.8 mm/a and ~6.3 mm/a for Kamb Ice Stream,~-95.3 mm/a and ~-102.5 mm/a for Amundsen Sea Embayment,~13.6 mm/a and ~-8.1 mm/a for Enderby Land.The total ice mass change of the whole Antarctica is found to be ~ 82 + 29 Gt/a after GIA corrections which is quite close to that estimated from satellite altimetry data.Furthermore,the effects of GIA on the ice height changes observed from ICESat are less than 8%.The results related to our new GIA model in this paper can be utilized to precisely monitor the present ice mass balance in Antarctica from space geodetic techniques.
【Fund】: 国家杰出青年科学基金(40825012);; 国家基金创新研究群体科学基金项目(41021003)资助;; WUPatrick由加拿大NSERC的OperatingGrant资助
【CateGory Index】: P343.6
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