Mon Oct 13, F. Flechtner
• Sorted by Date • Sorted by Last Name of First Author •
Xie, Huan, Li, Rongxing, Tong, Xiaohua, Ju, Xiaolei, Liu, Jun, Shen, Yunzhong, Chen, Lei, Liu, Shijie, Sun, Bo, Cui, Xiangbin, Tian, Yixiang, and Ye, Wenkai, 2016. A comparative study of changes in the Lambert Glacier/Amery Ice Shelf system, East Antarctica, during 2004-2008 using gravity and surface elevation observations. Journal of Glaciology, 62(235):888–904, doi:10.1017/jog.2016.76.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2016JGlac..62..888X,
author = {{Xie}, Huan and {Li}, Rongxing and {Tong}, Xiaohua and {Ju}, Xiaolei and {Liu}, Jun and {Shen}, Yunzhong and {Chen}, Lei and {Liu}, Shijie and {Sun}, Bo and {Cui}, Xiangbin and {Tian}, Yixiang and {Ye}, Wenkai},
title = "{A comparative study of changes in the Lambert Glacier/Amery Ice Shelf system, East Antarctica, during 2004-2008 using gravity and surface elevation observations}",
journal = {Journal of Glaciology},
year = 2016,
month = oct,
volume = {62},
number = {235},
pages = {888-904},
abstract = "{We present results of a regional comparative study of surface mass
changes from 2004 to 2008 based on Gravity Recovery and Climate
Experiment (GRACE), The Ice, Cloud and Land Elevation Satellite
(ICESat) and CHINARE observations over the Lambert Glacier/Amery
Ice Shelf system (LAS). Estimation of the ICESat mass change
rates benefitted from the density measurements along the CHINARE
traverse and a spatial density adjustment method for reducing
the effect of spatial density variations. In the high-elevation
inland region, a positive trend was estimated from both ICESat
and GRACE data, which is in line with the CHINARE accumulation
measurements. In the coastal region, there were areas with high
level accumulations in both ICESat and GRACE trend maps. In many
high flow-speed glacier areas, negative mass change rates may be
caused by dynamic ice flow discharges that have surpassed the
snow accumulation. Overall, the mass change rate estimate in the
LAS of 2004-2008 from the GRACE, ICESat and CHINARE data is 5.41
{\ensuremath{\pm}} 4.59 Gt a{\ensuremath{-}}1, indicating a
balanced to slightly positive mass trend. Along with other
published results, this suggests that a longer-term positive
mass trend in the LAS may have slowed in recent years.}",
doi = {10.1017/jog.2016.76},
adsurl = {https://ui.adsabs.harvard.edu/abs/2016JGlac..62..888X},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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