ARISE (Antarctic Remote Ice Sensing Experiment) in the East 2003: Validation of satellite-derived sea-ice data products

被引:27
|
作者
Massom, Robert A. [1 ]
Worby, Anthony [1 ,2 ]
Lytle, Victoria [3 ]
Markus, Thorsten [4 ]
Allison, Ian [1 ,2 ]
Scambos, Theodore [5 ]
Enomoto, Hiroyuki [6 ]
Tateyama, Kazutaka [6 ]
Haran, Terence [5 ]
Comiso, Josefino C. [4 ]
Pfaffling, Andreas [7 ]
Tamura, Takeshi [8 ]
Muto, Atsuhiro [9 ]
Kanagaratnam, Pannir [10 ]
Giles, Barry [1 ,2 ]
Young, Neal [1 ,2 ]
Hyland, Glenn [1 ,2 ]
Key, Erica [11 ]
机构
[1] Univ Tasmania, Antarctic Climate & Ecosyst CRC, Sandy Bay, Tas 7005, Australia
[2] Australian Antarctic Div, Kingston, Tas 7050, Australia
[3] Norwegian Polar Res Inst, Polar Environm Ctr, CIiC Int Project Off, NO-9296 Tromso, Norway
[4] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[5] Univ Colorado, Natl Snow & Ice Data Ctr, Boulder, CO 80309 USA
[6] Kitami Inst Technol, Kitami, Hokkaido 0908507, Japan
[7] Alfred Wegener Inst Polar & Marine Res, D-27515 Bremerhaven, Germany
[8] Hokkaido Univ, Grad Sch Environm Earth Sci, Sapporo, Hokkaido 0600819, Japan
[9] Chiba Univ, Ctr Environm Remote Sensing, Inage Ku, Chiba 2638522, Japan
[10] Univ Kansas, Ctr Remote Sensing Ice Sheets, Lawrence, KS 66045 USA
[11] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, MPO Div, Remote Sensing Lab, Miami, FL 33149 USA
来源
关键词
D O I
10.3189/172756406781811268
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Preliminary results are presented from the first validation of geophysical data products (ice concentration, snow thickness on sea ice (h,) and ice temperature (T-I) from the NASA EOS Aqua AMSR-E sensor, in East Antarctica (in September-October 2003). The challenge of collecting sufficient measurements with which to validate the coarse-resolution AMSR-E data products adequately was addressed by means of a hierarchical approach, using detailed in situ measurements, digital aerial photography and other satellite data. Initial results from a circumnavigation of the experimental site indicate that, at least under cold conditions with a dry snow cover, there is a reasonably close agreement between satellite- and aerial-photo-derived ice concentrations, i.e. 97.2 +/- 3.6% for NT2 and 96.5 +/- 2.5% for BBA algorithms vs 94.3% for the aerial photos. In general, the AMSR-E concentration represents a slight overestimate of the actual concentration, with the largest discrepancies occurring in regions containing a relatively high proportion of thin ice. The AMSR-E concentrations from the NT2 and BBA algorithms are similar on average, although differences of up to 5% occur in places, again related to thin-ice distribution. The AMSR-E ice temperature (TI) product agrees with coincident surface measurements to approximately 0.5 degrees C in the limited dataset analyzed. Regarding snow thickness, the AMSR h(s) retrieval is a significant underestimate compared to in situ measurements weighted by the percentage of thin ice (and open water) present. For the case study analyzed, the underestimate was 46% for the overall average, but 23% compared to smooth-ice measurements. The spatial distribution of the AMSR-E h(s) product follows an expected and consistent spatial pattern, suggesting that the observed difference may be an offset (at least under freezing conditions). Areas of discrepancy are identified, and the need for future work using the more extensive dataset is highlighted.
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页码:288 / +
页数:2
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