Intercomparisons of Brightness Temperature Observations Over Land From AMSR-E and WindSat

被引:10
|
作者
Das, Narendra Narayan [1 ]
Colliander, Andreas [1 ]
Chan, Steven K. [1 ]
Njoku, Eni G. [1 ]
Li, Li [2 ]
机构
[1] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[2] Naval Res Lab, Washington, DC 20375 USA
来源
基金
美国国家科学基金会; 美国国家航空航天局;
关键词
Passive microwave remote sensing; radiometers; soil moisture; SOIL-MOISTURE RETRIEVAL; RADIOFREQUENCY INTERFERENCE; MICROWAVE RADIOMETER; ICE-SHEET; INSTRUMENT; PERFORMANCE; SIGNATURES; EMISSION; SYSTEM; OCEAN;
D O I
10.1109/TGRS.2013.2241445
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
The Advanced Microwave Scanning Radiometer-EOS (AMSR-E) on Aqua and WindSat on Coriolis instruments have collected multichannel passive microwave data over the global land and oceans since 2002 and 2003, respectively. AMSR-E on Aqua ceased operation in October 2011 due to a malfunction in the antenna scanning mechanism. AMSR-E and WindSat have similar frequencies, bandwidths, polarizations, incidence angles and instantaneous fields of view (IFOVs), but there are some differences in their configurations. The altitudes and local overpass times also differ between the AMSR-E and WindSat sensors. The time series of data from the two instruments have a long period of overlap, which can be used to intercompare and cross-calibrate the instrument data sets taking into account the instrument differences. This would allow retrieval of geophysical parameters using common algorithms that could take advantage of the increased time duration and sampling coverage afforded by combining data from the two sensors. In this paper, we focus on land applications and compare the multichannel data from these two sensors over land. Channels useful primarily for soil moisture and vegetation water content studies (i.e., similar to 6, similar to 10, similar to 18, and similar to 37 GHz at H- and V-pol) are used in the comparisons. To minimize differences caused by surface temperature effects related to local overpass times, only descending passes (with Equator crossing times for AMSR-E of 1: 30 A. M. and WindSat 6: 00 A. M.) are considered. Homogeneous and temporally stable sites such as Dome-C, Antarctica and the Amazon forest, and a flat and bare region in the Sahara desert are chosen to evaluate similarities and differences among comparable channel observations. Taking into consideration the sensor configurations and geophysical conditions during the descending overpasses, reasonably good agreement is observed between AMSR-E and WindSat measurements over the globe.
引用
收藏
页码:452 / 464
页数:13
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