NPOESS aircraft sounder testbed-microwave (NAST-M): Instrument description and initial flight results

被引:32
作者
Blackwell, WJ [1 ]
Barrett, JW
Chen, FW
Leslie, RV
Rosenkranz, PW
Schwartz, MJ
Staelin, DH
机构
[1] MIT, Elect Res Lab, Cambridge, MA 02139 USA
[2] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2001年 / 39卷 / 11期
基金
美国国家航空航天局; 美国国家科学基金会;
关键词
aircraft instrumentation; hurricane images; microwave imaging; microwave radiometry; precipitation; temperature profile retrievals;
D O I
10.1109/36.964981
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 National Polar-Orbiting Operational Environmental Satellite System (NPOESS) aircraft sounder testbed (NAST) has recently been developed and deployed on the NASA ER-2 high-altitude aircraft. The testbed consists of two co-located cross-track scanning instruments: a Fourier transform interferometer spectrometer (NAST-1) [1] with spectral coverage of 3.7-15.5 mum and a passive microwave spectrometer (NAST-M) with 17 channels near the oxygen absorption lines at 50-57 GHz and 118.75 GHz. The testbed provides the first coregistered imagery from high-resolution microwave and infrared sounders and will provide new data that will help 1) validate meteorological satellite environmental data record (EDR) feasibility, 2) define future satellite instrument specifications, and 3) demonstrate operational issues in ground validation, data calibration, and retrievals of meteorological parameters. To help validate the performance and potential of NAST-M, imagery was collected from more than 20 overpasses of hurricanes Bonnie and Earl during the Convection and Moisture Experiment (CAMEX-3), Florida, Summer 1998. The warm core and convection morphology of Hurricane Bonnie (August, 1998) is clearly revealed both by aircraft-based microwave brightness temperature imagery and temperature retrievals within the eye. Radiance comparisons with the Advanced Microwave Sounding Unit (AMSU) on the NOAA-15 satellite and radiosonde observations yield root mean-squared (RMS) agreements of approximately 1 K or less.
引用
收藏
页码:2444 / 2453
页数:10
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