Joint 3D-Wind Retrievals with Stereoscopic Views from MODIS and GOES

被引:18
作者
Carr, James L. [1 ]
Wu, Dong L. [2 ]
Wolfe, Robert E. [2 ]
Madani, Houria [1 ]
Lin, Guoqing [2 ,3 ]
Tan, Bin [2 ,3 ]
机构
[1] Carr Astronaut, 6404 Ivy Lane,Suite 333, Greenbelt, MD 20770 USA
[2] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20770 USA
[3] Sci Syst & Applicat Inc, 10210 Greenbelt Rd,Suite 600, Lanham, MD 20706 USA
关键词
3D-winds; atmospheric motion vectors (AMVs); MODIS; GOES-R; ABI; planetary boundary layer (PBL); stereo imaging; parallax; PERFORMANCE;
D O I
10.3390/rs11182100
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Atmospheric motion vectors (AMVs), derived by tracking patterns, represent the winds in a layer characteristic of the pattern. AMV height (or pressure), important for applications in atmospheric research and operational meteorology, is usually assigned using observed IR brightness temperatures with a modeled atmosphere and can be inaccurate. Stereoscopic tracking provides a direct geometric height measurement of the pattern that an AMV represents. We extend our previous work with multi-angle imaging spectro-radiometer (MISR) and GOES to moderate resolution imaging spectroradiometer (MODIS) and the GOES-R series advanced baseline imager (ABI). MISR is a unique satellite instrument for stereoscopy with nine angular views along track, but its images have a narrow (380 km) swath and no thermal IR channels. MODIS provides a much wider (2330 km) swath and eight thermal IR channels that pair well with all but two ABI channels, offering a rich set of potential applications. Given the similarities between MODIS and VIIRS, our methods should also yield similar performance with VIIRS. Our methods, as enabled by advanced sensors like MODIS and ABI, require high-accuracy geographic registration in both systems but no synchronization of observations. AMVs are retrieved jointly with their heights from the disparities between triplets of ABI scenes and the paired MODIS granule. We validate our retrievals against MISR-GOES retrievals, operational GOES wind products, and by tracking clear-sky terrain. We demonstrate that the 3D-wind algorithm can produce high-quality AMV and height measurements for applications from the planetary boundary layer (PBL) to the upper troposphere, including cold-air outbreaks, wildfire smoke plumes, and hurricanes.
引用
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页数:35
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