Separating snow and forest temperatures with thermal infrared remote sensing

被引:31
作者
Lundquist, Jessica D. [1 ]
Chickadel, Chris [2 ]
Cristea, Nicoleta [1 ]
Currier, William Ryan [1 ]
Henn, Brian [1 ,3 ]
Keenan, Eric [1 ]
Dozier, Jeff [4 ]
机构
[1] Univ Washington, Civil & Environm Engn, Seattle, WA 98195 USA
[2] Univ Washington, Appl Phys Lab, Seattle, WA 98105 USA
[3] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA
[4] Univ Calif Santa Barbara, Bren Sch Environm Sci & Management, Santa Barbara, CA 93106 USA
关键词
Thermal infrared; MODIS; Land surface temperature; Fractional snow covered area; Mixed pixel; Forest temperature; Snow surface temperature; LAND-SURFACE TEMPERATURE; INCOMING LONGWAVE RADIATION; IN-SITU; MODIS; AIR; EMISSIVITY; COVER; CLIMATE; MODEL; ICE;
D O I
10.1016/j.rse.2018.03.001
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Thermal infrared sensing from space is a well-developed field, but mixed pixels pose a problem for many applications. We present a field study in Dana Meadows, Yosemite National Park, California to scale from point (similar to 2-m resolution) to aerial (similar to 5-m resolution gridded, 1 km x 6 km extent) to satellite (MODIS, similar to 1000-m resolution, global extent) observations. We demonstrate how multiple thermal bands on MODIS can be used to separate snow and forest temperatures and determine the fractional snow-covered area (f(scA)) over a 3 km x 3 km array of 9 MODIS grid cells. During the day, visible, near-infrared, and shortwave-infrared bands provide a first guess of f(scA) and help to constrain the solution. This technique, which has estimated errors < 2 degrees C and 10% f(scA) for many expected conditions, enables better understanding of the snowpack energy balance, atmospheric inversions and cold air pools, and forest health.
引用
收藏
页码:764 / 779
页数:16
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