Quantitative Assessment of Satellite L-Band Vegetation Optical Depth in the US Corn Belt

被引:4
|
作者
Togliatti, Kaitlin [1 ]
Lewis-Beck, Colin [2 ]
Walker, Victoria A. [3 ]
Hartman, Theodore [1 ]
VanLoocke, Andy [1 ]
Cosh, Michael H. [4 ]
Hornbuckle, Brian K. [1 ]
机构
[1] Iowa State Univ Sci & Technol, Dept Agron, Ames, IA 50011 USA
[2] Univ Iowa, Dept Stat & Actuarial Sci, Iowa City, IA 52242 USA
[3] Univ Montana, Numer Terradynam Simulat Grp, Missoula, MT 59812 USA
[4] USDA ARS, Hydrol & Remote Sensing Lab, Beltsville, MD 20705 USA
关键词
L-band; satellite microwave radiometry; soil moisture active passive (SMAP); soil moisture and ocean salinity (SMOS); vegetation optical depth (VOD); SOIL-MOISTURE; MICROWAVE EMISSION; DATA SETS; SMOS; PRODUCTS; BIOMASS;
D O I
10.1109/LGRS.2020.3034174
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
Satellite L-band vegetation optical depth (L-VOD) contains new information about terrestrial ecosystems. However, it has not been evaluated against the geophysical variable that it represents, plant water, the mass of liquid water contained within vegetation tissue per ground area. We quantitatively assess the seasonal variation of three L-VOD products at the South Fork Core Validation Site in the Corn Belt state of Iowa where L-VOD is directly proportional to crop plant water. We use three satellite-scale crop plant water estimates: in situ measurements; a normalized difference water index (NDWI) calibrated with in situ measurements; and a crop model. We find that overall the L-VOD satellite products are 0.02-0.09 Np (0.4-1.7 kg . m(-2)) lower than the three estimates. We show that overestimation of L-VOD can be attributed to dynamic soil surface roughness, and hypothesize that crop plant water observations will require the incorporation of this effect into retrieval algorithms.
引用
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页数:5
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