Downscaling SMAP Brightness Temperatures to 3 km Using CYGNSS Reflectivity Observations: Factors That Affect Spatial Heterogeneity
نویسندگان
چکیده
NASA’s Soil Moisture Active Passive (SMAP) mission only retrieved ~2.5 months of 3 km near surface soil moisture (NSSM) before its radar transmitter malfunctioned. NSSM remains an important area study, and multiple applications would benefit from data. With the goal creating a product, we developed algorithm to downscale SMAP brightness temperatures (TBs) using Cyclone Global Navigation Satellite System (CYGNSS) reflectivity The purpose downscaling TB is represent spatial heterogeneity at finer scale than possible via passive microwave data alone. Our SMAP/CYGNSS uses β as scaling factor that adjusts based on variations in CYGNSS reflectivity. spatially varying slope negative linear relationship between emissivity (TB divided by temperature) In this paper, describe uncertainties analyze factors affect patterns β. TBs are more heterogeneous 9 enhanced TBs. median root mean square difference (RMSD) 3.03 K. Additionally, capture expected landscape. Lower (more negative) values yield greater generally found areas with low topographic roughness (<350 m), moderate variance (~0.01–0.0325), low-to-moderate annual precipitation (~0.25–1.5 Normalized Difference Vegetation Indices (~0.2–0.6). lowest croplands grasslands highest forested barren lands.
منابع مشابه
Evaluation of the SMAP brightness temperature downscaling algorithm using active–passive microwave observations
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ژورنال
عنوان ژورنال: Remote Sensing
سال: 2022
ISSN: ['2315-4632', '2315-4675']
DOI: https://doi.org/10.3390/rs14205262