Journal
REMOTE SENSING OF ENVIRONMENT
Volume 277, Issue -, Pages -Publisher
ELSEVIER SCIENCE INC
DOI: 10.1016/j.rse.2022.113059
Keywords
Soil moisture; L-band radiometry; SMAP; Deep neural networks
Funding
- Future Investigators in NASA Earth and Space Science and Technology program [80NSSC19K1333]
- Interdisciplinary Science program in Earth Science [80NSSC20K1294]
- Theory of Remote Sensing program [80NSSC20K1717]
- Heinz G. Stefan Fellowship
- Doctoral Dissertation Fellowship from the University of Minnesota
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This paper combines satellite and reanalysis data to develop and validate a new soil moisture product using a deep neural network. The results show that the method performs well in predicting soil moisture for most land cover types and climatic regions, and effectively captures temporal dynamics.
In this paper, it is demonstrated that while satellite soil moisture (SM) retrievals often have minimum biases, reanalysis data can capture more temporal variability of SM, especially for non-cropland areas - when validated against in situ measurements. Accordingly, this paper presents a deep neural network (DNN) that utilizes the merits of a suite of existing satellite and reanalysis products to produce a new SM product with minimum (maximum) bias (correlation) - using NASA's Soil Moisture Active Passive (SMAP) data and ERA5 reanalysis. The benchmark of the network is a bias-adjusted SM with maximum correlation with in situ data over each land cover type. The mean of the benchmark data is adjusted to the product that exhibits a minimum bias over each land-cover type. Consistent with the laws of L-band microwave propagation in soil and canopy, the input variables of DNN include polarized SMAP brightness temperatures, incidence angle, vegetation scattering albedo, surface roughness parameter, surface water fraction, effective soil temperatures, bulk density, clay fraction, and vegetation optical depth from the normalized difference vegetation index (NDVI) climatology. The DNN is trained and validated using two years (04/2015-03/2017) of global data and deployed for assessment of its performance from 04/2017 to 03/2021. The testing results against in situ measurements demonstrate that the DNN outputs typically exhibit improved error quality metrics over most land-cover types and climate regimes and can properly capture SM temporal dynamics, beyond each SMAP product across regional to continental scales.
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