Abstract
Soil moisture (SM) downscaling has been extensively investigated in recent years to improve coarse resolution of SM products. However, available methods for downscaling are generally based on pixel-to-pixel strategy, which ignores the information among pixels. Hence, a new downscaling method based on a convolutional neural network (CNN) is proposed to solve the problem. Furthermore, a weight layer is designed for the input, and residual SM is treated as the output of the CNN to improve the accuracy. This method is applied to downscale Soil Moisture Active Passive (SMAP) SM products (i.e., 36-km $\mathbf {L3{\_}SM{\_}P}$ and 9-km $\mathbf {L3{\_}SM{\_}P{\_}E}$ ) from January 1, 2018 to December 30, 2018. Compared with 9-km $\mathbf {L3{\_}SM{\_}P{\_}E}$ , the 9-km downscaling result is satisfactory with obtained correlation coefficient ( $R$ ), root mean square error (RMSE), and unbiased RMSE (ubRMSE) values of 95.81%, 2.77%, and 2.67%, respectively. Moreover, SMAP SM products (36 and 9 km) and downscaling SM (3 and 1 km) are validated by the in situ data, which are collected by the 109 stations of the Oklahoma Mesonet SM monitoring network. Mean $R$ , RMSE, and ubRMSE values are 67.92%, 7.94%, and 4.87% for 36-km $\mathbf {L3{\_}SM{\_}P}$ ; 67.78%, 8.35%, and 4.95% for 9-km $\mathbf {L3{\_}SM{\_}P{\_}E}$ ; 67.28%, 8.34%, and 4.97% for 3-km downscaling SM; 65.90%, 8.40%, and 5.18% for 1-km downscaling SM, respectively. The 3-km downscaling SM generated by this method can improve the coarse resolution of 9-km $\mathbf {L3{\_}SM{\_}P{\_}E}$ while preserving its accuracy. However, error will remarkably increase in the 1-km downscaling SM. Therefore, the proposed method provides a new strategy for SM downscaling and obtains satisfactory results in practice. Additional studies can be conducted in the future.
Highlights
S OIL moisture (SM) content is an important parameter in hydrological, meteorological, and agricultural applications [1], and its spatial–temporal dynamics play a crucial role in agricultural drought monitoring [2], climate change [3], and efficient management of water resources [4]
In situ data collected from Oklahoma Mesonet (OKM) are subsequently utilized to evaluate 3- and 1-km downscaling SM, as well as 36-km L3_SM_P and 9-km L3_SM_P_E
CNN_N performs significantly better than CNN_O
Summary
S OIL moisture (SM) content is an important parameter in hydrological, meteorological, and agricultural applications [1], and its spatial–temporal dynamics play a crucial role in agricultural drought monitoring [2], climate change [3], and efficient management of water resources [4]. Advanced Microwave Scanning Radiometer 2 (AMSR-2) [6], the Soil Moisture and Ocean Salinity [7], and the Soil Moisture Active Passive (SMAP) [8], [9], show high potential in various studies involving large-scale and long-term monitoring or spatial–temporal dynamical analyses of SM. The National Aeronautics and Space Administration (NASA) proposed SMAP mission to provide daily and moderate spatial resolution SM products using the L-band radiometer and radar together. The L-band radiometer and radar can provide 36- and 3-km observations, respectively, to generate corresponding SM products. A 9-km SM product can be produced through the active and passive joint retrieval algorithm This mission provided a potential way to estimate global SM in moderate resolution based on active and passive data and attracted much interest. The L-band radar ceased operations since July 2015
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