@Article{XuYaYaXuHuGoLi:2022:DoSMSo,
author = "Xu, Mengyuan and Yao, Ning and Yang, Haoxuan and Xu, Jia and Hu,
Annan and Gon{\c{c}}alves, Lu{\'{\i}}s Gustavo Gon{\c{c}}alves
de and Liu, Gang",
affiliation = "{China Agricultural University} and {Northwest Agriculture and
Forestry University} and {Tongji University} and {China
Agricultural University} and {University College London} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {China
Agricultural University}",
title = "Downscaling SMAP soil moisture using a wide \& deep learning
method over the Continental United States",
journal = "Journal of Hydrology",
year = "2022",
volume = "609",
pages = "e127784",
month = "June",
keywords = "SMAP, Soil moisture downscaling, The Continental United States,
Wide \& Deep learning method.",
abstract = "Soil moisture (SM) plays a critical role in drought monitoring,
agricultural management, flood forecasting, and other practical
applications. However, the relatively coarse spatial resolutions
of SM products derived from passive microwave satellite retrievals
(approximately 2555 km) greatly hamper their local-scale
applications. In this research, we proposed an SM downscaling
framework based on the Wide \& Deep Learning (WDL) method to
improve the spatial resolution of the level-3 daily composite of
Soil Moisture Active Passive (SMAP) radiometer SM product
(L3_SM_P). In this method, horizontally and vertically polarized
Brightness Temperature (TBh, and TBv, respectively), surface
reflectance and Land Surface Temperature (LST), topographic
attributes, soil properties, climate types, and landcover types
collected in the Continental United States (CONUS) during the
annual unfrozen season (April 1st to November 1st) from 2015 to
2017 were used as auxiliary datasets to downscale the spatial
resolution of the SMAP SM (L3_SM_P) product from its original 36
km to 1 km. Precipitation and in-situ SM measurements obtained
from 211 sites distributed across the International Soil Moisture
Network (ISMN) over the CONUS were utilized to validate the
downscaled SM. The results demonstrated that the correlation (R)
between the downscaled and the in-situ SM ranged from 0.325 to
0.997; the average R value was 0.715. The unbiased Root Mean
Square Error (ubRMSE) values ranged from 0.010 to 0.141 m3/m3,
with an average ubRMSE of 0.041 m3/m3, which meets the accuracy of
SMAP SM requirement of ubRMSE approximately 0.04 m 3/m3. The
downscaled SM also showed good temporal consistency with the
in-situ SM and exhibited a high response to the precipitation
data. The downscaled SM not only maintained high spatial
consistency with the original SMAP SM but also provides more
detailed spatial SM variations.",
doi = "10.1016/j.jhydrol.2022.127784",
url = "http://dx.doi.org/10.1016/j.jhydrol.2022.127784",
issn = "0022-1694",
language = "en",
targetfile = "xu_2022.pdf",
urlaccessdate = "12 maio 2024"
}