Quantifying the potential of using Soil Moisture Active Passive (SMAP) soil moisture variability to predict subsurface water dynamics

被引:0
|
作者
Nayak, Aruna Kumar [1 ]
Xu, Xiaoyong [1 ,2 ]
Frey, Steven K. [3 ,4 ]
Khader, Omar [3 ,5 ]
Erler, Andre R. [3 ]
Lapen, David R. [6 ]
Russell, Hazen A.J. [7 ]
Sudicky, Edward A. [3 ,4 ]
机构
[1] Department of Chemical and Physical Sciences, University of Toronto Mississauga, Mississauga,ON, Canada
[2] Department of Geography, Geomatics and Environment, University of Toronto Mississauga, Mississauga,ON, Canada
[3] Aquanty, Waterloo,ON, Canada
[4] Department of Earth and Environmental Sciences, University of Waterloo, Waterloo,ON, Canada
[5] Department of Water and Water Structural Engineering, Zagazig University, Al Sharqia, Egypt
[6] Agriculture and Agri-Food Canada, Ottawa Research and Development Centre, Ottawa,ON, Canada
[7] Natural Resources Canada, Ottawa,ON, Canada
基金
美国国家航空航天局;
关键词
Fertilizers - Groundwater resources - Soil moisture - Soil surveys - Surface water resources - Surface waters - Tropics;
D O I
10.5194/hess-29-215-2025
中图分类号
学科分类号
摘要
Advances in satellite Earth observation have opened up new opportunities for global monitoring of soil moisture (SM) at fine to medium resolution, but satellite remote sensing can only measure the near-surface soil moisture (SSM). As such, it is critically important to examine the potential of satellite SSM measurements to derive the water resource variations in deeper subsurface. This study compares the SSM variability captured by the Soil Moisture Active and Passive (SMAP) satellite and the Soil Water Index (SWI) derived from SMAP SSM with subsurface SM and groundwater (GW) dynamics simulated by a high-resolution fully integrated surface water-groundwater model over an agriculturally dominated watershed in eastern Canada across two spatial scales, namely SMAP product grid (9 km) and watershed (∼4000 km2). SMAP measurements compare well with the hydrologic simulations in terms of SSM variability at both scales. Simulated subsurface SM and GW storage show lagged and smoother characteristics relative to SMAP SSM variability with an optimal delay of ∼1 d for the 25-50 cm SM, ∼6 d for the 50-100 cm SM, and ∼11 d for the GW storage for both scales. Modeled subsurface SM dynamics agree well with the SWI derived from SMAP SSM using the classic characteristic time lengths (15 d for the 0-25 cm layer and 20 d for the 0-100 cm layer). The simulated GW storage showed a slightly delayed variation relative to the derived SWI. The quantified optimal characteristic time length Topt for SWI estimation (by matching the variations in SMAP-derived SWI and modeled root zone SM) is comparable to Topt obtained in other agricultural regions around the world. This work demonstrates SMAP SM measurements as a potentially useful aid when predicting root zone SM and GW dynamics and validating fully integrated hydrologic models across different spatial scales. This study also provides insights into the dynamics of near-surface-subsurface water interaction and the capabilities and approaches of satellite-based SM monitoring and high-resolution fully integrated hydrologic modeling. © 2025 Aruna Kumar Nayak et al.
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页码:215 / 244
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