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A snowfall map can represent how snow depth varies across a region, such as Colorado, over a fixed time period. Since different locations may receive different amounts of snow, the snowfall depth is described by a function of two variables. If f(x,y) represents the snow depth at a point in a rectangular region, then the average snowfall over the entire region is found by comparing the total accumulated snowfall with the area being measured.Total Snowfall over a RegionThe total snowfall over a...

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A reduced latency regional gap-filling method for SMAP using random forest regression.

Xiaoyi Wang1,2, Haishen Lü1,2, Wade T Crow3

  • 1State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, National Cooperative Innovation Center for Water Safety and Hydro-science, College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China.

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|January 9, 2023
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Summary

This study fills data gaps in Soil Moisture Active/Passive (SMAP) L3 soil moisture products using random forest models and near-real-time data. This enhances the spatiotemporal support for SMAP soil moisture data in crop-dominated regions.

Keywords:
Earth sciencesRemote sensingSoil science

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Area of Science:

  • Earth Science
  • Remote Sensing
  • Hydrology

Background:

  • The Soil Moisture Active/Passive (SMAP) mission provides crucial satellite-based soil moisture data.
  • Large spatial-temporal data gaps in SMAP products hinder near-real-time (NRT) applications.
  • Effective gap-filling methods are needed to improve the utility of SMAP soil moisture data.

Purpose of the Study:

  • To develop and validate a method for filling data gaps in the SMAP L3 soil moisture product.
  • To enhance the spatiotemporal coverage of SMAP soil moisture data for NRT applications.
  • To utilize NRT operational metadata and surface parameterization for soil moisture retrieval.

Main Methods:

  • Employed a random forest model to retrieve missing SMAP L3 soil moisture values.
  • Utilized NRT operational metadata (precipitation, skin temperature) and surface parameterization.
  • Tested the gap-filling method on SMAP descending (6 AM) and ascending (6 PM) orbits in a crop-dominated area (2015-2019).
  • Validated gap-filled estimates against in situ data and using triple collocation analysis.

Main Results:

  • Optimized random forest models achieved a high goodness of fit (R² ≥ 0.86).
  • The gap-filling scheme effectively addressed missing data points in SMAP L3 soil moisture.
  • Validation confirmed the reliability of the gap-filled soil moisture estimates.

Conclusions:

  • The proposed gap-filling scheme successfully enhances the spatiotemporal support for SMAP L3 soil moisture data.
  • This method, driven by low-latency data, offers a viable solution for NRT applications.
  • The study demonstrates the potential of machine learning approaches for improving satellite soil moisture data.