Estimating High-Resolution Groundwater Storage from GRACE: A Random Forest Approach

Gravity Recovery and Climate Experiment (GRACE) data have become a widely used global dataset for evaluating the variability in groundwater storage for the different major aquifers. Moreover, the application of GRACE has been constrained to the local scale due to lower spatial resolution. The curren...

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Main Authors: Md Mafuzur Rahaman, Balbhadra Thakur, Ajay Kalra, Ruopu Li, Pankaj Maheshwari
Format: Article
Language:English
Published: MDPI AG 2019-06-01
Series:Environments
Subjects:
Online Access:https://www.mdpi.com/2076-3298/6/6/63
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spelling doaj-20ee3fb72752467e93f4950001b91f392020-11-25T01:14:03ZengMDPI AGEnvironments2076-32982019-06-01666310.3390/environments6060063environments6060063Estimating High-Resolution Groundwater Storage from GRACE: A Random Forest ApproachMd Mafuzur Rahaman0Balbhadra Thakur1Ajay Kalra2Ruopu Li3Pankaj Maheshwari4Department of Civil and Environmental Engineering, Southern Illinois University, 1230 Lincoln Drive, Carbondale, IL 62901, USADepartment of Civil and Environmental Engineering, Southern Illinois University, 1230 Lincoln Drive, Carbondale, IL 62901, USADepartment of Civil and Environmental Engineering, Southern Illinois University, 1230 Lincoln Drive, Carbondale, IL 62901, USADepartment of Geography and Environmental Resources, Southern Illinois University, 1000 Faner Drive, Carbondale, IL 62901, USATransportation Engineer, Louis Berger, 444 E. Warm Springs Road, Suite 118, Las Vegas, NV 89119, USAGravity Recovery and Climate Experiment (GRACE) data have become a widely used global dataset for evaluating the variability in groundwater storage for the different major aquifers. Moreover, the application of GRACE has been constrained to the local scale due to lower spatial resolution. The current study proposes Random Forest (RF), a recently developed unsupervised machine learning method, to downscale a GRACE-derived groundwater storage anomaly (GWSA) from 1° × 1° to 0.25° × 0.25° in the Northern High Plains aquifer. The RF algorithm integrated GRACE to other satellite-based geospatial and hydro-climatological variables, obtained from the Noah land surface model, to generate a high-resolution GWSA map for the period 2009 to 2016. This RF approach replicates local groundwater variability (the combined effect of climatic and human impacts) with acceptable Pearson correlation (0.58 ~ 0.84), percentage bias (−14.67 ~ 2.85), root mean square error (15.53 ~ 46.69 mm), and Nash-Sutcliffe efficiency (0.58 ~ 0.84). This developed RF model has significant potential to generate finer scale GWSA maps for managing groundwater at both local and regional scales, especially for areas with sparse groundwater monitoring wells.https://www.mdpi.com/2076-3298/6/6/63GRACERandom ForestNorthern High Plains aquiferland surface model
collection DOAJ
language English
format Article
sources DOAJ
author Md Mafuzur Rahaman
Balbhadra Thakur
Ajay Kalra
Ruopu Li
Pankaj Maheshwari
spellingShingle Md Mafuzur Rahaman
Balbhadra Thakur
Ajay Kalra
Ruopu Li
Pankaj Maheshwari
Estimating High-Resolution Groundwater Storage from GRACE: A Random Forest Approach
Environments
GRACE
Random Forest
Northern High Plains aquifer
land surface model
author_facet Md Mafuzur Rahaman
Balbhadra Thakur
Ajay Kalra
Ruopu Li
Pankaj Maheshwari
author_sort Md Mafuzur Rahaman
title Estimating High-Resolution Groundwater Storage from GRACE: A Random Forest Approach
title_short Estimating High-Resolution Groundwater Storage from GRACE: A Random Forest Approach
title_full Estimating High-Resolution Groundwater Storage from GRACE: A Random Forest Approach
title_fullStr Estimating High-Resolution Groundwater Storage from GRACE: A Random Forest Approach
title_full_unstemmed Estimating High-Resolution Groundwater Storage from GRACE: A Random Forest Approach
title_sort estimating high-resolution groundwater storage from grace: a random forest approach
publisher MDPI AG
series Environments
issn 2076-3298
publishDate 2019-06-01
description Gravity Recovery and Climate Experiment (GRACE) data have become a widely used global dataset for evaluating the variability in groundwater storage for the different major aquifers. Moreover, the application of GRACE has been constrained to the local scale due to lower spatial resolution. The current study proposes Random Forest (RF), a recently developed unsupervised machine learning method, to downscale a GRACE-derived groundwater storage anomaly (GWSA) from 1° × 1° to 0.25° × 0.25° in the Northern High Plains aquifer. The RF algorithm integrated GRACE to other satellite-based geospatial and hydro-climatological variables, obtained from the Noah land surface model, to generate a high-resolution GWSA map for the period 2009 to 2016. This RF approach replicates local groundwater variability (the combined effect of climatic and human impacts) with acceptable Pearson correlation (0.58 ~ 0.84), percentage bias (−14.67 ~ 2.85), root mean square error (15.53 ~ 46.69 mm), and Nash-Sutcliffe efficiency (0.58 ~ 0.84). This developed RF model has significant potential to generate finer scale GWSA maps for managing groundwater at both local and regional scales, especially for areas with sparse groundwater monitoring wells.
topic GRACE
Random Forest
Northern High Plains aquifer
land surface model
url https://www.mdpi.com/2076-3298/6/6/63
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AT ajaykalra estimatinghighresolutiongroundwaterstoragefromgracearandomforestapproach
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