Please use this identifier to cite or link to this item: http://bura.brunel.ac.uk/handle/2438/28197
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dc.contributor.authorLi, X-
dc.contributor.authorLong, D-
dc.contributor.authorSlater, LJ-
dc.contributor.authorMoulds, S-
dc.contributor.authorShahid, M-
dc.contributor.authorHan, P-
dc.contributor.authorZhao, F-
dc.date.accessioned2024-02-04T08:31:03Z-
dc.date.available2024-02-04T08:31:03Z-
dc.date.issued2023-03-08-
dc.identifierORCID iD: Xueying Li https://orcid.org/0000-0002-0910-1954-
dc.identifierORCID iD: Di Long https://orcid.org/0000-0001-9033-5039-
dc.identifierORCID iD: Louise J. Slater https://orcid.org/0000-0001-9416-488X-
dc.identifierORCID iD: Simon Moulds https://orcid.org/0000-0002-7297-482X-
dc.identifierORCID iD: Muhammad Shahid https://orcid.org/0000-0003-0771-4498-
dc.identifiere2022WR033597-
dc.identifier.citationLi, X. et al. (2023) 'Soil Moisture to Runoff (SM2R): A Data-Driven Model for Runoff Estimation Across Poorly Gauged Asian Water Towers Based on Soil Moisture Dynamics', Water Resources Research, 59 (3), e2022WR033597, pp. 1 - 28. doi: 10.1029/2022WR033597.en_US
dc.identifier.issn0043-1397-
dc.identifier.urihttps://bura.brunel.ac.uk/handle/2438/28197-
dc.descriptionData Availability Statement: RA5L reanalysis data (Muñoz Sabater, 2019) are available at https://cds.climate.copernicus.eu/cdsapp#!/dataset/10.24381/cds.68d2bb30 . Data sets from the HWSD (Fischer et al., 2008) are accessed at https://www.fao.org/soils-portal/data-hub/soil-maps-and-databases/harmonized-world-soil-database-v12/en/ . Glacier elevation changes (Berthier et al., 2021) are provided at https://doi.org/10.6096/13 , and the RGI 6.0 glacier mask (RGI Consortium, 2017) can be accessed at https://doi.org/10.7265/4m1f-gd79 . Percentages of persistent snow cover in each water tower (Immerzeel et al., 2019) are provided at https://doi.org/10.5281/zenodo.3521933 . Soil moisture estimated from GLDAS NOAH [Beaudoing and Rodell, 2020; Rodell et al., 2004] and CLSM [B. Li et al., 2019; B. Li et al., 2020] land surface models can be accessed at https://disc.gsfc.nasa.gov/datasets/GLDAS_NOAH025_M_2.1/summary and https://disc.gsfc.nasa.gov/datasets/GLDAS_CLSM025_DA1_D_2.2/summary , respectively. Precipitation estimated from the IMERG product (Huffman et al., 2019) can be accessed at https://disc.gsfc.nasa.gov/datasets/GPM_3IMERGDF_06/summary . Runoff estimation results of this study (Li & Long, 2023) are available at https://doi.org/10.5281/zenodo.7505876 .en_US
dc.descriptionSupporting Information is available online at https://doi.org/10.1029/2022WR033597 .-
dc.description.abstractCopyright © 2022 The Author(s) and American Geophysical Union. Almost 2 billion people depend on freshwater provided by the Asian water towers, yet long-term runoff estimation is challenging in this high-mountain region with a harsh environment and scarce observations. Most hydrologic models rely on observed runoff for calibration, and have limited applicability in the poorly gauged Asian water towers. To overcome such limitations, here we propose a novel data-driven model, SM2R (Soil Moisture to Runoff), to simulate monthly runoff based on soil moisture dynamics using reanalysis forcing data. The SM2R model was applied and examined in 20 drainage basins across seven Asian water towers during the past four decades of 1981–2020. Without invoking any observations for calibration, the overall good performance of SM2R-derived runoff (correlation coefficient ≥0.74 and normalized root mean square error ≤0.22 compared to observed runoff at 20 gauges) suggests considerable potential for runoff simulation in poorly gauged basins. Even though the SM2R model is forced by ERA5-Land (ERA5L) reanalysis data, it largely outperforms the ERA5L-estimated runoff across the seven Asian water towers, particularly in basins with widely distributed glaciers and frozen soil. The SM2R approach is highly promising for constraining hydrologic variables from soil moisture information. Our results provide valuable insights for not only long-term runoff estimation over key Asian basins, but also understanding hydrologic processes across poorly gauged regions globally.en_US
dc.description.sponsorshipSecond Tibetan Plateau Scientific Expedition and Research program. Grant Number: 2019QZKK0105 National Natural Science Foundation of China. Grant Number: 92047301,92047203 UK Research and Innovation. Grant Number: MR/V022008/1en_US
dc.format.extent1 - 28-
dc.format.mediumPrint-Electronic-
dc.languageEnglish-
dc.language.isoen_USen_US
dc.publisherWiley on behalf of American Geophysical Unionen_US
dc.rightsCopyright © 2023 American Geophysical Union. All Rights Reserved. AGU repositories policy – AGU allows the final published article to be placed in an institutional repository six months after publication and allows submitted articles to be accessible on the author’s personal website. [see AGU policy at: https://www.agu.org/Publish-with-AGU/Publish/Author-Resources/Policies/Prior-Publication-Policy.]-
dc.rights.urihttps://www.agu.org/Publish-with-AGU/Publish/Author-Resources/Policies/Prior-Publication-Policy-
dc.subjectrunoff estimationen_US
dc.subjectsoil moisture dynamicsen_US
dc.subjectthe Asian water towersen_US
dc.titleSoil Moisture to Runoff (SM2R): A Data-Driven Model for Runoff Estimation Across Poorly Gauged Asian Water Towers Based on Soil Moisture Dynamicsen_US
dc.typeArticleen_US
dc.identifier.doihttps://doi.org/10.1029/2022WR033597-
dc.relation.isPartOfWater Resources Research-
pubs.issue3-
pubs.publication-statusPublished-
pubs.volume59-
dc.identifier.eissn1944-7973-
dc.rights.holderAmerican Geophysical Union-
Appears in Collections:Dept of Civil and Environmental Engineering Research Papers

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