Decomposing impact of climate change and land surface alterations on catchment hydrology in Eastern Himalaya
Abstract Climate change is intensifying water challenges in the Eastern Himalayas. Bridging climate change and water demand is vital, especially in India’s ungauged Himalayan catchments. The proposed novel method aims to differentiate climate change and anthropogenic activity impacts on catchment hy...
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| Autor*in: |
Singh, Himani [verfasserIn] Sinha, Vinay Shankar Prasad [verfasserIn] Gaur, Shishir [verfasserIn] Khanduja, Ekansha [verfasserIn] Mathur, Anandi [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2024 |
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| Schlagwörter: |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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| Übergeordnetes Werk: |
Enthalten in: Environmental earth sciences - Springer Berlin Heidelberg, 2009, 83(2024), 16 vom: Aug. |
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| Übergeordnetes Werk: |
volume:83 ; year:2024 ; number:16 ; month:08 |
| Links: |
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| DOI / URN: |
10.1007/s12665-024-11748-2 |
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| Katalog-ID: |
SPR056830882 |
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| 520 | |a Abstract Climate change is intensifying water challenges in the Eastern Himalayas. Bridging climate change and water demand is vital, especially in India’s ungauged Himalayan catchments. The proposed novel method aims to differentiate climate change and anthropogenic activity impacts on catchment hydrology. In this study, evaporative demand was assessed by coupling SWAT and Budyko framework at the micro-watershed scale for understanding climate and surface changes in local hydrology. The coupled model considers climate parameters through SWAT to decompose the impacts of climate change and anthropogenic activities on watershed hydrology. The Budyko framework depicted the relationship between precipitation, evapotranspiration (ET), and potential evapotranspiration (PET) resulting in partitioning evaporative demand into green and blue ET. Parameters like d-statistics, responsivity, and elasticity assessed the buffer capacity of catchments against climate change. The study unveiled catchment characteristic (ω) values within the range of 1.70–1.56 from 2005 to 2030, indicative of a discernible shift in hydrological patterns attributed to changes in land use land cover (LULC) and climate variables. The investigation underscored the significant impact of LULC changes, manifesting as a reduction in snow and glacier cover alongside an augmentation in blue ET. The variation in precipitation, LULC, PET, and temperature were identified as primary influencers on hydrological regimes, rendering watersheds increasingly susceptible to climatic variations. Six catchments are unable to cope with or buffer against climate change and have low coping capacity. The study emphasizes the exigency to water resource management in ecologically delicate Eastern Himalayan ecosystem. | ||
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10.1007/s12665-024-11748-2 doi (DE-627)SPR056830882 (SPR)s12665-024-11748-2-e DE-627 ger DE-627 rakwb eng 550 VZ 38.95 bkl Singh, Himani verfasserin aut Decomposing impact of climate change and land surface alterations on catchment hydrology in Eastern Himalaya 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Climate change is intensifying water challenges in the Eastern Himalayas. Bridging climate change and water demand is vital, especially in India’s ungauged Himalayan catchments. The proposed novel method aims to differentiate climate change and anthropogenic activity impacts on catchment hydrology. In this study, evaporative demand was assessed by coupling SWAT and Budyko framework at the micro-watershed scale for understanding climate and surface changes in local hydrology. The coupled model considers climate parameters through SWAT to decompose the impacts of climate change and anthropogenic activities on watershed hydrology. The Budyko framework depicted the relationship between precipitation, evapotranspiration (ET), and potential evapotranspiration (PET) resulting in partitioning evaporative demand into green and blue ET. Parameters like d-statistics, responsivity, and elasticity assessed the buffer capacity of catchments against climate change. The study unveiled catchment characteristic (ω) values within the range of 1.70–1.56 from 2005 to 2030, indicative of a discernible shift in hydrological patterns attributed to changes in land use land cover (LULC) and climate variables. The investigation underscored the significant impact of LULC changes, manifesting as a reduction in snow and glacier cover alongside an augmentation in blue ET. The variation in precipitation, LULC, PET, and temperature were identified as primary influencers on hydrological regimes, rendering watersheds increasingly susceptible to climatic variations. Six catchments are unable to cope with or buffer against climate change and have low coping capacity. The study emphasizes the exigency to water resource management in ecologically delicate Eastern Himalayan ecosystem. Climate change (dpeaa)DE-He213 Eastern Himalayas (dpeaa)DE-He213 Ungauged watershed (dpeaa)DE-He213 Evaporative demand (dpeaa)DE-He213 Budyko framework (dpeaa)DE-He213 Sinha, Vinay Shankar Prasad verfasserin (orcid)0000-0001-8387-8625 aut Gaur, Shishir verfasserin aut Khanduja, Ekansha verfasserin aut Mathur, Anandi verfasserin aut Enthalten in Environmental earth sciences Springer Berlin Heidelberg, 2009 83(2024), 16 vom: Aug. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:83 year:2024 number:16 month:08 https://dx.doi.org/10.1007/s12665-024-11748-2 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.95 VZ AR 83 2024 16 08 |
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10.1007/s12665-024-11748-2 doi (DE-627)SPR056830882 (SPR)s12665-024-11748-2-e DE-627 ger DE-627 rakwb eng 550 VZ 38.95 bkl Singh, Himani verfasserin aut Decomposing impact of climate change and land surface alterations on catchment hydrology in Eastern Himalaya 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Climate change is intensifying water challenges in the Eastern Himalayas. Bridging climate change and water demand is vital, especially in India’s ungauged Himalayan catchments. The proposed novel method aims to differentiate climate change and anthropogenic activity impacts on catchment hydrology. In this study, evaporative demand was assessed by coupling SWAT and Budyko framework at the micro-watershed scale for understanding climate and surface changes in local hydrology. The coupled model considers climate parameters through SWAT to decompose the impacts of climate change and anthropogenic activities on watershed hydrology. The Budyko framework depicted the relationship between precipitation, evapotranspiration (ET), and potential evapotranspiration (PET) resulting in partitioning evaporative demand into green and blue ET. Parameters like d-statistics, responsivity, and elasticity assessed the buffer capacity of catchments against climate change. The study unveiled catchment characteristic (ω) values within the range of 1.70–1.56 from 2005 to 2030, indicative of a discernible shift in hydrological patterns attributed to changes in land use land cover (LULC) and climate variables. The investigation underscored the significant impact of LULC changes, manifesting as a reduction in snow and glacier cover alongside an augmentation in blue ET. The variation in precipitation, LULC, PET, and temperature were identified as primary influencers on hydrological regimes, rendering watersheds increasingly susceptible to climatic variations. Six catchments are unable to cope with or buffer against climate change and have low coping capacity. The study emphasizes the exigency to water resource management in ecologically delicate Eastern Himalayan ecosystem. Climate change (dpeaa)DE-He213 Eastern Himalayas (dpeaa)DE-He213 Ungauged watershed (dpeaa)DE-He213 Evaporative demand (dpeaa)DE-He213 Budyko framework (dpeaa)DE-He213 Sinha, Vinay Shankar Prasad verfasserin (orcid)0000-0001-8387-8625 aut Gaur, Shishir verfasserin aut Khanduja, Ekansha verfasserin aut Mathur, Anandi verfasserin aut Enthalten in Environmental earth sciences Springer Berlin Heidelberg, 2009 83(2024), 16 vom: Aug. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:83 year:2024 number:16 month:08 https://dx.doi.org/10.1007/s12665-024-11748-2 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.95 VZ AR 83 2024 16 08 |
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10.1007/s12665-024-11748-2 doi (DE-627)SPR056830882 (SPR)s12665-024-11748-2-e DE-627 ger DE-627 rakwb eng 550 VZ 38.95 bkl Singh, Himani verfasserin aut Decomposing impact of climate change and land surface alterations on catchment hydrology in Eastern Himalaya 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Climate change is intensifying water challenges in the Eastern Himalayas. Bridging climate change and water demand is vital, especially in India’s ungauged Himalayan catchments. The proposed novel method aims to differentiate climate change and anthropogenic activity impacts on catchment hydrology. In this study, evaporative demand was assessed by coupling SWAT and Budyko framework at the micro-watershed scale for understanding climate and surface changes in local hydrology. The coupled model considers climate parameters through SWAT to decompose the impacts of climate change and anthropogenic activities on watershed hydrology. The Budyko framework depicted the relationship between precipitation, evapotranspiration (ET), and potential evapotranspiration (PET) resulting in partitioning evaporative demand into green and blue ET. Parameters like d-statistics, responsivity, and elasticity assessed the buffer capacity of catchments against climate change. The study unveiled catchment characteristic (ω) values within the range of 1.70–1.56 from 2005 to 2030, indicative of a discernible shift in hydrological patterns attributed to changes in land use land cover (LULC) and climate variables. The investigation underscored the significant impact of LULC changes, manifesting as a reduction in snow and glacier cover alongside an augmentation in blue ET. The variation in precipitation, LULC, PET, and temperature were identified as primary influencers on hydrological regimes, rendering watersheds increasingly susceptible to climatic variations. Six catchments are unable to cope with or buffer against climate change and have low coping capacity. The study emphasizes the exigency to water resource management in ecologically delicate Eastern Himalayan ecosystem. Climate change (dpeaa)DE-He213 Eastern Himalayas (dpeaa)DE-He213 Ungauged watershed (dpeaa)DE-He213 Evaporative demand (dpeaa)DE-He213 Budyko framework (dpeaa)DE-He213 Sinha, Vinay Shankar Prasad verfasserin (orcid)0000-0001-8387-8625 aut Gaur, Shishir verfasserin aut Khanduja, Ekansha verfasserin aut Mathur, Anandi verfasserin aut Enthalten in Environmental earth sciences Springer Berlin Heidelberg, 2009 83(2024), 16 vom: Aug. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:83 year:2024 number:16 month:08 https://dx.doi.org/10.1007/s12665-024-11748-2 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.95 VZ AR 83 2024 16 08 |
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10.1007/s12665-024-11748-2 doi (DE-627)SPR056830882 (SPR)s12665-024-11748-2-e DE-627 ger DE-627 rakwb eng 550 VZ 38.95 bkl Singh, Himani verfasserin aut Decomposing impact of climate change and land surface alterations on catchment hydrology in Eastern Himalaya 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Climate change is intensifying water challenges in the Eastern Himalayas. Bridging climate change and water demand is vital, especially in India’s ungauged Himalayan catchments. The proposed novel method aims to differentiate climate change and anthropogenic activity impacts on catchment hydrology. In this study, evaporative demand was assessed by coupling SWAT and Budyko framework at the micro-watershed scale for understanding climate and surface changes in local hydrology. The coupled model considers climate parameters through SWAT to decompose the impacts of climate change and anthropogenic activities on watershed hydrology. The Budyko framework depicted the relationship between precipitation, evapotranspiration (ET), and potential evapotranspiration (PET) resulting in partitioning evaporative demand into green and blue ET. Parameters like d-statistics, responsivity, and elasticity assessed the buffer capacity of catchments against climate change. The study unveiled catchment characteristic (ω) values within the range of 1.70–1.56 from 2005 to 2030, indicative of a discernible shift in hydrological patterns attributed to changes in land use land cover (LULC) and climate variables. The investigation underscored the significant impact of LULC changes, manifesting as a reduction in snow and glacier cover alongside an augmentation in blue ET. The variation in precipitation, LULC, PET, and temperature were identified as primary influencers on hydrological regimes, rendering watersheds increasingly susceptible to climatic variations. Six catchments are unable to cope with or buffer against climate change and have low coping capacity. The study emphasizes the exigency to water resource management in ecologically delicate Eastern Himalayan ecosystem. Climate change (dpeaa)DE-He213 Eastern Himalayas (dpeaa)DE-He213 Ungauged watershed (dpeaa)DE-He213 Evaporative demand (dpeaa)DE-He213 Budyko framework (dpeaa)DE-He213 Sinha, Vinay Shankar Prasad verfasserin (orcid)0000-0001-8387-8625 aut Gaur, Shishir verfasserin aut Khanduja, Ekansha verfasserin aut Mathur, Anandi verfasserin aut Enthalten in Environmental earth sciences Springer Berlin Heidelberg, 2009 83(2024), 16 vom: Aug. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:83 year:2024 number:16 month:08 https://dx.doi.org/10.1007/s12665-024-11748-2 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.95 VZ AR 83 2024 16 08 |
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10.1007/s12665-024-11748-2 doi (DE-627)SPR056830882 (SPR)s12665-024-11748-2-e DE-627 ger DE-627 rakwb eng 550 VZ 38.95 bkl Singh, Himani verfasserin aut Decomposing impact of climate change and land surface alterations on catchment hydrology in Eastern Himalaya 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Climate change is intensifying water challenges in the Eastern Himalayas. Bridging climate change and water demand is vital, especially in India’s ungauged Himalayan catchments. The proposed novel method aims to differentiate climate change and anthropogenic activity impacts on catchment hydrology. In this study, evaporative demand was assessed by coupling SWAT and Budyko framework at the micro-watershed scale for understanding climate and surface changes in local hydrology. The coupled model considers climate parameters through SWAT to decompose the impacts of climate change and anthropogenic activities on watershed hydrology. The Budyko framework depicted the relationship between precipitation, evapotranspiration (ET), and potential evapotranspiration (PET) resulting in partitioning evaporative demand into green and blue ET. Parameters like d-statistics, responsivity, and elasticity assessed the buffer capacity of catchments against climate change. The study unveiled catchment characteristic (ω) values within the range of 1.70–1.56 from 2005 to 2030, indicative of a discernible shift in hydrological patterns attributed to changes in land use land cover (LULC) and climate variables. The investigation underscored the significant impact of LULC changes, manifesting as a reduction in snow and glacier cover alongside an augmentation in blue ET. The variation in precipitation, LULC, PET, and temperature were identified as primary influencers on hydrological regimes, rendering watersheds increasingly susceptible to climatic variations. Six catchments are unable to cope with or buffer against climate change and have low coping capacity. The study emphasizes the exigency to water resource management in ecologically delicate Eastern Himalayan ecosystem. Climate change (dpeaa)DE-He213 Eastern Himalayas (dpeaa)DE-He213 Ungauged watershed (dpeaa)DE-He213 Evaporative demand (dpeaa)DE-He213 Budyko framework (dpeaa)DE-He213 Sinha, Vinay Shankar Prasad verfasserin (orcid)0000-0001-8387-8625 aut Gaur, Shishir verfasserin aut Khanduja, Ekansha verfasserin aut Mathur, Anandi verfasserin aut Enthalten in Environmental earth sciences Springer Berlin Heidelberg, 2009 83(2024), 16 vom: Aug. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:83 year:2024 number:16 month:08 https://dx.doi.org/10.1007/s12665-024-11748-2 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.95 VZ AR 83 2024 16 08 |
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Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Climate change is intensifying water challenges in the Eastern Himalayas. Bridging climate change and water demand is vital, especially in India’s ungauged Himalayan catchments. The proposed novel method aims to differentiate climate change and anthropogenic activity impacts on catchment hydrology. In this study, evaporative demand was assessed by coupling SWAT and Budyko framework at the micro-watershed scale for understanding climate and surface changes in local hydrology. The coupled model considers climate parameters through SWAT to decompose the impacts of climate change and anthropogenic activities on watershed hydrology. The Budyko framework depicted the relationship between precipitation, evapotranspiration (ET), and potential evapotranspiration (PET) resulting in partitioning evaporative demand into green and blue ET. Parameters like d-statistics, responsivity, and elasticity assessed the buffer capacity of catchments against climate change. The study unveiled catchment characteristic (ω) values within the range of 1.70–1.56 from 2005 to 2030, indicative of a discernible shift in hydrological patterns attributed to changes in land use land cover (LULC) and climate variables. The investigation underscored the significant impact of LULC changes, manifesting as a reduction in snow and glacier cover alongside an augmentation in blue ET. The variation in precipitation, LULC, PET, and temperature were identified as primary influencers on hydrological regimes, rendering watersheds increasingly susceptible to climatic variations. Six catchments are unable to cope with or buffer against climate change and have low coping capacity. 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Singh, Himani |
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550 VZ 38.95 bkl Decomposing impact of climate change and land surface alterations on catchment hydrology in Eastern Himalaya Climate change (dpeaa)DE-He213 Eastern Himalayas (dpeaa)DE-He213 Ungauged watershed (dpeaa)DE-He213 Evaporative demand (dpeaa)DE-He213 Budyko framework (dpeaa)DE-He213 |
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decomposing impact of climate change and land surface alterations on catchment hydrology in eastern himalaya |
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Decomposing impact of climate change and land surface alterations on catchment hydrology in Eastern Himalaya |
| abstract |
Abstract Climate change is intensifying water challenges in the Eastern Himalayas. Bridging climate change and water demand is vital, especially in India’s ungauged Himalayan catchments. The proposed novel method aims to differentiate climate change and anthropogenic activity impacts on catchment hydrology. In this study, evaporative demand was assessed by coupling SWAT and Budyko framework at the micro-watershed scale for understanding climate and surface changes in local hydrology. The coupled model considers climate parameters through SWAT to decompose the impacts of climate change and anthropogenic activities on watershed hydrology. The Budyko framework depicted the relationship between precipitation, evapotranspiration (ET), and potential evapotranspiration (PET) resulting in partitioning evaporative demand into green and blue ET. Parameters like d-statistics, responsivity, and elasticity assessed the buffer capacity of catchments against climate change. The study unveiled catchment characteristic (ω) values within the range of 1.70–1.56 from 2005 to 2030, indicative of a discernible shift in hydrological patterns attributed to changes in land use land cover (LULC) and climate variables. The investigation underscored the significant impact of LULC changes, manifesting as a reduction in snow and glacier cover alongside an augmentation in blue ET. The variation in precipitation, LULC, PET, and temperature were identified as primary influencers on hydrological regimes, rendering watersheds increasingly susceptible to climatic variations. Six catchments are unable to cope with or buffer against climate change and have low coping capacity. The study emphasizes the exigency to water resource management in ecologically delicate Eastern Himalayan ecosystem. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
| abstractGer |
Abstract Climate change is intensifying water challenges in the Eastern Himalayas. Bridging climate change and water demand is vital, especially in India’s ungauged Himalayan catchments. The proposed novel method aims to differentiate climate change and anthropogenic activity impacts on catchment hydrology. In this study, evaporative demand was assessed by coupling SWAT and Budyko framework at the micro-watershed scale for understanding climate and surface changes in local hydrology. The coupled model considers climate parameters through SWAT to decompose the impacts of climate change and anthropogenic activities on watershed hydrology. The Budyko framework depicted the relationship between precipitation, evapotranspiration (ET), and potential evapotranspiration (PET) resulting in partitioning evaporative demand into green and blue ET. Parameters like d-statistics, responsivity, and elasticity assessed the buffer capacity of catchments against climate change. The study unveiled catchment characteristic (ω) values within the range of 1.70–1.56 from 2005 to 2030, indicative of a discernible shift in hydrological patterns attributed to changes in land use land cover (LULC) and climate variables. The investigation underscored the significant impact of LULC changes, manifesting as a reduction in snow and glacier cover alongside an augmentation in blue ET. The variation in precipitation, LULC, PET, and temperature were identified as primary influencers on hydrological regimes, rendering watersheds increasingly susceptible to climatic variations. Six catchments are unable to cope with or buffer against climate change and have low coping capacity. The study emphasizes the exigency to water resource management in ecologically delicate Eastern Himalayan ecosystem. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
| abstract_unstemmed |
Abstract Climate change is intensifying water challenges in the Eastern Himalayas. Bridging climate change and water demand is vital, especially in India’s ungauged Himalayan catchments. The proposed novel method aims to differentiate climate change and anthropogenic activity impacts on catchment hydrology. In this study, evaporative demand was assessed by coupling SWAT and Budyko framework at the micro-watershed scale for understanding climate and surface changes in local hydrology. The coupled model considers climate parameters through SWAT to decompose the impacts of climate change and anthropogenic activities on watershed hydrology. The Budyko framework depicted the relationship between precipitation, evapotranspiration (ET), and potential evapotranspiration (PET) resulting in partitioning evaporative demand into green and blue ET. Parameters like d-statistics, responsivity, and elasticity assessed the buffer capacity of catchments against climate change. The study unveiled catchment characteristic (ω) values within the range of 1.70–1.56 from 2005 to 2030, indicative of a discernible shift in hydrological patterns attributed to changes in land use land cover (LULC) and climate variables. The investigation underscored the significant impact of LULC changes, manifesting as a reduction in snow and glacier cover alongside an augmentation in blue ET. The variation in precipitation, LULC, PET, and temperature were identified as primary influencers on hydrological regimes, rendering watersheds increasingly susceptible to climatic variations. Six catchments are unable to cope with or buffer against climate change and have low coping capacity. The study emphasizes the exigency to water resource management in ecologically delicate Eastern Himalayan ecosystem. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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| title_short |
Decomposing impact of climate change and land surface alterations on catchment hydrology in Eastern Himalaya |
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https://dx.doi.org/10.1007/s12665-024-11748-2 |
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Sinha, Vinay Shankar Prasad Gaur, Shishir Khanduja, Ekansha Mathur, Anandi |
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| score |
7.401412 |