Contrasting changes of snowfall in response to temperature and rainfall over two distinct geographic ranges of the Himalayas: A study using the High Asia Refined analysis data
Snow is a major source of water and its monitoring is important for hydrological applications. It provides meltwater to various rivers such as the Indus, Ganges, and Brahmaputra in the Himalayan region. Significant changes in snowfall variability play a pivotal role in climate. The present study inv...
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description | Snow is a major source of water and its monitoring is important for hydrological applications. It provides meltwater to various rivers such as the Indus, Ganges, and Brahmaputra in the Himalayan region. Significant changes in snowfall variability play a pivotal role in climate. The present study investigates the temporal variability of snowfall, temperature, and rainfall over Nubra (latitude: 34.53°–35.67°N; longitude: 76.75°–77.81°E) and Bhagirathi (latitude: 30.33°–31.45°N; longitude: 78.15°–79.47°E) basins in the Himalayan region using 30 yrs of reanalysis data (1991–2020). The High Asia Refined analysis (HAR) and Climatic Research Unit (CRU) data were used to study the snowfall and maximum air temperature variabilities, respectively, over the study basins. For rainfall, high-resolution (0.25° × 0.25°) gridded rainfall data from the India Meteorological Department is used. We have studied the annual and monthly variability of daily snowfall, temperature and rainfall over the two basins. Our analysis shows the declining trend (–2 mm/decade) of snowfall over the Nubra basin and a slightly increasing trend (0.12 mm/decade) in the Bhagirathi basin from 2004. The monthly time series in maximum temperature anomaly shows a positive trend with a maximum anomaly found to be around 2 K during the winter period. From the rainfall analysis, an increasing trend in annual rainfall is observed, especially Nubra basin showing a notable increase. Further, warming of the troposphere is found to be ~2–3 K, which is another important factor for the reduction in snowfall. Thus, positive trends in maximum temperature, rainfall and warming troposphere are the controlling factors for the declining (increasing) trend in snowfall over the Nubra (Bhagirathi) basins. Thus, the present study shows simultaneous changes in snowfall, temperature and rainfall over the Himalayan region and assumes importance in climatic applications. |
doi_str_mv | 10.1007/s12040-023-02090-5 |
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It provides meltwater to various rivers such as the Indus, Ganges, and Brahmaputra in the Himalayan region. Significant changes in snowfall variability play a pivotal role in climate. The present study investigates the temporal variability of snowfall, temperature, and rainfall over Nubra (latitude: 34.53°–35.67°N; longitude: 76.75°–77.81°E) and Bhagirathi (latitude: 30.33°–31.45°N; longitude: 78.15°–79.47°E) basins in the Himalayan region using 30 yrs of reanalysis data (1991–2020). The High Asia Refined analysis (HAR) and Climatic Research Unit (CRU) data were used to study the snowfall and maximum air temperature variabilities, respectively, over the study basins. For rainfall, high-resolution (0.25° × 0.25°) gridded rainfall data from the India Meteorological Department is used. We have studied the annual and monthly variability of daily snowfall, temperature and rainfall over the two basins. Our analysis shows the declining trend (–2 mm/decade) of snowfall over the Nubra basin and a slightly increasing trend (0.12 mm/decade) in the Bhagirathi basin from 2004. The monthly time series in maximum temperature anomaly shows a positive trend with a maximum anomaly found to be around 2 K during the winter period. From the rainfall analysis, an increasing trend in annual rainfall is observed, especially Nubra basin showing a notable increase. Further, warming of the troposphere is found to be ~2–3 K, which is another important factor for the reduction in snowfall. Thus, positive trends in maximum temperature, rainfall and warming troposphere are the controlling factors for the declining (increasing) trend in snowfall over the Nubra (Bhagirathi) basins. Thus, the present study shows simultaneous changes in snowfall, temperature and rainfall over the Himalayan region and assumes importance in climatic applications.</description><identifier>ISSN: 0973-774X</identifier><identifier>ISSN: 0253-4126</identifier><identifier>EISSN: 0973-774X</identifier><identifier>DOI: 10.1007/s12040-023-02090-5</identifier><language>eng</language><publisher>New Delhi: Springer India</publisher><subject>Air temperature ; Analysis ; Annual rainfall ; Annual variations ; Basins ; Climatic analysis ; Daily precipitation ; Datasets ; Earth and Environmental Science ; Earth Sciences ; Glaciers ; Hydrologic data ; Hydrology ; Latitude ; Longitude ; Maximum temperatures ; Meltwater ; Precipitation ; Rainfall ; Rainfall data ; Regions ; Rivers ; Sea level ; Snow ; Snowfall ; Space Exploration and Astronautics ; Space Sciences (including Extraterrestrial Physics ; Temperature anomalies ; Temporal variability ; Temporal variations ; Trends ; Troposphere ; Variability</subject><ispartof>Journal of Earth System Science, 2023-05, Vol.132 (2), p.79, Article 79</ispartof><rights>Indian Academy of Sciences 2023</rights><rights>Indian Academy of Sciences 2023.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c270t-325aaa4d248221e7352ee1b58ad93a6e4eb12ecfb3600ec1d844dfad92bb50223</cites><orcidid>0000-0003-2987-1232</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12040-023-02090-5$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12040-023-02090-5$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Subrahmanyam, Kandula V</creatorcontrib><creatorcontrib>Srinivasulu, J</creatorcontrib><creatorcontrib>Kumar, Prashant</creatorcontrib><creatorcontrib>Bothale, Rajashree V</creatorcontrib><creatorcontrib>Sai, M V R Sesha</creatorcontrib><title>Contrasting changes of snowfall in response to temperature and rainfall over two distinct geographic ranges of the Himalayas: A study using the High Asia Refined analysis data</title><title>Journal of Earth System Science</title><addtitle>J Earth Syst Sci</addtitle><description>Snow is a major source of water and its monitoring is important for hydrological applications. It provides meltwater to various rivers such as the Indus, Ganges, and Brahmaputra in the Himalayan region. Significant changes in snowfall variability play a pivotal role in climate. The present study investigates the temporal variability of snowfall, temperature, and rainfall over Nubra (latitude: 34.53°–35.67°N; longitude: 76.75°–77.81°E) and Bhagirathi (latitude: 30.33°–31.45°N; longitude: 78.15°–79.47°E) basins in the Himalayan region using 30 yrs of reanalysis data (1991–2020). The High Asia Refined analysis (HAR) and Climatic Research Unit (CRU) data were used to study the snowfall and maximum air temperature variabilities, respectively, over the study basins. For rainfall, high-resolution (0.25° × 0.25°) gridded rainfall data from the India Meteorological Department is used. We have studied the annual and monthly variability of daily snowfall, temperature and rainfall over the two basins. Our analysis shows the declining trend (–2 mm/decade) of snowfall over the Nubra basin and a slightly increasing trend (0.12 mm/decade) in the Bhagirathi basin from 2004. The monthly time series in maximum temperature anomaly shows a positive trend with a maximum anomaly found to be around 2 K during the winter period. From the rainfall analysis, an increasing trend in annual rainfall is observed, especially Nubra basin showing a notable increase. Further, warming of the troposphere is found to be ~2–3 K, which is another important factor for the reduction in snowfall. Thus, positive trends in maximum temperature, rainfall and warming troposphere are the controlling factors for the declining (increasing) trend in snowfall over the Nubra (Bhagirathi) basins. Thus, the present study shows simultaneous changes in snowfall, temperature and rainfall over the Himalayan region and assumes importance in climatic applications.</description><subject>Air temperature</subject><subject>Analysis</subject><subject>Annual rainfall</subject><subject>Annual variations</subject><subject>Basins</subject><subject>Climatic analysis</subject><subject>Daily precipitation</subject><subject>Datasets</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Glaciers</subject><subject>Hydrologic data</subject><subject>Hydrology</subject><subject>Latitude</subject><subject>Longitude</subject><subject>Maximum temperatures</subject><subject>Meltwater</subject><subject>Precipitation</subject><subject>Rainfall</subject><subject>Rainfall data</subject><subject>Regions</subject><subject>Rivers</subject><subject>Sea level</subject><subject>Snow</subject><subject>Snowfall</subject><subject>Space Exploration and Astronautics</subject><subject>Space Sciences (including Extraterrestrial Physics</subject><subject>Temperature anomalies</subject><subject>Temporal variability</subject><subject>Temporal variations</subject><subject>Trends</subject><subject>Troposphere</subject><subject>Variability</subject><issn>0973-774X</issn><issn>0253-4126</issn><issn>0973-774X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kc1u1DAUhSNEJUrhBVhdiXXAP8k4YTcaAUWqhFQVqTvrJrnJuJrawdehmqfqK-JpQLDqwrKl-51zbJ-ieCfFBymE-chSiUqUQum8RCvK-kVxLlqjS2Oq25f_nV8Vr5nvhNCbxrTnxeMu-BSRk_MT9Hv0EzGEEdiHhxEPB3AeIvEcPBOkAInuZ4qYlkiAfoCIzj9x4RdFSA8BBncy6xNMFKaI8971mfrrm_YEl-4eD3hE_gRb4LQMR1j4lL8Opz1s2SFc0-g8DTkGD0d2DAMmfFOc5Timt3_2i-LHl883u8vy6vvXb7vtVdkrI1KpVY2I1aCqRilJRteKSHZ1g0OrcUMVdVJRP3Z6IwT1cmiqahjzUHVdLZTSF8X71XeO4edCnOxdWGK-CVvVynYjpTFNptRK9TEwRxrtHPPj4tFKYU_F2LUYm4uxT8XYOov0KuIM53-J_6yfUf0GvNSUuw</recordid><startdate>20230505</startdate><enddate>20230505</enddate><creator>Subrahmanyam, Kandula V</creator><creator>Srinivasulu, J</creator><creator>Kumar, Prashant</creator><creator>Bothale, Rajashree V</creator><creator>Sai, M V R Sesha</creator><general>Springer India</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><orcidid>https://orcid.org/0000-0003-2987-1232</orcidid></search><sort><creationdate>20230505</creationdate><title>Contrasting changes of snowfall in response to temperature and rainfall over two distinct geographic ranges of the Himalayas: A study using the High Asia Refined analysis data</title><author>Subrahmanyam, Kandula V ; 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It provides meltwater to various rivers such as the Indus, Ganges, and Brahmaputra in the Himalayan region. Significant changes in snowfall variability play a pivotal role in climate. The present study investigates the temporal variability of snowfall, temperature, and rainfall over Nubra (latitude: 34.53°–35.67°N; longitude: 76.75°–77.81°E) and Bhagirathi (latitude: 30.33°–31.45°N; longitude: 78.15°–79.47°E) basins in the Himalayan region using 30 yrs of reanalysis data (1991–2020). The High Asia Refined analysis (HAR) and Climatic Research Unit (CRU) data were used to study the snowfall and maximum air temperature variabilities, respectively, over the study basins. For rainfall, high-resolution (0.25° × 0.25°) gridded rainfall data from the India Meteorological Department is used. We have studied the annual and monthly variability of daily snowfall, temperature and rainfall over the two basins. Our analysis shows the declining trend (–2 mm/decade) of snowfall over the Nubra basin and a slightly increasing trend (0.12 mm/decade) in the Bhagirathi basin from 2004. The monthly time series in maximum temperature anomaly shows a positive trend with a maximum anomaly found to be around 2 K during the winter period. From the rainfall analysis, an increasing trend in annual rainfall is observed, especially Nubra basin showing a notable increase. Further, warming of the troposphere is found to be ~2–3 K, which is another important factor for the reduction in snowfall. Thus, positive trends in maximum temperature, rainfall and warming troposphere are the controlling factors for the declining (increasing) trend in snowfall over the Nubra (Bhagirathi) basins. Thus, the present study shows simultaneous changes in snowfall, temperature and rainfall over the Himalayan region and assumes importance in climatic applications.</abstract><cop>New Delhi</cop><pub>Springer India</pub><doi>10.1007/s12040-023-02090-5</doi><orcidid>https://orcid.org/0000-0003-2987-1232</orcidid></addata></record> |
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subjects | Air temperature Analysis Annual rainfall Annual variations Basins Climatic analysis Daily precipitation Datasets Earth and Environmental Science Earth Sciences Glaciers Hydrologic data Hydrology Latitude Longitude Maximum temperatures Meltwater Precipitation Rainfall Rainfall data Regions Rivers Sea level Snow Snowfall Space Exploration and Astronautics Space Sciences (including Extraterrestrial Physics Temperature anomalies Temporal variability Temporal variations Trends Troposphere Variability |
title | Contrasting changes of snowfall in response to temperature and rainfall over two distinct geographic ranges of the Himalayas: A study using the High Asia Refined analysis data |
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