Stable isotope evidence of dual (Arabian Sea and Bay of Bengal) vapour sources in monsoonal precipitation over north India

High resolution time series data of hydrogen ( δD) and oxygen ( δ 18O) isotope values of precipitation have been generated for the first time at Kolkata, eastern India where the summer monsoon clouds from Bay of Bengal (BOB) commence their journey over India. Use of a Rayleigh cum two component mixi...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Earth and planetary science letters 2006-10, Vol.250 (3), p.511-521
Hauptverfasser: Sengupta, Saikat, Sarkar, A.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 521
container_issue 3
container_start_page 511
container_title Earth and planetary science letters
container_volume 250
creator Sengupta, Saikat
Sarkar, A.
description High resolution time series data of hydrogen ( δD) and oxygen ( δ 18O) isotope values of precipitation have been generated for the first time at Kolkata, eastern India where the summer monsoon clouds from Bay of Bengal (BOB) commence their journey over India. Use of a Rayleigh cum two component mixing model and comparison of Kolkata data with the International Atomic Energy Agency (IAEA)–Global Network of Isotopes in Precipitation (GNIP) data base of New Delhi suggest that the precipitation at New Delhi cannot be explained by simple continental effect of a BOB vapour source alone, traveling and raining successively along Kolkata–New Delhi route. It is necessary to invoke an admixture of ∼ 20% vapour originating from the Arabian sea with the vapour coming from BOB and finally causing summer monsoon rains at New Delhi. The findings have major implications to the regional water vapour budget over India.
doi_str_mv 10.1016/j.epsl.2006.08.011
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_20405925</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0012821X06006029</els_id><sourcerecordid>20405925</sourcerecordid><originalsourceid>FETCH-LOGICAL-a354t-d8a0bdbd1af0f2c75b7aadb6499c85bf25e9451c33742eb67af690eab8368d063</originalsourceid><addsrcrecordid>eNp9kMFO3DAQhi1EJba0L8DJJ0QPCWMnziYSF0C0ICH1QCtxs8b2BLzK2qmdXQmenkTbM5eZw_zfSP_H2JmAUoBoLjcljXkoJUBTQluCEEdsJapWFSCq52O2AhCyaKV4PmFfc97AHFRNt2LvTxOagbjPcYojcdp7R8ESjz13Oxz4xXVC4zHwJ0KOwfEbfFuONxRecPjB9zjGXeJ5HpYy94FvY8gxhpkdE1k_-gknHwOPe0o8xDS98ofgPH5jX3ocMn3_v0_Z3593f27vi8ffvx5urx8LrFQ9Fa5FMM44gT300q6VWSM609RdZ1tleqmoq5WwVbWuJZlmjX3TAaFpq6Z10FSn7Pzwd0zx347ypLc-WxoGDBR3WUuoQXVSzUF5CNoUc07U6zH5LaY3LUAvmvVGL5r1ollDq2fNM3R1gGiusPeUdLZ-Mej83H7SLvrP8A-MPohy</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>20405925</pqid></control><display><type>article</type><title>Stable isotope evidence of dual (Arabian Sea and Bay of Bengal) vapour sources in monsoonal precipitation over north India</title><source>Access via ScienceDirect (Elsevier)</source><creator>Sengupta, Saikat ; Sarkar, A.</creator><creatorcontrib>Sengupta, Saikat ; Sarkar, A.</creatorcontrib><description>High resolution time series data of hydrogen ( δD) and oxygen ( δ 18O) isotope values of precipitation have been generated for the first time at Kolkata, eastern India where the summer monsoon clouds from Bay of Bengal (BOB) commence their journey over India. Use of a Rayleigh cum two component mixing model and comparison of Kolkata data with the International Atomic Energy Agency (IAEA)–Global Network of Isotopes in Precipitation (GNIP) data base of New Delhi suggest that the precipitation at New Delhi cannot be explained by simple continental effect of a BOB vapour source alone, traveling and raining successively along Kolkata–New Delhi route. It is necessary to invoke an admixture of ∼ 20% vapour originating from the Arabian sea with the vapour coming from BOB and finally causing summer monsoon rains at New Delhi. The findings have major implications to the regional water vapour budget over India.</description><identifier>ISSN: 0012-821X</identifier><identifier>EISSN: 1385-013X</identifier><identifier>DOI: 10.1016/j.epsl.2006.08.011</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>India ; Marine ; Monsoon ; Stable isotope ; Vapour mixing</subject><ispartof>Earth and planetary science letters, 2006-10, Vol.250 (3), p.511-521</ispartof><rights>2006 Elsevier B.V.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a354t-d8a0bdbd1af0f2c75b7aadb6499c85bf25e9451c33742eb67af690eab8368d063</citedby><cites>FETCH-LOGICAL-a354t-d8a0bdbd1af0f2c75b7aadb6499c85bf25e9451c33742eb67af690eab8368d063</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.epsl.2006.08.011$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>315,781,785,3551,27928,27929,45999</link.rule.ids></links><search><creatorcontrib>Sengupta, Saikat</creatorcontrib><creatorcontrib>Sarkar, A.</creatorcontrib><title>Stable isotope evidence of dual (Arabian Sea and Bay of Bengal) vapour sources in monsoonal precipitation over north India</title><title>Earth and planetary science letters</title><description>High resolution time series data of hydrogen ( δD) and oxygen ( δ 18O) isotope values of precipitation have been generated for the first time at Kolkata, eastern India where the summer monsoon clouds from Bay of Bengal (BOB) commence their journey over India. Use of a Rayleigh cum two component mixing model and comparison of Kolkata data with the International Atomic Energy Agency (IAEA)–Global Network of Isotopes in Precipitation (GNIP) data base of New Delhi suggest that the precipitation at New Delhi cannot be explained by simple continental effect of a BOB vapour source alone, traveling and raining successively along Kolkata–New Delhi route. It is necessary to invoke an admixture of ∼ 20% vapour originating from the Arabian sea with the vapour coming from BOB and finally causing summer monsoon rains at New Delhi. The findings have major implications to the regional water vapour budget over India.</description><subject>India</subject><subject>Marine</subject><subject>Monsoon</subject><subject>Stable isotope</subject><subject>Vapour mixing</subject><issn>0012-821X</issn><issn>1385-013X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNp9kMFO3DAQhi1EJba0L8DJJ0QPCWMnziYSF0C0ICH1QCtxs8b2BLzK2qmdXQmenkTbM5eZw_zfSP_H2JmAUoBoLjcljXkoJUBTQluCEEdsJapWFSCq52O2AhCyaKV4PmFfc97AHFRNt2LvTxOagbjPcYojcdp7R8ESjz13Oxz4xXVC4zHwJ0KOwfEbfFuONxRecPjB9zjGXeJ5HpYy94FvY8gxhpkdE1k_-gknHwOPe0o8xDS98ofgPH5jX3ocMn3_v0_Z3593f27vi8ffvx5urx8LrFQ9Fa5FMM44gT300q6VWSM609RdZ1tleqmoq5WwVbWuJZlmjX3TAaFpq6Z10FSn7Pzwd0zx347ypLc-WxoGDBR3WUuoQXVSzUF5CNoUc07U6zH5LaY3LUAvmvVGL5r1ollDq2fNM3R1gGiusPeUdLZ-Mej83H7SLvrP8A-MPohy</recordid><startdate>20061030</startdate><enddate>20061030</enddate><creator>Sengupta, Saikat</creator><creator>Sarkar, A.</creator><general>Elsevier B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20061030</creationdate><title>Stable isotope evidence of dual (Arabian Sea and Bay of Bengal) vapour sources in monsoonal precipitation over north India</title><author>Sengupta, Saikat ; Sarkar, A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a354t-d8a0bdbd1af0f2c75b7aadb6499c85bf25e9451c33742eb67af690eab8368d063</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>India</topic><topic>Marine</topic><topic>Monsoon</topic><topic>Stable isotope</topic><topic>Vapour mixing</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sengupta, Saikat</creatorcontrib><creatorcontrib>Sarkar, A.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><jtitle>Earth and planetary science letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sengupta, Saikat</au><au>Sarkar, A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Stable isotope evidence of dual (Arabian Sea and Bay of Bengal) vapour sources in monsoonal precipitation over north India</atitle><jtitle>Earth and planetary science letters</jtitle><date>2006-10-30</date><risdate>2006</risdate><volume>250</volume><issue>3</issue><spage>511</spage><epage>521</epage><pages>511-521</pages><issn>0012-821X</issn><eissn>1385-013X</eissn><abstract>High resolution time series data of hydrogen ( δD) and oxygen ( δ 18O) isotope values of precipitation have been generated for the first time at Kolkata, eastern India where the summer monsoon clouds from Bay of Bengal (BOB) commence their journey over India. Use of a Rayleigh cum two component mixing model and comparison of Kolkata data with the International Atomic Energy Agency (IAEA)–Global Network of Isotopes in Precipitation (GNIP) data base of New Delhi suggest that the precipitation at New Delhi cannot be explained by simple continental effect of a BOB vapour source alone, traveling and raining successively along Kolkata–New Delhi route. It is necessary to invoke an admixture of ∼ 20% vapour originating from the Arabian sea with the vapour coming from BOB and finally causing summer monsoon rains at New Delhi. The findings have major implications to the regional water vapour budget over India.</abstract><pub>Elsevier B.V</pub><doi>10.1016/j.epsl.2006.08.011</doi><tpages>11</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0012-821X
ispartof Earth and planetary science letters, 2006-10, Vol.250 (3), p.511-521
issn 0012-821X
1385-013X
language eng
recordid cdi_proquest_miscellaneous_20405925
source Access via ScienceDirect (Elsevier)
subjects India
Marine
Monsoon
Stable isotope
Vapour mixing
title Stable isotope evidence of dual (Arabian Sea and Bay of Bengal) vapour sources in monsoonal precipitation over north India
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-17T01%3A27%3A36IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Stable%20isotope%20evidence%20of%20dual%20(Arabian%20Sea%20and%20Bay%20of%20Bengal)%20vapour%20sources%20in%20monsoonal%20precipitation%20over%20north%20India&rft.jtitle=Earth%20and%20planetary%20science%20letters&rft.au=Sengupta,%20Saikat&rft.date=2006-10-30&rft.volume=250&rft.issue=3&rft.spage=511&rft.epage=521&rft.pages=511-521&rft.issn=0012-821X&rft.eissn=1385-013X&rft_id=info:doi/10.1016/j.epsl.2006.08.011&rft_dat=%3Cproquest_cross%3E20405925%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=20405925&rft_id=info:pmid/&rft_els_id=S0012821X06006029&rfr_iscdi=true