Acceleration of Climate Change in the Upper Layer of the Black Sea
The thermohaline regime trends of the Black Sea basin in the period 2000–2021 were studied based on the data from three retrospective analyses (reanalyses) of the hydrophysical fields of the Black Sea. It is shown that the cumulative effect of an increase in the average sea surface temperature (SST)...
Gespeichert in:
| Veröffentlicht in: | Doklady earth sciences 2024-09, Vol.518 (1), p.1550-1555 |
|---|---|
| Hauptverfasser: | , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 1555 |
|---|---|
| container_issue | 1 |
| container_start_page | 1550 |
| container_title | Doklady earth sciences |
| container_volume | 518 |
| creator | Korotaev, G. K. Belokopytov, V. N. Dorofeev, V. L. Mizyuk, A. I. Kholod, A. L. |
| description | The thermohaline regime trends of the Black Sea basin in the period 2000–2021 were studied based on the data from three retrospective analyses (reanalyses) of the hydrophysical fields of the Black Sea. It is shown that the cumulative effect of an increase in the average sea surface temperature (SST) and increasingly milder winter conditions in the Black Sea over the last seven to eight years led to a record-breaking warming and then to the disappearance of the ventilated cold intermediate layer (CIL) of the Black Sea in its traditional meaning by 2020. In addition, in the past seven to eight years, accelerated warming of seawaters has been observed within the permanent (main) pycnocline. Changes in the thermal regime of the upper layer of the sea are accompanied by a continuing increase in salinity in the main pycnocline. |
| doi_str_mv | 10.1134/S1028334X24602797 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_3085226046</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>3085226046</sourcerecordid><originalsourceid>FETCH-LOGICAL-a221t-20906b2202e51102feda560b38fad45d717b562512d9e0ca082f64d6f3cb6ba93</originalsourceid><addsrcrecordid>eNp1UE1PwzAMjRBIjMEP4BaJc8FxPtoet4ovaRKHMYlblbYO2yhtSbrD_j2ZhsQBcbEt-71nPzN2LeBWCKnulgIwk1K9oTKAaZ6esInQUiSZ1Oo01nGcHObn7CKELYBSSucTNp_VNbXk7bjpO947XrSbTzsSL9a2eye-6fi4Jr4aBvJ8YfcxRtChNW9t_cGXZC_ZmbNtoKufPGWrh_vX4ilZvDw-F7NFYhHFmCDkYCpEQNIinuOosdpAJTNnG6WbVKSVNqgFNjlBbSFDZ1RjnKwrU9lcTtnNUXfw_deOwlhu-53v4spSQqYRDSgTUeKIqn0fgidXDj468vtSQHl4VfnnVZGDR06I2Oja_yr_T_oG2PRodQ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>3085226046</pqid></control><display><type>article</type><title>Acceleration of Climate Change in the Upper Layer of the Black Sea</title><source>SpringerLink Journals - AutoHoldings</source><creator>Korotaev, G. K. ; Belokopytov, V. N. ; Dorofeev, V. L. ; Mizyuk, A. I. ; Kholod, A. L.</creator><creatorcontrib>Korotaev, G. K. ; Belokopytov, V. N. ; Dorofeev, V. L. ; Mizyuk, A. I. ; Kholod, A. L.</creatorcontrib><description>The thermohaline regime trends of the Black Sea basin in the period 2000–2021 were studied based on the data from three retrospective analyses (reanalyses) of the hydrophysical fields of the Black Sea. It is shown that the cumulative effect of an increase in the average sea surface temperature (SST) and increasingly milder winter conditions in the Black Sea over the last seven to eight years led to a record-breaking warming and then to the disappearance of the ventilated cold intermediate layer (CIL) of the Black Sea in its traditional meaning by 2020. In addition, in the past seven to eight years, accelerated warming of seawaters has been observed within the permanent (main) pycnocline. Changes in the thermal regime of the upper layer of the sea are accompanied by a continuing increase in salinity in the main pycnocline.</description><identifier>ISSN: 1028-334X</identifier><identifier>EISSN: 1531-8354</identifier><identifier>DOI: 10.1134/S1028334X24602797</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Climate change ; Earth and Environmental Science ; Earth Sciences ; Oceanology ; Pycnocline ; Pycnoclines ; Salinity ; Sea surface temperature ; Surface temperature</subject><ispartof>Doklady earth sciences, 2024-09, Vol.518 (1), p.1550-1555</ispartof><rights>Pleiades Publishing, Ltd. 2024. ISSN 1028-334X, Doklady Earth Sciences, 2024, Vol. 518, Part 1, pp. 1550–1555. © Pleiades Publishing, Ltd., 2024. ISSN 1028-334X, Doklady Earth Sciences, 2024. © Pleiades Publishing, Ltd., 2024.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a221t-20906b2202e51102feda560b38fad45d717b562512d9e0ca082f64d6f3cb6ba93</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1028334X24602797$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1028334X24602797$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27922,27923,41486,42555,51317</link.rule.ids></links><search><creatorcontrib>Korotaev, G. K.</creatorcontrib><creatorcontrib>Belokopytov, V. N.</creatorcontrib><creatorcontrib>Dorofeev, V. L.</creatorcontrib><creatorcontrib>Mizyuk, A. I.</creatorcontrib><creatorcontrib>Kholod, A. L.</creatorcontrib><title>Acceleration of Climate Change in the Upper Layer of the Black Sea</title><title>Doklady earth sciences</title><addtitle>Dokl. Earth Sc</addtitle><description>The thermohaline regime trends of the Black Sea basin in the period 2000–2021 were studied based on the data from three retrospective analyses (reanalyses) of the hydrophysical fields of the Black Sea. It is shown that the cumulative effect of an increase in the average sea surface temperature (SST) and increasingly milder winter conditions in the Black Sea over the last seven to eight years led to a record-breaking warming and then to the disappearance of the ventilated cold intermediate layer (CIL) of the Black Sea in its traditional meaning by 2020. In addition, in the past seven to eight years, accelerated warming of seawaters has been observed within the permanent (main) pycnocline. Changes in the thermal regime of the upper layer of the sea are accompanied by a continuing increase in salinity in the main pycnocline.</description><subject>Climate change</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Oceanology</subject><subject>Pycnocline</subject><subject>Pycnoclines</subject><subject>Salinity</subject><subject>Sea surface temperature</subject><subject>Surface temperature</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp1UE1PwzAMjRBIjMEP4BaJc8FxPtoet4ovaRKHMYlblbYO2yhtSbrD_j2ZhsQBcbEt-71nPzN2LeBWCKnulgIwk1K9oTKAaZ6esInQUiSZ1Oo01nGcHObn7CKELYBSSucTNp_VNbXk7bjpO947XrSbTzsSL9a2eye-6fi4Jr4aBvJ8YfcxRtChNW9t_cGXZC_ZmbNtoKufPGWrh_vX4ilZvDw-F7NFYhHFmCDkYCpEQNIinuOosdpAJTNnG6WbVKSVNqgFNjlBbSFDZ1RjnKwrU9lcTtnNUXfw_deOwlhu-53v4spSQqYRDSgTUeKIqn0fgidXDj468vtSQHl4VfnnVZGDR06I2Oja_yr_T_oG2PRodQ</recordid><startdate>20240901</startdate><enddate>20240901</enddate><creator>Korotaev, G. K.</creator><creator>Belokopytov, V. N.</creator><creator>Dorofeev, V. L.</creator><creator>Mizyuk, A. I.</creator><creator>Kholod, A. L.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20240901</creationdate><title>Acceleration of Climate Change in the Upper Layer of the Black Sea</title><author>Korotaev, G. K. ; Belokopytov, V. N. ; Dorofeev, V. L. ; Mizyuk, A. I. ; Kholod, A. L.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a221t-20906b2202e51102feda560b38fad45d717b562512d9e0ca082f64d6f3cb6ba93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Climate change</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Oceanology</topic><topic>Pycnocline</topic><topic>Pycnoclines</topic><topic>Salinity</topic><topic>Sea surface temperature</topic><topic>Surface temperature</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Korotaev, G. K.</creatorcontrib><creatorcontrib>Belokopytov, V. N.</creatorcontrib><creatorcontrib>Dorofeev, V. L.</creatorcontrib><creatorcontrib>Mizyuk, A. I.</creatorcontrib><creatorcontrib>Kholod, A. L.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical 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 & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Doklady earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Korotaev, G. K.</au><au>Belokopytov, V. N.</au><au>Dorofeev, V. L.</au><au>Mizyuk, A. I.</au><au>Kholod, A. L.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Acceleration of Climate Change in the Upper Layer of the Black Sea</atitle><jtitle>Doklady earth sciences</jtitle><stitle>Dokl. Earth Sc</stitle><date>2024-09-01</date><risdate>2024</risdate><volume>518</volume><issue>1</issue><spage>1550</spage><epage>1555</epage><pages>1550-1555</pages><issn>1028-334X</issn><eissn>1531-8354</eissn><abstract>The thermohaline regime trends of the Black Sea basin in the period 2000–2021 were studied based on the data from three retrospective analyses (reanalyses) of the hydrophysical fields of the Black Sea. It is shown that the cumulative effect of an increase in the average sea surface temperature (SST) and increasingly milder winter conditions in the Black Sea over the last seven to eight years led to a record-breaking warming and then to the disappearance of the ventilated cold intermediate layer (CIL) of the Black Sea in its traditional meaning by 2020. In addition, in the past seven to eight years, accelerated warming of seawaters has been observed within the permanent (main) pycnocline. Changes in the thermal regime of the upper layer of the sea are accompanied by a continuing increase in salinity in the main pycnocline.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1028334X24602797</doi><tpages>6</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1028-334X |
| ispartof | Doklady earth sciences, 2024-09, Vol.518 (1), p.1550-1555 |
| issn | 1028-334X 1531-8354 |
| language | eng |
| recordid | cdi_proquest_journals_3085226046 |
| source | SpringerLink Journals - AutoHoldings |
| subjects | Climate change Earth and Environmental Science Earth Sciences Oceanology Pycnocline Pycnoclines Salinity Sea surface temperature Surface temperature |
| title | Acceleration of Climate Change in the Upper Layer of the Black Sea |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-13T16%3A39%3A10IST&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=Acceleration%20of%20Climate%20Change%20in%20the%20Upper%20Layer%20of%20the%20Black%20Sea&rft.jtitle=Doklady%20earth%20sciences&rft.au=Korotaev,%20G.%20K.&rft.date=2024-09-01&rft.volume=518&rft.issue=1&rft.spage=1550&rft.epage=1555&rft.pages=1550-1555&rft.issn=1028-334X&rft.eissn=1531-8354&rft_id=info:doi/10.1134/S1028334X24602797&rft_dat=%3Cproquest_cross%3E3085226046%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=3085226046&rft_id=info:pmid/&rfr_iscdi=true |