{"id":26,"date":"2020-08-10T08:11:40","date_gmt":"2020-08-10T07:11:40","guid":{"rendered":"http:\/\/www.oceanblogs.org\/msm94\/?page_id=26"},"modified":"2020-08-10T08:19:20","modified_gmt":"2020-08-10T07:19:20","slug":"uber-about","status":"publish","type":"page","link":"https:\/\/www.oceanblogs.org\/msm94\/uber-about\/","title":{"rendered":"\u00dcber \/ About"},"content":{"rendered":"\n<p>Der Tiefe Westliche Randstrom (DWBC) im Subpolaren Nordatlantik stellt eine Schl\u00fcsselkomponente der Thermohalinen Zirkulation dar. Schwankungen im Volumentransport und der Charakteristik der Wassermassen im DWBC k\u00f6nnen Indikatoren f\u00fcr Klima\u00e4nderungen sein. Das dichteste Wasser im Randstrom wird aus der Overflow\/Entrainment Quelle (haupts\u00e4chlich D\u00e4nemark Stra\u00dfe Overflow) im Gr\u00f6nland-Schottland R\u00fccken eingespeist. Leichtere Wasser werden aus den Konvektionsgebieten des Subpolaren Nordatlantiks, haupts\u00e4chlich der Labradorsee, eingebracht. Die Daten, die w\u00e4hrend der Fahrt MSM94 gewonnen werden, dienen dazu, die Prozesse in der Fokusregionen Labradorsee besser zu verstehen. Die Fahrt ist stark in internationale Programme und Analysen eingebettet, die unter anderem die St\u00e4rke der Umw\u00e4lzzirkulation im Nordatlantik (<a href=\"https:\/\/www.o-snap.org\/\" target=\"_blank\" rel=\"noreferrer noopener\">OSNAP<\/a>) und die Kohlenstoffdioxidaufnahme der Labrador (\u201eOcean Frontier Institute, EU <a href=\"https:\/\/eurosea.eu\/\" target=\"_blank\" rel=\"noreferrer noopener\">EuroSea<\/a>\u201c) untersuchen. Das Arbeitsprogramm der Fahrt MSM94 beinhaltet die Aufnahme und Auslegung von verankerten Ger\u00e4ten und die Vermessung der Wassers\u00e4ule mit der CTD-Rosette und Unterwegsdaten.<\/p>\n\n\n\n<p><em>The Deep Western Boundary Current (DWBC) represents a key component of thermohaline circulation. Fluctuations in volume transport and the characteristics of water masses in the DWBC may be indicators for changes in climate. The densest water in the DWBC originate from the overflow\/entrainment sources (mainly Denmark Strait Overflow) in the Greenland-Scotland Ridge. Lighter waters are formed in the convection areas primarily in the Labrador Sea. Improvement of process understanding in the focus regions Labrador Sea will be achieved with data from the MSM94 expedition. It is embedded in international programs and analysis efforts that examine, among others, the strength of Atlantic overturning circulation (<a href=\"https:\/\/www.o-snap.org\/\" target=\"_blank\" rel=\"noreferrer noopener\">OSNAP<\/a>) and the carbon dioxide uptake of the Labrador Sea(\u2018Ocean FrontierInstitute\u2019, EU <a href=\"https:\/\/eurosea.eu\/\" target=\"_blank\" rel=\"noreferrer noopener\">EuroSea<\/a>).The work program of MSM94 include the redeployment of moorings and the surveys of the water column using the CTD Rosette and underway data.<\/em><\/p>\n\n\n\n<p><strong>Kontakt \/ Contact<\/strong><\/p>\n\n\n\n<p>Dr. Johannes Karstensen, Chief Scientist MSM94<br>GEOMAR Helmholtz Centre for Ocean Research Kiel<br><a href=\"https:\/\/www.geomar.de\/en\/jkarstensen\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/www.geomar.de\/en\/jkarstensen<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Der Tiefe Westliche Randstrom (DWBC) im Subpolaren Nordatlantik stellt eine Schl\u00fcsselkomponente der Thermohalinen Zirkulation dar. Schwankungen im Volumentransport und der Charakteristik der Wassermassen im DWBC k\u00f6nnen Indikatoren f\u00fcr Klima\u00e4nderungen sein. Das dichteste Wasser im Randstrom wird aus der Overflow\/Entrainment Quelle (haupts\u00e4chlich D\u00e4nemark Stra\u00dfe Overflow) im Gr\u00f6nland-Schottland R\u00fccken eingespeist. Leichtere Wasser werden aus den Konvektionsgebieten des [&hellip;]<\/p>\n","protected":false},"author":212,"featured_media":10,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-26","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/www.oceanblogs.org\/msm94\/wp-json\/wp\/v2\/pages\/26","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.oceanblogs.org\/msm94\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.oceanblogs.org\/msm94\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.oceanblogs.org\/msm94\/wp-json\/wp\/v2\/users\/212"}],"replies":[{"embeddable":true,"href":"https:\/\/www.oceanblogs.org\/msm94\/wp-json\/wp\/v2\/comments?post=26"}],"version-history":[{"count":4,"href":"https:\/\/www.oceanblogs.org\/msm94\/wp-json\/wp\/v2\/pages\/26\/revisions"}],"predecessor-version":[{"id":51,"href":"https:\/\/www.oceanblogs.org\/msm94\/wp-json\/wp\/v2\/pages\/26\/revisions\/51"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.oceanblogs.org\/msm94\/wp-json\/wp\/v2\/media\/10"}],"wp:attachment":[{"href":"https:\/\/www.oceanblogs.org\/msm94\/wp-json\/wp\/v2\/media?parent=26"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}