dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel Barents Sea Inflow Shutdown: A New Mechanism for Rapid Climate Changes
VerfasserIn V. A. Semenov, W. Park, M. Latif
Konferenz EGU General Assembly 2009
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 11 (2009)
Datensatznummer 250022956
 
Zusammenfassung
A new mechanism for rapid climate transitions in the high latitudes is described which involves complex ocean-sea ice-atmosphere interactions. A shutdown of the Barents Sea Inflow (BSI) which carries a vast amount of heat into the Arctic Ocean is at the heart of the mechanism. The BSI shutdown is studied in a multi-millennium integration with a global climate model forced by periodically (1000 yr) varying solar constant (+-2W/m2). A positive feedback exists in the model between the inflow, the sea ice cover, and the atmospheric circulation, and BSI shutdown events are associated with a strong cooling in the northern latitudes and a subsequent rearrangement of the Arctic Ocean surface current system. The results reveal the existence of a bifurcation point in the Arctic climate system and provide a new perspective for understanding rapid climate fluctuations evident in paleo-climate records of the North Atlantic, the Nordic Seas, and Europe.