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Autor:
Patton, Genevieve
To better understand how our climate will change in the future, we look to past analogues of our current climate and rely on indicators of past fluctuations preserved in marine sediment. One such indicator is the isotopic composition of neodymium pre
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https://explore.openaire.eu/search/publication?articleId=doi_________::39be730065a5508b759dcb02c61e1df9
Autor:
Mulitza, Stefan, Bergmann, Fenna, Br��ck, Liane, Chiessi, Cristiano Mazur, Govin, Aline, Klann, Marco, Kuhnert, Henning, L��bben, Birgit, Max, Lars, Meyer, Vera, Morard, Raphael, M��ller, Vasco, Patton, Genevieve, Paul, Andr��, Poirier, Andr��, Riesen, Paul, Schade, Tobias, St��ber, Uwe, V��lker, Georg Sebastian, V��lpel, Rike, Von Dobeneck, Tilo
Abrupt millennial-scale climate fluctuations have been associated with changes in the Atlantic Meridional Overturning Circulation (AMOC) and particularly North Atlantic Deep Water (NADW) formation. Information on the history of Labrador Sea Water (LS
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f4aefcc4f0fc9f22a366bef60628531