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es ack n, eoscie 3; acc he L lanti Th depe ptur ar, a Eve present-day circulation can settle into a stable ‘off ’ mode, whereas the glacial THC was mono-stable. Mono-stability may serve as an Clark et al., 2002). The concept of THC fluctuations results suggest that the THC is highly sensitive to cha...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.491.5810 2023-05-15T17:31:27+02:00 ce Re The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.491.5810 http://www.ifm.zmaw.de/fileadmin/files/images/Staff/romanova/Prange_et_al_04.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.491.5810 http://www.ifm.zmaw.de/fileadmin/files/images/Staff/romanova/Prange_et_al_04.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.ifm.zmaw.de/fileadmin/files/images/Staff/romanova/Prange_et_al_04.pdf text ftciteseerx 2016-08-14T00:03:19Z es ack n, eoscie 3; acc he L lanti Th depe ptur ar, a Eve present-day circulation can settle into a stable ‘off ’ mode, whereas the glacial THC was mono-stable. Mono-stability may serve as an Clark et al., 2002). The concept of THC fluctuations results suggest that the THC is highly sensitive to changes in the North Atlantic freshwater budget, such that anomalous freshwater inputs can trigger a collapse state for the spatial pattern of sea surface temperature tempo-spatial signature in the Atlantic Ocean can only be simulated by perturbing a glacial state of the ocean. ARTICLE IN PRESSof the circulation, thereby causing an abrupt tempera-2. Glacial climate simulations with an AGCM We employ three different SST reconstructions for the Text North Atlantic Unknown |
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es ack n, eoscie 3; acc he L lanti Th depe ptur ar, a Eve present-day circulation can settle into a stable ‘off ’ mode, whereas the glacial THC was mono-stable. Mono-stability may serve as an Clark et al., 2002). The concept of THC fluctuations results suggest that the THC is highly sensitive to changes in the North Atlantic freshwater budget, such that anomalous freshwater inputs can trigger a collapse state for the spatial pattern of sea surface temperature tempo-spatial signature in the Atlantic Ocean can only be simulated by perturbing a glacial state of the ocean. ARTICLE IN PRESSof the circulation, thereby causing an abrupt tempera-2. Glacial climate simulations with an AGCM We employ three different SST reconstructions for the |
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The Pennsylvania State University CiteSeerX Archives |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.491.5810 http://www.ifm.zmaw.de/fileadmin/files/images/Staff/romanova/Prange_et_al_04.pdf |
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North Atlantic |
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North Atlantic |
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http://www.ifm.zmaw.de/fileadmin/files/images/Staff/romanova/Prange_et_al_04.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.491.5810 http://www.ifm.zmaw.de/fileadmin/files/images/Staff/romanova/Prange_et_al_04.pdf |
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