Difference between revisions of "Publication.10.1029/2002GL016612"
From Linked Earth Wiki
( Publication (L) )
(WTLiPD: New page Publication.10.1029/2002GL016612 with Category: Publication_(L)) |
(WTLiPD: Edit Page) |
||
Line 1: | Line 1: | ||
− | [[Category:Publication_(L)]] | + | [[Category:Publication_(L)]]{{#set:| |
+ | Abstract=Variations in tropical sea surface temperature patterns and the phasing relative to climate change in higher-latitudes provide insight into the mechanisms of climate change on both orbital and shorter time-scales. Here, we present well-dated, high-resolution records of planktonic foraminiferal 18O and Mg/Ca-based SST spanning the last deglaciation from the Sulu Sea, located in the western equatorial Pacific. The results indicate that the last glacial maximum was 2.3 ± 0.5°C cooler than present in the Sulu Sea with a concomitant decrease in sea surface salinity. The similarity between variations in surface salinity in the Sulu Sea, the western and eastern equatorial Pacific, and the Greenland ice-core record suggests that the observed changes in salinity reflect large-scale rearrangement of atmospheric patterns, which were coherent and synchronous throughout the Northern Hemisphere. The results suggest that the glacial equatorial Pacific climate was strongly influencedby both tropical, and extra-tropical forcing, although it is not clear whether interannual (ENSO) variability is a good analogue of glacial-interglacial climate change.| | ||
+ | Author (L)=Yair_Rosenthal| | ||
+ | Author (L)=Delia_W._Oppo| | ||
+ | Author (L)=Braddock_K._Linsley| | ||
+ | HasDOI (L)=10.1029/2002GL016612| | ||
+ | HasLink (L)=http://dx.doi.org/10.1029/2002GL016612| | ||
+ | Issue (L)=8| | ||
+ | Journal (L)=Geophysical Research Letters| | ||
+ | Pages (L)=1428| | ||
+ | PubDataUrl=doi.org| | ||
+ | PublicationYear (L)=2003| | ||
+ | Publisher=Wiley-Blackwell| | ||
+ | Title (L)=The amplitude and phasing of climate change during the last deglaciation in the Sulu Sea, western equatorial Pacific| | ||
+ | Type=journal-article| | ||
+ | Volume (L)=30}} |