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- W643674828 abstract "A unique multi-proxy reconstruction of surface and bottom water conditions in Marguerite Bay, documents the influence of warm upper circumpolar deep water (UCDW) on the West Antarctic Peninsula through the Holocene. We demonstrate that persistent incursions of UCDW during the early Holocene were associated with restricted sea ice, enhanced primary productivity and ice shelf collapse. From ~6 kyr BP the influence of UCDW in Marguerite Bay began to wane, coincident with the equatorward migration of the Southern Hemisphere Westerly Winds (SWW). Weakening UCDW influence continued through the Holocene and by ~3.7 kyr BP lengthy sea ice seasons within Marguerite Bay were only episodically interrupted by incursions of UCDW. This late Holocene interval appears to have been sensitive to ENSO forcing as opposed to the SWW-forcing that dominated the early to mid Holocene. However, recent observations suggest that the early Holocene-like oceanographic configuration is now becoming re-established along the WAP as SWW intensify and explains the recent accelerated ice shelf loss." @default.
- W643674828 created "2016-06-24" @default.
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- W643674828 date "2013-01-01" @default.
- W643674828 modified "2023-09-27" @default.
- W643674828 title "Recent Antarctic Peninsula warm water upwelling linked to accelerated ice shelf loss" @default.
- W643674828 hasPublicationYear "2013" @default.
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