onr:"swepub:oai:DiVA.org:su-134262"
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| Fältnamn | Indikatorer | Metadata |
|---|---|---|
| 000 | 02862naa a2200445 4500 | |
| 001 | oai:DiVA.org:su-134262 | |
| 003 | SwePub | |
| 008 | 161003s2016 | |||||||||||000 ||eng| | |
| 024 | 7 | a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1342622 URI |
| 024 | 7 | a https://doi.org/10.1038/ncomms125772 DOI |
| 040 | a (SwePub)su | |
| 041 | a engb eng | |
| 042 | 9 SwePub | |
| 072 | 7 | a ref2 swepub-contenttype |
| 072 | 7 | a art2 swepub-publicationtype |
| 100 | 1 | a Williams, G. D.4 aut |
| 245 | 1 0 | a The suppression of Antarctic bottom water formation by melting ice shelves in Prydz Bay |
| 264 | c 2016-08-23 | |
| 264 | 1 | b Springer Science and Business Media LLC,c 2016 |
| 338 | a print2 rdacarrier | |
| 520 | a A fourth production region for the globally important Antarctic bottom water has been attributed to dense shelf water formation in the Cape Darnley Polynya, adjoining Prydz Bay in East Antarctica. Here we show new observations from CTD-instrumented elephant seals in 2011-2013 that provide the first complete assessment of dense shelf water formation in Prydz Bay. After a complex evolution involving opposing contributions from three polynyas (positive) and two ice shelves (negative), dense shelf water (salinity 34.65-34.7) is exported through Prydz Channel. This provides a distinct, relatively fresh contribution to Cape Darnley bottom water. Elsewhere, dense water formation is hindered by the freshwater input from the Amery and West Ice Shelves into the Prydz Bay Gyre. This study highlights the susceptibility of Antarctic bottom water to increased freshwater input from the enhanced melting of ice shelves, and ultimately the potential collapse of Antarctic bottom water formation in a warming climate. | |
| 650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskapx Multidisciplinär geovetenskap0 (SwePub)105032 hsv//swe |
| 650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geosciences, Multidisciplinary0 (SwePub)105032 hsv//eng |
| 700 | 1 | a Herraiz-Borreguero, L.4 aut |
| 700 | 1 | a Roquet, Fabienu Stockholms universitet,Meteorologiska institutionen (MISU)4 aut0 (Swepub:su)froqu |
| 700 | 1 | a Tamura, T.4 aut |
| 700 | 1 | a Ohshima, K. I.4 aut |
| 700 | 1 | a Fukamachi, Y.4 aut |
| 700 | 1 | a Fraser, A. D.4 aut |
| 700 | 1 | a Gao, L.4 aut |
| 700 | 1 | a Chen, H.4 aut |
| 700 | 1 | a McMahon, C. R.4 aut |
| 700 | 1 | a Harcourt, R.4 aut |
| 700 | 1 | a Hindell, M.4 aut |
| 710 | 2 | a Stockholms universitetb Meteorologiska institutionen (MISU)4 org |
| 773 | 0 | t Nature Communicationsd : Springer Science and Business Media LLCg 7q 7x 2041-1723 |
| 856 | 4 | u https://doi.org/10.1038/ncomms12577y Fulltext |
| 856 | 4 | u https://www.nature.com/articles/ncomms12577.pdf |
| 856 | 4 8 | u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-134262 |
| 856 | 4 8 | u https://doi.org/10.1038/ncomms12577 |
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