VIAF

Virtual International Authority File

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Leader     00000nz a2200037n 45 0
001     WKP|Q57084904  (VIAF cluster)  (Authority/Source Record)
003     WKP
005     20241121000323.0
008     241121nneanz||abbn n and d
035 ‎‡a  (WKP)Q57084904‏
024 ‎‡a  0000-0002-1333-2544‏ ‎‡2  orcid‏
035 ‎‡a  (OCoLC)Q57084904‏
100 0 ‎‡a  James A Smith‏ ‎‡9  it‏ ‎‡9  es‏ ‎‡9  ast‏
375 ‎‡a  1‏ ‎‡2  iso5218‏
400 0 ‎‡a  জেমস এ স্মিথ‏ ‎‡9  bn‏
400 0 ‎‡a  James A. Smith‏ ‎‡c  researcher on Antarctica‏ ‎‡9  en‏
400 0 ‎‡a  James A Smith‏ ‎‡c  onderzoeker‏ ‎‡9  nl‏
670 ‎‡a  Author's Anthropogenic and internal drivers of wind changes over the Amundsen Sea, West Antarctica, during the 20th and 21st centuries‏
670 ‎‡a  Author's Enhanced glacial discharge from the eastern Antarctic Peninsula since the 1700s associated with a positive Southern Annular Mode‏
670 ‎‡a  Author's Evidence for a palaeo-subglacial lake on the Antarctic continental shelf‏
670 ‎‡a  Author's Holocene history of the 79° N ice shelf reconstructed from epishelf lake and uplifted glaciomarine sediments‏
670 ‎‡a  Author's How much, how deposited, how old – what can we learn from sediments in Pine Island Bay?‏
670 ‎‡a  Author's Initial results from International Thwaites Glacier Collaboration cruise NBP20-02‏
670 ‎‡a  Author's Rapid retreat of Thwaites Glacier in the pre-satellite era‏
670 ‎‡a  Author's Temperate rainforests near the South Pole during peak Cretaceous warmth‏
670 ‎‡a  Author's The marine geological imprint of Antarctic ice shelves‏
909 ‎‡a  (orcid) 0000000213332544‏ ‎‡9  1‏
919 ‎‡a  anthropogenicandinternaldriversofwindchangesovertheamundsenseawestantarcticaduringthe20and21stcenturies‏ ‎‡A  Anthropogenic and internal drivers of wind changes over the Amundsen Sea, West Antarctica, during the 20th and 21st centuries‏ ‎‡9  1‏
919 ‎‡a  marinegeologicalimprintofantarcticiceshelves‏ ‎‡A  The marine geological imprint of Antarctic ice shelves‏ ‎‡9  1‏
919 ‎‡a  temperaterainforestsnearthesouthpoleduringpeakcretaceouswarmth‏ ‎‡A  Temperate rainforests near the South Pole during peak Cretaceous warmth‏ ‎‡9  1‏
919 ‎‡a  rapidretreatofthwaitesglacierinthepresatelliteera‏ ‎‡A  Rapid retreat of Thwaites Glacier in the pre-satellite era‏ ‎‡9  1‏
919 ‎‡a  initialresultsfrominternationalthwaitesglaciercollaborationcruisenbp2002‏ ‎‡A  Initial results from International Thwaites Glacier Collaboration cruise NBP20-02‏ ‎‡9  1‏
919 ‎‡a  howmuchhowdepositedhowoldwhatcanwelearnfromsedimentsinpineislandbay‏ ‎‡A  How much, how deposited, how old – what can we learn from sediments in Pine Island Bay?‏ ‎‡9  1‏
919 ‎‡a  holocenehistoryofthe79niceshelfreconstructedfromepishelflakeandupliftedglaciomarinesediments‏ ‎‡A  Holocene history of the 79° N ice shelf reconstructed from epishelf lake and uplifted glaciomarine sediments‏ ‎‡9  1‏
919 ‎‡a  evidenceforapalaeosubglaciallakeontheantarcticcontinentalshelf‏ ‎‡A  Evidence for a palaeo-subglacial lake on the Antarctic continental shelf‏ ‎‡9  1‏
919 ‎‡a  enhancedglacialdischargefromtheeasternantarcticpeninsulasincethe1700sassociatedwithapositivesouthernannularmode‏ ‎‡A  Enhanced glacial discharge from the eastern Antarctic Peninsula since the 1700s associated with a positive Southern Annular Mode‏ ‎‡9  1‏
946 ‎‡a  b‏ ‎‡9  1‏
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997 ‎‡a  0 0 lived 0 0‏ ‎‡9  1‏