Sea ice formation rate and vertical structure revealed by elephant seal in wilkins sound (2010)
- Authors:
- Autor USP: WAINER, ILANA ELAZARI KLEIN COARACY - IO
- Unidade: IO
- Subjects: PLATAFORMA CONTINENTAL; SALINIDADE DO MAR
- Language: Inglês
- Imprenta:
- Publisher place: Buenos Aires
- Date published: 2010
- Conference titles: SCAR Open Science Conference
-
ABNT
SANTINI, M F et al. Sea ice formation rate and vertical structure revealed by elephant seal in wilkins sound. 2010, Anais.. Buenos Aires: Instituto Oceanográfico, Universidade de São Paulo, 2010. . Acesso em: 12 mar. 2026. -
APA
Santini, M. F., Wainer, I. E. K. C., Souza, R. B., Muelbert, M. M. C., & Hindell, M. A. (2010). Sea ice formation rate and vertical structure revealed by elephant seal in wilkins sound. In . Buenos Aires: Instituto Oceanográfico, Universidade de São Paulo. -
NLM
Santini MF, Wainer IEKC, Souza RB, Muelbert MMC, Hindell MA. Sea ice formation rate and vertical structure revealed by elephant seal in wilkins sound. 2010 ;[citado 2026 mar. 12 ] -
Vancouver
Santini MF, Wainer IEKC, Souza RB, Muelbert MMC, Hindell MA. Sea ice formation rate and vertical structure revealed by elephant seal in wilkins sound. 2010 ;[citado 2026 mar. 12 ] - Description of the mean conditions and of the interannual variability at the southwestern atlantic ocean (1982-1994)
- Labmet: O Laboratório de Meteorologia Marinha
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- Temporal analysis of water masses and sea ice formation rate west of the Antarctic Peninsula in 2008 estimated from southern elephant seals' SRDL–CTD data
- Investigação da variabilidade da água profunda do mar de weddell no século XX
- Indices climáticos de escala planetária de sua correlação com as chuvas das regiões NE e Sul do Brasil em escala decadal
- Investigação da variabilidade climática do mar de Weddell no século XX através da reanálise oceânica
- Implementation of a regional numerical model of the Southern Ocean
- Assessment of the structure and variability of weddell sea water masses in distinct ocean reanalysis products
- The impacts of deglacial meltwater forcing on the South Atlantic Ocean deep circulation since the Last Glacial Maximum
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