Ukrainian Antarctic Journal

No 12 (2013): Ukrainian Antarctic Journal
Articles

The results of oceanographic researches in the coastal regions of Indian sector of Antarctica in December, 2011 and January-February, 2012 (by materials of 57th Russian Antarctic expedition)

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  • A. Yu. Artamonov,
  • Yu. V. Artamonov,
  • V. I. Bochkarev,
  • V. P. Bunyakin,
  • I. A. Repina
A. Yu. Artamonov
A.M. Obukhov Institute of Atmospheric Physics of Russian Academy of Sciences, Moscow
Yu. V. Artamonov
Marine Hydrophysical Institute of NAS of Ukraine, Sevastopol
V. I. Bochkarev
National Antarctic Scientific Center of the State Agency for Science, Innovations and Informatization, Kyiv
V. P. Bunyakin
Arctic and Antarctic Research Institute of the Federal Service for Hydrometeorology and Environmental Monitoring of Russia, Saint Petersburg
I. A. Repina
A.M.Obukhov Institute of Atmospheric Physics Russian Academy of Sciences, Moscow
DOI: https://doi.org/10.33275/1727-7485.12.2013.256
Published December 15, 2013
Keywords
  • thermohaline water structure,
  • atmosphere,
  • intra-daily variability,
  • inter-daily changes,
  • synoptic processes,
  • Sanny fjord,
  • Pruds Bay,
  • Sodruzhestva Sea,
  • Indian sector of Antarctica,
  • Antarctic adjacent oceans areas
    • ...More
    Less
How to Cite
Artamonov, A. Y., Artamonov, Y. V., Bochkarev, V. I., Bunyakin, V. P., & Repina, I. A. (2013). The results of oceanographic researches in the coastal regions of Indian sector of Antarctica in December, 2011 and January-February, 2012 (by materials of 57th Russian Antarctic expedition). Ukrainian Antarctic Journal, (12), 126-137. https://doi.org/10.33275/1727-7485.12.2013.256

Abstract

In the work the results of thermohaline water structure investigations in coastal regions of Indian sector of Antarctica, carrying out R/V “Academic Fedorov” in December, 2011 and January-February, 2012 are presented. Shown, that the intra-daily variability of temperature and salinity field is observed against a background of inter-daily changes, which due to displacement of boundary between cold and more fresh shelf water and more warm and salty ocean water. The water structure reconstruction is result from the active synoptic processes in atmosphere above Antarctic adjacent oceans areas.

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References

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