By Jaswant Singh, H. N. Dutta
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Additional resources for Antarctica: The Most Interactive Ice-Air-Ocean Environment (Arctic Regioni and Antarctica Issues and Research)
Undoubtedly, the open ocean spaces are at a much higher temperature than the areas covered by a variety of sea ice. This type of variability may not be seen on daily basis, Figure 10. shows the facsimile recorded on February 10, 2002, in which surface based inversion is predominantly present in the lower atmosphere. However, dull thermal convection seems to be appearing during 10001400 hrs. At the same time, the surface based inversion is spiky, which means, vertical movement of wind or turbulence is present in the lower atmosphere.
Mauldin, M. Hutterli, J. Dibb, D. B. Brooks, B. M. Roberts, Y. Wang, D. Tan and F. Flocke: Antarctic tropospheric chemistry investigation (ANTCI) 2003 overview, Atmospheric Environment. 42, 27492761 (2008). , Kodama, Y. , Winter warming over Dome Fuji, East Antarctica and semiannual oscillation in the atmospheric circulation. J. Geoph. 1029/98JD02001 (1998). , J. Savarino, S. Morin, J. F. Martins: Photolysis imprint in the nitrate stable isotope signal in snow and atmosphere of East Antarctica and implications for reactive nitrogen cycling, Atmos.
Int. J. , 20, 21-34 (2004). , Study of Environmental Parameters in relation to the ecosystem over Antarctica, Ph. D. Thesis, Guru Jambeshwar University, Hisar. December, 2002. Genthon, C. and G. Krinner: Antarctic surface mass balance and systematic biases in general circulation models. J. Geoph. , 106, 20653-20664 (2001). , S. K. K. Pasricha, Kh. N. Dutta Sodar studies of foggy boundary layer characteristics. In Proceedings of the 11th International Symposium on Acoustic Remote Sensing (ISARS) and Associated Techniques of the Atmosphere and Oceans, Rome, Italy, 24-28 June 263-266 (2002).
Antarctica: The Most Interactive Ice-Air-Ocean Environment (Arctic Regioni and Antarctica Issues and Research) by Jaswant Singh, H. N. Dutta