Abstract
In the framework of this consideration we will primarily address research topics of the Antarctic region which are more or less interrelated with global climate. Earlier as well as recent field and model investigations have provided convincing evidence that certain physical processes in the polar atmosphere, ocean and cryosphere may support, enhance or even initiate global climate changes. Since the main components of the Earth’s climate are strongly coupled through non-linear interaction mechanisms, any perturbations excited somewhere in the system may suffer from significant changes in amplitude and frequency during their migration through the interrelated physical domain. Therefore, investigations of Antarctic geophysical processes should ideally cover a wide range of time and space scales and should include all important interacting climate elements. But in reality individual field observations and model studies have to be limited with respect to space and time due to technical, logistic and financial restrictions as well as to the lack of experienced manpower. Consequently, international programmes are required to create joint research projects in such a way that various single contributions may provide a satisfactory basis for reasonable syntheses.
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References
Egger J (1991) On the mean atmospheric circulation over Antarctica. Geophys Astrophys Fluid Dynam 58: 75–90
Foldvik A, Gammelsroed T, Slotsvik N, Toerrensen T (1985) Oceanographic conditions on the Weddell Sea shelf during the German Antarctic expedition 1979/80. Polar Res 3: 209–226
Hellmer HH, Olbers D (1991) On the thermohaline circulation under the Filchner-Ronne ice shelves. Antarct Sci 3: 433–442
Hibler WD III, Ackley SF (1983) Numerical simulations of the Weddell Sea pack-ice. J Geophys Res 88: 2873–2887
Hibler WD III, Bryan K (1987) A diagnostic ice-ocean model. J Phys Oceanogr 17: 987–1015
Koch C (1988) A coupled sea-ice-atmospheric boundary layer model. Part I: Description of the model and 1979 standard run. Beitr Phys Atmos 61: 344–354
Lemke P, Owens WB, Hibler WD III (1990) A coupled sea ice-mixed layer pycnocline model for the Weddell Sea. J Geophys Res 95: 9513–9525
Oerter H, Eicken H, Miller H (1991) The physical properties of the marine ice under the Filchner-Ronne shelf ice, Filch.-Ronne Ice Shelf Progr Rep 5. Alfred-Wegener-Inst, Bremerhaven, pp 13–18
Simmonds I, Budd WF (1990) A simple parameterization of ice leads in a general circulation model, and the sensitivity of climate to change in Antarctic ice concentration. Ann Glaciol 14: 266–269
Weiss RF (1987) Winter Weddell Sea Project 1986: Trace gas studies duing legs ANT V/2 and V/3 of Polarstern. Antarct J US 22: 99–100
Wolff J-O, Maier-Raimer E, Olbers D (1991) Wind-driven flow over topography in a zonal ß-plane channel: a quasigeostrophic model of the Antarctic Circumpolar Current. J Phys Oceanogr 21: 236–264
Zwally HJ, Comiso JC, Parkinson C, Campbell WJ, Carsey FD, Gloersen P (1983) Antarctic sea ice, 1973–1976: Satellite passive-microwave observations. NASA, Washington, DC, 206 pp
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© 1994 Springer-Verlag Berlin Heidelberg
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Augstein, E. (1994). Future Ocean-Atmosphere Research in the Antarctic Region. In: Hempel, G. (eds) Antarctic Science. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-78711-9_17
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DOI: https://doi.org/10.1007/978-3-642-78711-9_17
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-540-57559-7
Online ISBN: 978-3-642-78711-9
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