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Mondet J., Leroux C., Vinay G., Candaudap F., Le Meur E. & Fily M. (1997). Images of Antarctic Sastrugi at different scales from Ground to Satellite..
Abstract: Proceedings of the EARSel Workshop Remote sensing of land ice and snow, University of Freiburg, Germany
Programme: 254
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Barthes L., Andre R., Cerisier J.C. & Villain J.P. (1998). Separation of multiple echoes using a high-resolution spectral analysis for SuperDARN HF rdars. Radio science, 33(4), 1005–1017.
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Francois J.M., Altintas A. & Gerday C. (1997). Characterization of the single Tyrosine containing Troponin C from Lungfish white muscle. Comparison with several fast skeletal muscle Troponin C's from fish species. Comp. Biochem. Physiol., Part A Mol. Integr. Physiol., 117B(4), 589–598.
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Murphy B.F. (1996). The performance of the arpege-climat general circulation model in the Antarctic. (Vol. 51).
Abstract: Note de centre: METEO FRANCE
Programme: 211
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. (2007). Comparison of polar ozone loss rates simulated by one-dimensional and three-dimensional models with Match observations in recent Antarctic and Arctic winters. J. Geophys. Res., 112.
Abstract: Simulations of ozone loss rates using a three-dimensional chemical transport model and a box model during recent Antarctic and Arctic winters are compared with experimental loss rates. The study focused on the Antarctic winter 2003, during which the first Antarctic Match campaign was organized, and on Arctic winters 1999/2000, 2002/2003. The maximum ozone loss rates retrieved by the Match technique for the winters and levels studied reached 6 ppbv/sunlit hour and both types of simulations could generally reproduce the observations at 2-sigma error bar level. In some cases, for example, for the Arctic winter 2002/2003 at 475 K level, an excellent agreement within 1-sigma standard deviation level was obtained. An overestimation was also found with the box model simulation at some isentropic levels for the Antarctic winter and the Arctic winter 1999/2000, indicating an overestimation of chlorine activation in the model. Loss rates in the Antarctic show signs of saturation in September, which have to be considered in the comparison. Sensitivity tests were performed with the box model in order to assess the impact of kinetic parameters of the ClO-Cl2O2 catalytic cycle and total bromine content on the ozone loss rate. These tests resulted in a maximum change in ozone loss rates of 1.2 ppbv/sunlit hour, generally in high solar zenith angle conditions. In some cases, a better agreement was achieved with fastest photolysis of Cl2O2 and additional source of total inorganic bromine but at the expense of overestimation of smaller ozone loss rates derived later in the winter.
Keywords: Ozone loss rates; transport model; trajectory model; 0340 Atmospheric Composition and Structure: Middle atmosphere: composition and chemistry; 0341 Atmospheric Composition and Structure: Middle atmosphere: constituent transport and chemistry; 3334 Atmospheric Processes: Middle atmosphere dynamics; 3360 Atmospheric Processes: Remote sensing; 3319 Atmospheric Processes: General circulation
Programme: 209
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Loeb V.J., Kellermann A.K., Koubbi P., North A.W. & Wwhite M.G. (1993). Antarctic larval fish assemblages: a review. Bull. Mar. Sci., 53(2), 416–449.
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Condis C., Rivera L. & Muller A. (1997). EOPG, Strasbourg, .
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Delille D., Marty G., Cansemi Soullard M. & Frankignoulle M. (1997). Influence of subantarctic Macrocystis bed metabolism in diel changes of marine bacterioplankton and CO2 fluxes. J. Plankton Res., 19(9), 1251–1264.
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Couartou O. & Sanchez L. (1996).
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Maurette M., Brownlee D.E., Sutton S.R., Joswick D. & Joswiak A.C. (1992). Antarctic micrometeorites smaller than 50 um. Lunar and planetary science, 23, 857–858.
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