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Charrier I., Jouventin P., Mathevon N. & Aubin T. (2001). Individual identify coding depends on call type in the south polar skua Catharacta maccormicki. Polar Biol., 24, 378–382.
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Bourgeois O., Dauteuil O. & Van Vliet Lanoe B. (2000). Geothermal control on flow patterns in the last glacial maximum ice sheet of iceland. Earth surface processes and landforms, 25, 59–76.
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Gounelle M., Maurette M., Engrand C. & Kurat G. (1998). Cometary origin for Antarctic micrometeorites: new experimental evidence. Meteorit Planet Sci, 33, 61.
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Bocher P., Labidoire B. & Cherel Y. (2000). Maximum dive depths of common diving petrels(pelecanoides urinatrix) during the annual cycle Mayes Island, Kerguelen. J. Zool. (Lond.), 251, 517–524.
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Bondar T N, Golovkov V P, . (1992). IZMIRAN Candidate Models for DGRF 1985, IGRF 1990 and a Secular Variation Forecast Model for the 1990-1995 Period
. Journal of geomagnetism and geoelectricity, 44(9), 709–717.
Abstract: Two candidate main field models for 1985 and 1990 as well as a forecast for the secular variation are represented as a series of spherical harmonic coefficients up to n=m=10 and n=m=8, respectively. IZMSV, US/UK, USGS forecasting models are compared with extrapolated secular variation observations and with one another. The IZMSV and the USGS are shown to agree best.
Programme: 139
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Frenot Y. & Jouventin P. (1998).
Abstract: station Biologique Paimpont:Rapport interne IFRTP
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Murphy B.F. & Pettre P. (1995). Investigation of changes in tne variability of high southern latitude circulation with the ARPEGE Climate Model. 2..
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Pisano E., Ozouf Costaz C., Hureau J.C. & Williams R. (1995). Antarct. Sci., 7(4), 381–386.
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Bergerat F., Angelier J. & Homberg C. (2000). Tectonics, 19(6), 1161–1177.
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Pilpenko V.A., Kleimenova N.G., Kozyreva O.V., Yumoto K. & Bitterly J. (1996). Is cusp the source of middle latitude Pc3 ? Geomagnetism and aeronomy, 36(2), 36–48.
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