|
|
Biuw M., Boehme L., Guinet C., Hindell M., Costa D., Charrassin J.B., Roquet F., Bailleul F., Meredith M., Thorpe S, Tremblay Y, McDonald B., Park Y.-H., Rintoul S., Bindoff N., Goebel M., Crocker D., Lovell P., Nicholson J., Monks F., Fedak M. (2007). Variations in behaviour and condition of a Southern Ocean top predator in relation to in-situ oceanographic conditions. Proc. Natl. Acad. Sci. U.S.A., 104, 13705–13710.
|
|
|
|
Schott, J.J., and Linthe H.J. (2007). The hourly mean computation problem revisited. (Vol. 398). Bachelor's thesis, , .
|
|
|
|
Andriambahoaka, Z., Schott, J.J., and Ranaivonomenjanahary F. (2007). Repeat station data reduction using the CM4 model. (Vol. 398). Bachelor's thesis, , .
Abstract: Publs. Inst. Geophys. Pol. Acad. Sc.
Programme: 139;905
|
|
|
|
Frenot Y., Convey P., Lebouvier M., Chown S.L., Whinam J., Selkirk P.M., Skotnicki M. & Bergstrom D.M. (2008). Antarctic and Subantarctic Biological Invasions: Sources, extents, impacts and implications. Gateway Antarctica, 801, 53–96.
Abstract: In Rogan-Finnemore M. (ed) Non-native species in the Antarctic. Gateway Antarctica Special Publication Series, Number 0801
Programme: 136
|
|
|
|
De Meeûs, T, K.D. McCoy, F. Prugnolle, P. Durand, C. Chevillon, S. Hurtrez-Boussès & F. Renaud. (2007). Population genetics and molecular epidemiology or how to «débusquer la bête”. Infection Genetics Evolution. Infection Genetics Evolution, 7, 308–332.
|
|
|
|
ANGELIER F, MOE B, CLEMENT-CHASTEL C, BECH C, CHASTEL O. (2007). Corticosterone levels in relation to change of mate in Black-legged kittiwakes. Condor, 109, 668–674.
|
|
|
|
ANGELIER F, CLEMENT-CHASTEL C, GABRIELSEN GW, CHASTEL O. (2007). Corticosterone and Time-activity budget: an experiment with Black-legged kittiwakes. Hormones and behavior, 52, 487–491.
|
|
|
|
Motte E., Ricaud P., Gabard B., Niclas M. & Gangneron F. (2008). A 22 GHz Mobile Microwave Radiometer (MobRa) for the study of stratospheric water vapor. IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 46(10), 3104–3114.
|
|
|
|
Morin, S. (2008). Analyse de la composition isotopique de l’ion nitrate dans la basse atmosphère polaire et marine. Doctoral thesis, , .
Abstract: PhD Dissertation, Univ. Paris Est (Marne la Vallée, France), 2008
Thèse de Doctorat. Université Paris Est
Programme: 355;1011
|
|
|
|
Charrassin, J.B., Hindell, M., Rintoul, S.R., Roquet, F., Sokolov,S., Biuw, M., Costa D., Boehme, L.,Lovell, P., Coleman R., Timmerman, R., Meijers A., Meredith M., Park Y.H., Bailleul F., Tremblay Y., Bost C.A., McMahon C.R., Field I.C., Fedak M.A. , Guinet C. (2008). Southern Ocean frontal structure and sea ice formation rates revealed by elephant seals. Proc. Natl. Acad. Sci. U.S.A., 105, 11634–11639.
Abstract: Polar regions are particularly sensitive to climate change, with the potential for significant feedbacks between ocean circulation, sea ice, and the ocean carbon cycle. However, the difficulty in obtaining in situ data means that our ability to detect and interpret change is very limited, especially in the Southern Ocean, where the ocean beneath the sea ice remains almost entirely unobserved and the rate of sea-ice formation is poorly known. Here, we show that southern elephant seals (Mirounga leonina) equipped with oceanographic sensors can measure ocean structure and water mass changes in regions and seasons rarely observed with traditional oceanographic platforms. In particular, seals provided a 30-fold increase in hydrographic profiles from the sea-ice zone, allowing the major fronts to be mapped south of 60°S and sea-ice formation rates to be inferred from changes in upper ocean salinity. Sea-ice production rates peaked in early winter (April–May) during the rapid northward expansion of the pack ice and declined by a factor of 2 to 3 between May and August, in agreement with a three-dimensional coupled ocean–sea-ice model. By measuring the high-latitude ocean during winter, elephant seals fill a “blind spot” in our sampling coverage, enabling the establishment of a truly global ocean-observing system.
Programme: 109;394;452
|
|
