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Ropert-Coudert Y, Hindell MA, Phillips R, Charrassin JB, Trudelle L, Raymond B. (2014). Chapter 8. Biogeographic patterns of birds and mammals.
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. (2014). Chapter 12. Conclusions: present and future of Southern Ocean Biogeography.
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. (2014). Long-Period Moment-Tensor Inversion: The Global CMT Project.
Abstract: Book title : Encyclopedia of Earthquake Engineering
Programme: 133
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Sittler, B., J. Lang, and O. Gilg. (2015). (Vol. 53). Bachelor's thesis, , .
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. (2015). Statistical analysis of CMEs' geoeffectiveness over one year of solar maximum during cycle 23.
Abstract: 26th IUGG general assembly 2015
Programme: 139
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Leduc-Leballeur Marion, Picard Ghislain, Mialon Arnaud, Arnaud Laurent, Lefebvre Eric, Possenti Philippe, Kerr Yann, . (2015). Modeling L-Band Brightness Temperature at Dome C in Antarctica and Comparison With SMOS Observations (Vol. 53). Bachelor's thesis, , .
Keywords: Antarctica, Brightness temperature, Dome C, Ice, L-band, L-band brightness temperature, L-band characteristics, Microwave, SMOS observations, Scattering, Snow, Temperature measurement, brightness suggest snowpack, emission e-folding depth, hydrological techniques, incidence angles, ocean waves, radiative transfer, radiative transfer (RT) theory, radiative transfer theory, remote sensing, seasonal variations, snow, snow emission stability, snow properties, snowpack variability density, soil, soil moisture ocean salinity satellite observation, wave approach, wave theory,
Programme: 1073,1110
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. (2015). Cephalic kidney and spleen cell culture in Antarctic teleosts. In Ozouf-Costaz C., Pisano. E., Foresti F. & L.F. de Almeida toledo, Eds. Fish cytogenetic techniques. Rau-fin fish and chondrichthyans. pp. 74-81.CRC Press..
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ANTOMARCHI V., JOLIET F. (2015).
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Bost Charles-André, Delord Karine, Barbraud Christophe, Cotté Cédric, Péron Clara, Weimerskirch Henri. (2014). The King Penguin: Life History, current status and priority conservation actions.
Abstract: In: Penguins Book. (Eds P. dee Boersma & P. G. Borboroglu), University of Washinton Press, Washington. In press
Programme: 109
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. (2017). Late Holocene glacier activity on the Kerguelen Island, South Indian Ocean – reconstructed from distal glacier-fed lake sediments. Bachelor's thesis, , .
Abstract: The Southern Hemisphere`s westerly winds play a vital role in regulating Earth`s climate by shielding Antarctic ice from low latitude heat, driving global ocean circulation and storing vast amounts of CO2. Both strength and position of this globally significant atmospheric pattern are rapidly shifting in the face of ongoing warming. A string of recent studies links these developments to dramatic changes in temperature, precipitation, sea ice extent and cryosphere stability unfolding throughout the Southern Ocean region. Critically, a lack of baseline information restricts our ability to understand the causes and patterns of these shifts and represent them in the future projections that underpin climate policies. Especially in the Southern Ocean, there are few time series recording past climate due to few suitable land areas and the few Sub-Antarctic Islands is remote and has cumbersome logistics. Kerguelen Island is located within the Antarctic Circumpolar Current and the Southern Westerly wind belt and contains several glaciers and smaller ice caps. Terrestrial archives recording past history of the glaciers at Kerguelen thus have a unique potential to record past changes in oceanic and atmospheric circulation patterns from southern mid latitudes. Here we present results from the first distal glacier fed lake study at the Kerguelen Island. A 2.8 m long sediment core was obtained from Lac Guynemer (121masl.), a lake that receives glacial meltwater from Glacier Guynemer at the Pic Guynemer (1188masl.), located at the Peninsule Loranchet at the northern part of Kerguelen Island. The sediment core has been analyzed with highresolution core scanning X-ray fluorescence (XRF), CT scanning, magnetic parameters, loss on ignition and dry bulk density, to reconstruct past glacier variability of Glacier Guynemer. The sediment record covers an interval over c. 1000 – 3500 cal. yr BP and show dynamic glacier variability during the Neoglacial time period, in phase with other glaciers reconstructed from the Southern Hemisphere.
Programme: 1094
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