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- > Climate change and variability. Special issue (supprimer)
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Par Collection Par Auteur- SÄLLSKAPET, S., (Editeur scientifique) (3)
- HAAKENSEN, N. (1)
- HANSSON, M. (1)
- HOLMGREN, K. (1)
- MÖRTH, M. (1)
- NYMAN, M. (1)
- ONAC, B.P. (1)
- PERŞOIU, A. (1)
- ROCCHI, S. (1)
- SALINGER, M.J. (1)
- WINKLER, S. (1)
- CHINN, T. (1)
- HOLMLUND, P. (1)
- LEMASURIER, W.E. (1)
- 2005 (3)
- Analyse isotopique ; Antarctique ; Cénozoïque ; Erosion glaciaire ; Fluctuation du glacier ; Microfossile ; Oxygène 18 ; Paléoclimatologie ; Paléogéographie ; Roche volcanique (1)
- Antarctica ; Cenozoic ; Glacial erosion ; Glacier fluctuation ; Isotope analysis ; Oxygen 18 ; Palaeoclimatology ; Palaeogeography ; Volcanic rock (1)
- Atmospheric circulation ; El Niño ; Glacier ; Glacier advance ; Glacier mass balance ; Holocene ; New Zealand ; Norway ; Ocean atmosphere interaction (1)
- Avancée du glacier ; Bilan de masse ; Circulation atmosphérique ; El Niño ; Glacier ; Holocène ; Interaction océan-atmosphère ; Norvège ; Nouvelle-Zélande (1)
- C 14 dating ; Cave ; Glaciology ; Ice ; Karst ; Organic materials ; Palaeoclimatology ; Permafrost ; Romania (1)
- Datation C 14 ; Glace ; Glaciologie ; Grotte ; Karst ; Matière organique ; Paléoclimatologie ; Pergélisol ; Roumanie (1)
- Climate change and variability. Special issue (3)
- Assessing the palaeoclimate potential of cave glaciers : the example of the Scărişoara ice cave (Romania) (1)
- Recent glacier advances in Norway and New Zealand : a comparison of their glaciological and meteorological causes (1)
- Terrestrial record of Post-Eocene climate history in Marie Byrd Land (MBL), West Antarctica (1)
- Norway and New Zealand both experienced recent glacial advances, commencing in the early 1980s and ceasing around 2000, which were more exensive than any other since the end of the Little Ice Age. Common to both countries, the positive glacier
- to the present. The AA. have attempted to synthesize these data sources to provide a more complete record, and to reconcile them with climatic events recorded elsewhere in Antarctica and the deep sea.
- spans more than 1000 years. Observations on the exposure indicate that a basal melting phase may have occurred in the past.