A G.C.M. simulation of the importance of insolation forcing for the initiation of the Laurentide ice sheet = Une simulation «General Circulation Model» (GCM) sur l'importance de l'insolation ayant provoqué la formation de la calotte glaciaire LaurentideROYER, J. F; DEQUE, M; PESTIAUX, P et al.Palaeoclimatic research and models. Workshop. 1983, pp 164-167Conference Paper

Towards an inventory of the great ice sheets = Vers un inventaire des grandes calottes glaciairesSWITHINBANK, C.Geografiska annaler. Series A. Physical geography. 1983, Vol 65, Num 3-4, pp 289-294, issn 0435-3676Article

IZOTOPNAYA I GEOKHIMICHESKAYA GLYATSIOLOGIYA = GLACIOLOGIE GEOCHIMIQUE ET ISOTOPIQUEKOTLYAROV VLADIMIR MIKHAJLOVICH; GORDIENKO FELIKS GENNADIEVICH.1982; ; SUN; LENINGRAD: GIDROMETEOIZDAT; DA. 1982; 288 P.; 22 CM; ABS. ENG; BIBL. 259 REF.; ILL.Book

Flow law for ice in polar ice sheetsDOAKE, C. S. M; WOLFF, E. W.Nature (London). 1985, Vol 314, Num 6008, pp 255-257, issn 0028-0836Article

Basal sliding relations deduced from ice-sheet dataMORLAND, L. W; SMITH, G. D; BOULTON, G. S et al.Journal of Glaciology. 1984, Vol 30, Num 105, pp 131-139, issn 0022-1430Article

Which are the most suitable Antarctic subglacial lakes for exploration ?SIEGERT, M.J.Polar geography (1995). 2002, Vol 26, Num 2, pp 134-146, issn 1088-937X, 13 p.Article

A review of the use of radio-echo sounding in glaciologyPLEWES, L.A; HUBBARD, B.Progress in physical geography. 2001, Vol 25, Num 2, pp 203-236, issn 0309-1333Article

Les données des carottes de glace de l'Antarctique: évolution du climat et de l'environnement atmosphérique depuis le dernier maximum glaciaireLORIUS, C.Cahiers du quaternaire. 1983, pp 37-49, issn 0246-5582, no h. sérArticle

Glacial ecology and glaciology of the last mid-latitudde ice sheets = Ecologie glaciaire et glaciologie des dernières calottes glaciaires de latitude moyenneBOULTON, G. S; SMITH, G. D; JONES, A. S et al.Journal of the Geological Society (London). 1985, Vol 142, Num 3, pp 447-474, issn 0016-7649Article

Ice-sheet modelling for climate studies = Modélisation de calotte glaciaire pour les études climatiquesOERLEMANS, J.Palaeoclimatic research and models. Workshop. 1983, pp 157-163Conference Paper

THE THEORY OF THERMAL CONVECTION IN POLAR ICE SHEETS.HUGHES TJ.1976; J. GLACIOL.; G.B.; DA. 1976; VOL. 16; NO 74; PP. 41-71; ABS. FR. ALLEM.; BIBL. 1 P. 1/2; (INT. SYMP. THERM. REGIME GLACIERS ICE SHEETS. PROC.; BURNABY; 1978)Conference Paper

Antarctic subglacial topography and ice-sheet evolutionSIEGERT, M.J.Earth surface processes and landforms. 2008, Vol 33, Num 4, pp 646-660, issn 0197-9337, 15 p.Article

Density profile of a 413.5 M deep fresh recovered at Mizuho Station, East AntarcticaNAKAWO, M; NARITA, H.Memoirs of National Institute of Polar Research. Special issue. 1985, Num 39, pp 141-156, issn 0386-0744Article

Evaluating the performance of cryospheric modelsVAN DER LEEN, C.J.Polar geography (1995). 1999, Vol 23, Num 2, pp 83-96, issn 1088-937XArticle

Les risques volcaniques et volcano-glaciaires dans les montagnes peuplées. Identification, cartographie, évaluationTHOURET, J.-C.Bulletin de l'Association de géographes français. 1990, Num 2, pp 133-148, issn 0004-5322Conference Paper

Creep buckling of ice shelves and the formation of pressure rollersCOLLINS, I. F; MCCRAE, I. R.Journal of Glaciology. 1985, Vol 31, Num 109, pp 242-252, issn 0022-1430Article

Quelques résultats d'études expérimentales des propriétés mécaniques de la calotte glaciaireEPIFANOV, V. P.Izvestiâ Akademii nauk SSSR. Mehanika tverdogo tela. 1985, Num 2, pp 182-191, issn 0572-3299Article

Caractéristiques topographiques avoisinnant la station Syowa déterminés par des mesures de gravité. Quelques conséquences sur la topographie du bedrock sous la calotte glaciaireNAGAO, T.Nankyoku Shiryo. 1984, Num 82, pp 20-29, issn 0085-7289Article

Cosmogenic Be 10-ages from the Store Koldewey island, NE GreenlandHÅKANSSON, L; GRAF, A; STRASKY, S et al.Geografiska annaler. Series A. Physical geography. 2007, Vol 89, Num 3, pp 195-202, issn 0435-3676, 8 p.Article

Maximální dosah kontinentálního zalednění na úpatí Ořešníku a Poledníku v severním svahu Jizerský hor = L'étendue maximale des calottes glaciaires continentales au pied de l'Orešnik et du Polednik sur le versant nord des montagnes Jizerské horyTRACZYK, A; ENGEL, Z.Geografie. Sbornik Ceské geografické spolecnosti. 2006, Vol 111, Num 2, pp 141-151, issn 1212-0014, 11 p.Article

Preservation of Arctic landscapes overriden by cold-based ice sheetsDAVIS, P.T; BRINER, J.P; COULTHARD, R.D et al.Quaternary research (Print). 2006, Vol 65, Num 1, pp 156-163, issn 0033-5894, 8 p.Article

Elevation change on the Greelnand ice sheet at Qamanarssup Sermina, West GreenlandTAURISANO, A; BOGGILD, C.E; SCHJOTH, F et al.Polar geography (1995). 2003, Vol 27, Num 1, pp 59-68, issn 1088-937X, 10 p.Article

the saturation of MANDSAT MSS detectors over large ice massesDOWDESWELL, J. A; MCINTYRE, N. F.International journal of remote sensing (Print). 1986, Vol 7, Num 1, pp 151-164, issn 0143-1161Article

If Martian ice caps flow: ablation mechanisms and appearanceFISHER, D. A.Icarus (New York, NY). 1993, Vol 105, Num 2, pp 501-511, issn 0019-1035Article

The reconstruction of former ice sheets and their mass balance characteristics using a non-lineary viscous flow modelBOULTON, G. S; SMITH, G. D; MORLAND, L. W et al.Journal of Glaciology. 1984, Vol 30, Num 105, pp 140-152, issn 0022-1430Article