<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.the-cryosphere-discuss.net/inc/tcd/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>The Cryosphere Discussions</journal_title>
		<journal_url>www.the-cryosphere-discuss.net</journal_url>
		<issn>1994-0432</issn>
		<eissn>1994-0440</eissn>
		<volume_number>4</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/tcd-4-1035-2010</doi>
	<article_url>http://www.the-cryosphere-discuss.net/4/1035/2010/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/4/1035/2010/tcd-4-1035-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/4/1035/2010/tcd-4-1035-2010.pdf</fulltext_pdf>
	<start_page>1035</start_page>
	<end_page>1061</end_page>
	<publication_date>2010-07-19</publication_date>
	<article_title content_type="html">Rapid changes of the ice mass configuration in the dynamic Diablotins ice cave – Fribourg Prealps, Switzerland</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. Morard</name>
			<email>sebastien.morard@unifr.ch</email>
		</author>
		<author numeration="2" affiliations="2,3">
			<name>M. Bochud</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>R. Delaloye</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Geography Unit, Department of Geosciences, University of Fribourg, Fribourg, Switzerland</affiliation>
		<affiliation numeration="2" content_type="html">Geology Unit, Department of Geosciences, University of Fribourg, Fribourg, Switzerland</affiliation>
		<affiliation numeration="3" content_type="html">Spéléo-Club des Préalpes Fribourgeoises (SCPF), Fribourg, Switzerland</affiliation>
	</affiliations>
	<abstract content_type="html">The Gouffre des Diablotins is a deep cave system located in the Swiss
Prealps. In 1991, the entrance zone of the cave was almost free of ice.
Nevertheless ice volume sharply increased in 1994, plugging almost totally
the gallery from the lower entrance. The ice cave have also experience
flooded period between 1996 and 2007, and very heterogeneous ice surface
morphology and textures have formed. Continuous cave climate measurements
initiated in 2009 showed the predominant role of winter atmospheric air
conditions to drive both the efficiency of chimney-effect circulation and
seasonal modifications of the ice mass. Main part of the ice loss is
currently due to sublimation in wintertime.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Arenson, L. U. and Sego, D. C.: Considering convective air fluxes in the design of engineered structures in cold regions, See to Sky Geotechnique, 1033–1040, 2006. </reference>
		<reference numeration="2" content_type="text"> Atkinson, T. C., Smart, P. L., and Wigley, T. M. L.: Climate and natural radon levels in Castleguard cave, Columbia icefields, Alberta, Canada, Arctic Alpine Res., 15/4, 487–502, 1983. </reference>
		<reference numeration="3" content_type="text"> Bella, P.: Morphology of ice surface in the Dobsina ice cave, in: Proceedings of the 2nd~International Workshop on Ice caves, 8–12~May~2006, Demanovska Dolina, Slovak Republic, 15–23, 2006. </reference>
		<reference numeration="4" content_type="text"> Bovey, M.: Gouffre des Diablotins, in Akten des 10. Nationalen Kongresses für Höhlenforschung, Breitenbach, Switzerland, 170–172, 1995. </reference>
		<reference numeration="5" content_type="text"> Delaloye, R., Reynard, E., Lambiel, C., Marescot, L., Monnet, R.: Thermal anomaly in a cold scree slope (Creux-du-Van, Switzerland), in: Proceedings of the 8th~International Conference on Permafrost, 21–25~July~2003, Zürich, Switzerland, 175–180, 2003. </reference>
		<reference numeration="6" content_type="text"> Forbes, J.: Air temperature and relative humidity study: Torgac cave, New Mexico, J. Cave and Karst Stud., 60/1, 27–32, 1998. </reference>
		<reference numeration="7" content_type="text"> Ford, D. C. and Williams, P. W.: Karst geomorphology and hydrology, Chapman &amp; Hall, London, 1989. </reference>
		<reference numeration="8" content_type="text"> Jutzet, J. M.: Brèves nouvelles: Gouffre~B15 aux Morteys (Préalpes fribourgeoises), Stalactite, Société Suisse de Spéléologie, 41/2, 99, 1991. </reference>
		<reference numeration="9" content_type="text"> Lauriol, B., Carrier, L., and Thibaudeau, P.: Topoclimatic zones and ice dynamics in the caves of the northern Yukon, Canada, Arctic, 41/3, 215–220, 1988. </reference>
		<reference numeration="10" content_type="text"> Lauriol, B. and Clark, I. D.: An approach to determine the origin and age of massive ice blockages in two arctic caves, Permafrost Periglac., 4, 77–85, 1993. </reference>
		<reference numeration="11" content_type="text"> Lauriol, B., Prévost, C., and Lacelle, D.: The distribution of diatoma flora in ice caves of the northern Yukon Territory, Canada: relationship to air circulation and freezing, Int. J. Speleol., 35/2, 83–92, 2006. </reference>
		<reference numeration="12" content_type="text"> Law, J. and van Dijk, D.: Sublimation as a geomorphic process: a review, Permafrost Periglac., 5, 237–249, 1994. </reference>
		<reference numeration="13" content_type="text"> Lismonde, B.: Mesure de la propagation d&apos;une perturbation de pression au Trou qui Souffle (Méaudre, Isère), Kartologia, 22/2, 43–47, 1993. </reference>
		<reference numeration="14" content_type="text"> Lismonde, B.: L&apos;âne de Buridan, le principe de Curie et l&apos;effet de cheminée: courants d&apos;air dans les cavités en forme de U, Karstologia, 37/1, 23–28, 2001. </reference>
		<reference numeration="15" content_type="text"> Lismonde, B.: Climatologie du monde souterrain: Vents des ténèbres, Edition du Comité Départemental de Spéléologie de Isère, Tome~1, 2002a. </reference>
		<reference numeration="16" content_type="text"> Lismonde, B.: Climatologie du monde souterrain: Aérologie des systèmes karstiques, Edition du Comité Départemental de Spéléologie de Isère, Tome~2, 2002b. </reference>
		<reference numeration="17" content_type="text"> Luetscher, M., Jeannin P.Y., Haeberli, W.: Energy fluxes in an ice cave of sporadic permafrost in the Swiss Jura mountains – concept and first observational results, in: Proceedings of the 8~th International Conference on Permafrost, 21–25~July~2003, Zürich, Switzerland, 691–696, 2003. </reference>
		<reference numeration="18" content_type="text"> Luetscher, M.: Variations spatio-temporelles du volume de glace à la Glacière de Monlési (Boveresse/NE), Cavernes, 2, 3–7, 2004. </reference>
		<reference numeration="19" content_type="text"> Luetscher, M. and Jeannin, P. Y.: Temperature distribution in karst systems: the role of air and water fluxes, Speleogenesis and Vvolution of Karst Aquifers, 16, 344–350, 2004a. </reference>
		<reference numeration="20" content_type="text"> Luetscher, M. and Jeannin, P. Y.: A process-based classification of alpine ice caves, Theor. Appl. Karstol., 17, 5–10, 2004b. </reference>
		<reference numeration="21" content_type="text"> Luetscher, M.: Processes in ice caves and their significance for paleoenvironmental reconstructions, Ph.D thesis, Swiss Institute for Speleology and Karst Studies (SISKA), 51~pp., 2005. </reference>
		<reference numeration="22" content_type="text"> Luetscher, M., Jeannin P. Y., and Haeberli, W.: Ice caves as an indicator of winter climate evolution: a case study from the Jura Mountains, The Holocene, 15/7, 982–993, 2005. </reference>
		<reference numeration="23" content_type="text"> Morard, S., Delaloye, R., and Dorthe, J.: Seasonal thermal regime of a mid-latitude ventilated debris accumulation, in: Proceedings of the 9th~International Conference on Permafrost, 29~June–3~July~2008, Fairbanks, Alaska, 1233-1238, 2008. </reference>
		<reference numeration="24" content_type="text"> Ohata, T., Furukawa, T., and Higuchi, K.: Glacioclimatological study of perennial ice in the Fuji ice cave, Japan, Part~1, Seasonal variation and mechanism of maintenance, Arctic Alpine Res, 26/3, 227–237, 1994a. </reference>
		<reference numeration="25" content_type="text"> Ohata, T., Furukawa, T., and Osada, K.: Glacioclimatological study of perennial ice in the Fuji ice cave, Japan, Part~2, Interannual variation and relation to climate, Arctic Alpine Res, 26/3, 238–244, 1994b. </reference>
		<reference numeration="26" content_type="text"> Rachlewick, G. and Szczucinski, W.: Seasonal, annual and decadal ice mass balance changes in the ice cave Jaskinia Lodowa w Ciemniaku, the Tatra Mountains, Poland, Theor. Appl. Karstol., 17, 11–18, 2004. </reference>
		<reference numeration="27" content_type="text"> Saar, R.: Die Dachstein-Rieseneishöhle nächst Obertraun und ihre Funktion als dynamische Wetterhöhle, Jb d oö Musealsvereins, Linz, 263–319, 1955. </reference>
		<reference numeration="28" content_type="text"> SCPF: Spéléo-Club des Préalpes Fribourgeoises, http://www.scpf.info/, last access: 28~May~2010. </reference>
		<reference numeration="29" content_type="text"> Turri, S., Citterio, M., Bini, A., Maggi, V., Udisti, R., and Stenni, B.: Etude glaciologique et climatologique des cavités glacées du Moncodeno (Grigna septentrionale, province de Lecco, Lombardie), Kartologia, 42/2, 37–44, 2003. </reference>
	</references>
</article>

