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<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-4-1433-2010</doi>
	<article_url>http://www.the-cryosphere-discuss.net/4/1433/2010/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/4/1433/2010/tcd-4-1433-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/4/1433/2010/tcd-4-1433-2010.pdf</fulltext_pdf>
	<start_page>1433</start_page>
	<end_page>1448</end_page>
	<publication_date>2010-08-25</publication_date>
	<article_title content_type="html">Interplay between linear, dissipative and permanently critical mechanical processes in Arctic sea ice</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Chmel</name>
			<email>chmel@mail.ioffe.ru</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>V. Smirnov</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>A. Panov</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Ioffe Physico-Technical Institute, St.-Petersburg, Russia</affiliation>
		<affiliation numeration="2" content_type="html">Arctic and Antarctic Research Institute, St.-Petersburg, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">Mechanical processes in the Arctic ice pack result in fragmented sea
ice cover, the regular geometry of which could be described in main
features in terms of the conventional mechanics. However, the size
distribution of sea ice floes does not exhibit the random
(poissonian-like) statistics and follows the power law typical for
self-similar (fractal) structures. The analysis of ice floe
oscillations in the frequency range specific for cracking, shearing
and stick-slip motion evidences the self-organized dynamics of sea
ice fracturing, which manifests itself in scaling distributions of
both the discrete energy discharges in fracture events and the
recurrence times between that one. So determined space-time-energy
self-similarity characterises the ice pack as the non-equilibrium,
nonlinear thermodynamic system where the synergic relations are
established through conventional long propagating wave/oscillations.
The presented experimental data were collected at the Russian
ice-research camp &quot;North Pole 35&quot; drifting on the Arctic ice pack
in 2008.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Chmel,~A., Smirnov,~V N., and Astakhov,~A P.: The fractality of sea-ice drift dynamics as revealed from the \qutNorth Pole 32 monitoring, J. Stat. Mech., P02002, 1–11, 2005. </reference>
		<reference numeration="2" content_type="text"> Chmel, A., Smirnov, V. N., and Panov, L. V.: Scaling aspects of the sea-ice-drift dynamics and pack fracture, Ocean Sci., 3, 291–298, doi:10.5194/os-3-291-2007, 2007. </reference>
		<reference numeration="3" content_type="text"> Erlingsson,~B.: Two-dimensional deformation patterns in sea ice, J Glaciol., 34, 301–308, 1988. </reference>
		<reference numeration="4" content_type="text"> Marco,~J R. and Thompson,~R E.: Rectilinear leads and internal motions in the ice pack of the Western Arctic Ocean, J. Geophys. Res., 82, 979–987, 1977. </reference>
		<reference numeration="5" content_type="text"> Obukhov,~S P.: Self-organized criticality: Goldstone modes and their interactions, Phys. Rev. Lett., 65, 1395–1398, 1990. </reference>
		<reference numeration="6" content_type="text"> Rothrock,~D A. and Thorndike,~A S.: Measuring the sea-ice floe size distribution, J. Geophys. Res., 89, 6477–6486, 1984. </reference>
		<reference numeration="7" content_type="text"> Smirnov,~V N.: Dynamic processes in sea ice, Gidrometeoizdat, St Petersburg, Russia, 1996 (in Russian). </reference>
		<reference numeration="8" content_type="text"> Weiss J. and Marsan,~D.: Scale properties of sea ice deformation and fracturing, C. R. Physique, 735–751, 2004. </reference>
	</references>
</article>

