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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-4-1107-2010</doi>
	<article_url>http://www.the-cryosphere-discuss.net/4/1107/2010/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/4/1107/2010/tcd-4-1107-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/4/1107/2010/tcd-4-1107-2010.pdf</fulltext_pdf>
	<start_page>1107</start_page>
	<end_page>1150</end_page>
	<publication_date>2010-07-22</publication_date>
	<article_title content_type="html">Spatial and temporal variability in summer snow pack in the Dronning Maud Land, Antarctica</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>T. Vihma</name>
			<email>timo.vihma@fmi.fi</email>
		</author>
		<author numeration="2" affiliations="2,3">
			<name>O.-P. Mattila</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>R. Pirazzini</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>M. M. Johansson</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, Finland</affiliation>
		<affiliation numeration="2" content_type="html">Department of Physics, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland</affiliation>
		<affiliation numeration="3" content_type="html">now at: Finnish Environmental Institute, P.O. Box 140, 00251 Helsinki, Finland</affiliation>
	</affiliations>
	<abstract content_type="html">Snow temperature, density, and layering were measured in four summers in the
Dronning Maud Land, Antarctica. Data from a 310-km-long transect showed that
the most homogeneous snow pack located in the Riiser-Larsen Ice Shelf, while
horizontal gradients in snow density, temperature, and hardness were larger
in the escarpment region. In the local scale, day-to-day temporal variability
dominated the standard deviation of snow temperature, while the diurnal cycle
was next important, and horizontal variability in the scale of 0.4 to 10 m
was the smallest component. The day-to-day and total small-scale variability
decreased exponentially with depth with an e-folding depth at 0.25 to
0.30 m. Snow temperature depended on the cloud cover in the uppermost
0.30 m and snow density in the uppermost 0.10 m. Both in the intra-pit and
transect scales, the ratio of horizontal to temporal variability increased
with depth. In the intra-pit scale the temporal variability in snow density
exceeded the horizontal variability throughout the uppermost 0.50 m layer,
but in the 100-km scale only in the uppermost centimetres. The horizontal
standard deviation of snow density increased rapidly between the scales of
0.4 and 2 m, and much more gradually from 10&lt;sup&gt;1&lt;/sup&gt; to 10&lt;sup&gt;2&lt;/sup&gt; m.</abstract>
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