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<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>3</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cpd-3-469-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/469/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/469/2007/cpd-3-469-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/469/2007/cpd-3-469-2007.pdf</fulltext_pdf>
	<start_page>469</start_page>
	<end_page>500</end_page>
	<publication_date>2007-03-08</publication_date>
	<article_title content_type="html">Thermal signal propagation in soils in Romania: conductive and non-conductive processes</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Demetrescu</name>
			<email>crisan@geodin.ro</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>D. Nitoiu</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>C. BoroneanÅ£</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>A. Marica</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>B. Lucaschi</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Geodynamics, Bucharest, Romania</affiliation>
		<affiliation numeration="2" content_type="html">National Meteorological Administration, Bucharest, Romania</affiliation>
	</affiliations>
	<abstract content_type="html">Temperature data recorded in 2002 and 2003 at 10 stations out of
the 70 of the Romanian automatic weather stations network are
presented and analyzed in terms of the heat transfer from air to
underground. The air temperature at 2 m, the soil
temperatures at 0, 5, 10, 20, 50 and 100 cm below soil
surface as well as precipitation and snow thickness have been
monitored. The selected locations sample various climate
environments in Romania. First order modelling confirm that at
certain locations and for certain time intervals soil temperatures
track air temperature variations and consequently the heat
transfer is by conduction, while at others, processes such as soil
freezing and/or solar radiation heating play an important part in
the heat flux balance at the air/soil interface. However, the
propagation of the annual thermal signal in the first meter of
soil is through conduction; the effective thermal diffusivity for
8 stations with continuous time series at all depth levels ranges
from 3 to 10&amp;times;10&lt;sup&gt;&amp;ndash;6&lt;/sup&gt;m&lt;sup&gt;2&lt;/sup&gt;s&lt;sup&gt;&amp;ndash;1&lt;/sup&gt;.</abstract>
	<references>
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</article>

