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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-3-631-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/631/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/631/2007/cpd-3-631-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/631/2007/cpd-3-631-2007.pdf</fulltext_pdf>
	<start_page>631</start_page>
	<end_page>653</end_page>
	<publication_date>2007-03-20</publication_date>
	<article_title content_type="html">Repeated temperature logs from the sites of the Czech, Slovenian and Portuguese borehole climate stations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. Šafanda</name>
			<email>jsa@ig.cas.cz</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>D. Rajver</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>A. Correia</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>P. Dědeček</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Geophysical Institute Prague, Bo&amp;#x010D;ní II/1401, 141 31 Praha, Czech Republic</affiliation>
		<affiliation numeration="2" content_type="html">Geological Survey of Slovenia, Dimi&amp;#x010D;eva 14, Ljubljana, Slovenia</affiliation>
		<affiliation numeration="3" content_type="html">Department of Physics, University of Evora, 7000 Evora, Portugal</affiliation>
	</affiliations>
	<abstract content_type="html">Two borehole climate stations were established in Slovenia and Portugal
within a joint Czech-Slovenian-Portuguese project in the years 2003&amp;ndash;2005.
They completed the older Czech station, which has been operating since the
year 1994. We report here on the repeated temperature logs carried out
within 6 boreholes at the sites of the stations and their surroundings
within a time span of 8&amp;ndash;20 years (1985&amp;ndash;2005). The repeated logs
revealed subsurface warming in all the boreholes amounting to 0.2&amp;ndash;0.6&amp;deg;C below the depth of the annual run at 20 m. The depth of the Czech
borehole (140 m) and the Portuguese borehole (180 m) was sufficient enough
for a reconstruction of the ground surface temperature (GST) history of the
last 150&amp;ndash;200 years and their comparison with the surface air temperature
(SAT) series measured in Prague (since 1771) and Lisbon (1856),
respectively. The reconstructed histories reproduce reasonably well the
amplitude of the recent warming, 1&amp;ndash;1.5&amp;deg;C above the long-term mean.
The depth of all four Slovenian boreholes, 100 m, did not allow the
inversion, but it was possible to apply it to a deep borehole 5 km apart
from the Slovenian station. The obtained GST history was compared with SAT
series from Ljubljana (since 1851). Alternatively, a compatibility of the
observed temporal changes of subsurface temperature with surface air
temperature series measured in Prague, Ljubljana and Lisbon was checked by
comparing differences of the repeated logs with the synthetic ones. These
were calculated by using the SAT series as a forcing function at a surface
of transient geothermal models of the borehole sites. A degree of agreement
varies from very well to rather poor, probably depending on unaccounted site
specific factors, which are to be specified by a long-term temperature
monitoring at the established stations.</abstract>
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</article>

