<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.clim-past-discuss.net/inc/cpd/copernicus.dtd">
<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>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cpd-3-1-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/1/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/1/2007/cpd-3-1-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/1/2007/cpd-3-1-2007.pdf</fulltext_pdf>
	<start_page>1</start_page>
	<end_page>17</end_page>
	<publication_date>2007-01-10</publication_date>
	<article_title content_type="html">Climatic changes in the Urals over the past millennium. An analysis of geothermal and meteorological data</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. Yu. Demezhko</name>
			<email>ddem54@inbox.ru</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>I. V. Golovanova</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Geophysics UB RAS, Ekaterinburg, Russia</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Geology, URS RAS, Ufa, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">This investigation is based on a study of two paleoclimatic curves obtained
in the Urals (51&amp;ndash;59&amp;deg; N, 58&amp;ndash;61&amp;deg; E): i) a ground surface temperature
history (GSTH) reconstruction since 800 AD and ii) meteorological data for
the last 170 years. Temperature anomalies measured in 49 boreholes were used
for the GSTH reconstruction. It is shown that a traditional averaging of the
histories leads to the lowest estimates of amplitude of past temperature
fluctuations. The interval estimates method, accounting separately for the
rock&apos;s thermal diffusivity variations and the influence of a number of
non-climatic causes, was used for obtaining the average GSTH.
&lt;br&gt;&lt;br&gt;
Joint analysis of GSTH and meteorological data bring us to the following
conclusions. First, ground surface temperatures in the Medieval maximum
during 1100&amp;ndash;1200 was 0.38 K higher than the 20th century mean temperature
(1900&amp;ndash;1960). The Little Ice Age cooling was culminated in 1720 when surface
mean temperature was 1.58 K below than the 20th century mean temperature.
Secondly, contemporary warming began approximately one century prior to the
first instrumental measurements in the Urals. The rate of warming was
+0.25K/100years in the 18th century, +1.15 K/100years in the 19th and +0.75
K/100years in the first 80 years of the 20th. Finally, the mean rate of
temperature warming increased in final decades of 20th century. An analysis
of linear regression coefficients in running intervals of 11, 21 and 31
years, shows that there were periods of warming with almost the same rates
in the past, including the 19th century.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Bartlett, M. G. and Chapman D. S.: The timing, depth, and duration of snow events: implication for ground surface temperature histories recovered from boreholes, 1998 AGU Fall Meeteng abstracts, San Fr., F842, 1998. </reference>
		<reference numeration="2" content_type="text"> Beltrami, H. and Mareshal, J.-C.: Recent warming in eastern Canada inferred from geothermal measurements, Geophys. Res. Lett., 18, 4, 605&amp;ndash;608, 1991. </reference>
		<reference numeration="3" content_type="text"> Demezhko, D.Yu. and Shchapov, V.A.: 80 000 years ground surface temperature history inferred from the temperature-depth log measured in the superdeep hole SG-4 (the Urals, Russia), Global and Planetary Change, 29 (1&amp;ndash;2), 219&amp;ndash;230, 2001. </reference>
		<reference numeration="4" content_type="text"> Demezhko, D. Yu.: Geothermal method for palaeoclimate reconstructions (examples from the Urals, Russia), Ekaterinburg, UB RAS, 144 p., (in Russian), 2001. </reference>
		<reference numeration="5" content_type="text"> Demezhko, D. Yu., Utkin, V. I., Shchapov, V. A., and Golovanova, I. V.: Variations in the Earth&apos;s Surface Temperature in the Urals during the Last Millennium Based on Borehole Temperature Data, Doklady Earth Sciences, 403, 5, 764&amp;ndash;766, 2005. </reference>
		<reference numeration="6" content_type="text"> Hansen, J. and Lebedeff, S.: Global trends of measured Air surface temperature, J. Geophys. Res., 92, 13 345&amp;ndash;13 372, 1987. </reference>
		<reference numeration="7" content_type="text"> Klimenko, V. V., Klimanov, V.A.: Climate of the North Hemisphere in the Medieval Optimum. Doklady Akademii Nauk, 371, 4, 539&amp;ndash;543, (in Russian), 2000. </reference>
		<reference numeration="8" content_type="text"> Pollack, H. N., Demezhko, D. Yu., Duchkov, A. D., Golovanova, I. V., Huang, S., Shchapov, V. A., and Smerdon, J. E.: Surface temperature trends in Russia over the past five centuries reconstructed from borehole temperatures, J. Geoph. Res., 108(Â4), 2180, doi: 10. 1029/2002JB002154, 2003. </reference>
		<reference numeration="9" content_type="text"> Pollack, H. N. and Smerdon J. E.: Borehole climate reconstruction: Spatial structure and hemispheric averages, J. Geoph.Res., 109 D11106, doi:10. 1029/2003JD004163, 2004. </reference>
		<reference numeration="10" content_type="text"> Smerdon, J. E., Pollack, H. N., Cermak, V., Enz, J. W., Kresl, M., Safanda, J., and Wehmiller J. F.: Daily, seasonal, and annual relationships between air and subsurface temperatures, J. Geophys. Res., 111, D07101, doi:10.1029/2004JD005578, 2006. </reference>
		<reference numeration="11" content_type="text"> Tyson, P. D., Mason, S. J., Jones, M. Q. W., and Cooper, G. R. J.: Global warming and geothermal profiles: The surface rock-temperature response in South Africa, Geophys. Res. Lett., 25, 14, 2711&amp;ndash;2713, 1998. </reference>
	</references>
</article>

