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<article language="en">
	<journal>
		<journal_title>Climate of the Past</journal_title>
		<journal_url>www.clim-past.net</journal_url>
		<issn>1814-9324</issn>
		<eissn>1814-9332</eissn>
		<volume_number>3</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cp-3-637-2007</doi>
	<article_url>http://www.clim-past.net/3/637/2007/</article_url>
	<abstract_html>http://www.clim-past.net/3/637/2007/cp-3-637-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past.net/3/637/2007/cp-3-637-2007.pdf</fulltext_pdf>
	<start_page>637</start_page>
	<end_page>645</end_page>
	<publication_date>2007-11-02</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. Boroneant</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 available in 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 the
surface as well as rain fall and snow cover thickness have been
monitored. The selected locations sample various climate
environments in Romania. Preliminary analytical modelling shows
that soil temperatures track air temperature variations at certain
locations and, consequently, the heat transfer is by conduction,
while at other stations 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 uppermost one meter of soil is mainly
by conduction; the inferred 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;minus;7&lt;/sup&gt; m&lt;sup&gt;2&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Bartlett, M. G., Chapman, D. S., and Harris, R. N.: Snow and the ground temperature record of climate change, J. Geophys. Res., 109, F04008, doi:10.1029/2004JF000224, 2004. </reference>
		<reference numeration="2" content_type="text"> Bartlett, M. G., Chapman, D. S., and Harris, R. N.: Snow effect on North American ground temperatures, 1950&amp;ndash;2002, J. Geophys. Res., 110, F03008, doi:10.1029/2005JF000293, 2005. </reference>
		<reference numeration="3" content_type="text"> Beltrami, H.: On the relationship between ground temperature histories and meteorological records: a report on the Pomquet station, Global Planet. Change, 29, 327&amp;ndash;349, 2001. </reference>
		<reference numeration="4" content_type="text"> Beltrami, H.: Climate from borehole data: Energy fluxes and temperatures since 1500, Geophys. Res. Lett., 29, 2111, doi:10.1029/2002GL015702, 2002. </reference>
		<reference numeration="5" content_type="text"> Beltrami, H. and Kellman, L.: An examination of short-and long-term air-ground temperature coupling, Global Planet. Change, 38, 291&amp;ndash;303, 2003. </reference>
		<reference numeration="6" content_type="text"> Boronean\ct, C., Ioni\ctÃ£, M., and Dumitrescu, A.: Trends and shifts in the seasonal temperature mean in Romania during the period 1961&amp;ndash;2000, International Workshop &quot;Significant Scientific Research on Global Environmental Change in Central and Eastern Europe&quot;, Sinaia, 6&amp;ndash;8 October, 2004. </reference>
		<reference numeration="7" content_type="text"> Briffa, K. R. and Osborn, T. J.: Blowing hot and cold, Science, 295, 2227&amp;ndash;2228, 2002. </reference>
		<reference numeration="8" content_type="text"> Carslaw, H. S. and Jaeger, J. C.: Conduction of Heat in Solids, 2nd ed., Oxford Univ. Press, New York, 1959. </reference>
		<reference numeration="9" content_type="text"> Chapman, D. S., Bartlett, M. G., and Harris, R. N.: Comment on &quot;Ground vs. surface air temperature trends: Implications for borehole surface temperature reconstructions&quot; by Mann M. E. and Schmidt G., Geophys. Res. Lett., 31, L07205, doi:10.1029/2003GL019054, 2004. </reference>
		<reference numeration="10" content_type="text"> Demetrescu, C., Nitoiu, D., Boronean\ct, C., Marica, A., and Lucaschi, B.: Preliminary analysis of two-year long records of air and underground temperatures as measured at automatic weather stations in Romania, Rev. Rom. Geophys., 50, 99&amp;ndash;106, 2006. </reference>
		<reference numeration="11" content_type="text"> Esper, J., Cook, E. R., and Schweingruber, F. H.: Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability, Science, 295, 2250&amp;ndash;2253, doi:10.1126/science.1066208, 2002. </reference>
		<reference numeration="12" content_type="text"> Esper, J., Frank, D. C., and Wilson, R. J. S.: Climate reconstructions: low-frequency ambition and high-frequency ratification, EOS, 85, 113, p. 120, 2004. </reference>
		<reference numeration="13" content_type="text"> GonzÃ¡lez-Rouco, J. F., von Storch, H., and Zorita, E.: Deep soil temperature as proxy for surface air-temperature in a coupled model simulation of the last thousand years, Geophys. Res. Lett., 30, 2116&amp;ndash;2119, 2003. </reference>
		<reference numeration="14" content_type="text"> GonzÃ¡lez-Rouco, J. F., Beltrami, H., Zorita, E., and von Storch, H.: Simulation and inversion of borehole temperature profiles in surrogate climates: Spatial distribution and surface coupling, Geophys. Res. Lett., 33, L01703, doi:10.1029/2005GL024693, 2006. </reference>
		<reference numeration="15" content_type="text"> Grundstein, A., Todhunter, P., and Mote, T.: Snowpack control over the thermal offset of air and soil temperatures in eastern North Dakota, Geophys, Res. Lett., 32, L08503, doi:10.1029/2005GL022532, 2005. </reference>
		<reference numeration="16" content_type="text"> Harris, R. and Chapman, D.: Geothermics and climate change 1.Analysis of borehole temperatures with emphasis on resolving power, J. Geophys. Res., 103(B4), 7363&amp;ndash;7360, 1998. </reference>
		<reference numeration="17" content_type="text"> Hegerl, G. C., Crowley, T. J., Allen, M., Hyde, W. T., Pollack, H. N., Smerdon, J. E., and Zorita, E.: Detection of human influence on a new, validated 1500-year temperature reconstruction, J. Climate, 20, 650&amp;ndash;666, 2007. </reference>
		<reference numeration="18" content_type="text"> Huang, S., Pollack, H. N., and Shen, P. Y.: Temperature trends over the last five centuries reconstructed from borehole temperatures, Nature, 403, 756&amp;ndash;758, 2000. </reference>
		<reference numeration="19" content_type="text"> Hurley, S. and Wiltshire, R. J.: Computing thermal diffusivity from soil temperature measurements, Computers and Geosciences, 19, 475&amp;ndash;477, 1993. </reference>
		<reference numeration="20" content_type="text"> Kane, D., Hinkel, K., Goering, D., Hinzman, L., and Outcalt, S.: Non-conductive heat transfer associated with frozen soils, Global Planet. Change, 29, 275&amp;ndash;292, 2001. </reference>
		<reference numeration="21" content_type="text"> Mann, M. E., Rutherford, S., Bradley, R. S., Hughes, M. K., and Keiming, F. T.: Optimal surface temperature reconstructions using terrestrial borehole data, J. Geophys. Res., 108(D7), 4203, doi:10.1029/2002JD002532, 2003. </reference>
		<reference numeration="22" content_type="text"> Mann, M. E. and Schmidt, G. A.: Ground vs. surface air temperature trends: Implications for borehole surface temperature reconstructions, Geophys. Res. Lett., 30, 1607, doi:10.1029/2003GL017170, 2003. </reference>
		<reference numeration="23" content_type="text"> McIntyre, S. and McKitrick, R.: Hockey sticks, principal components, and spurious significance, Geophys. Res. Lett., 32, L03710, doi:10.1029/2004GL021750, 2005. </reference>
		<reference numeration="24" content_type="text"> Nitoiu, D. and Beltrami, H.: Subsurface thermal effects of land use changes, J. Geophys. Res., 110, F01005, doi:10.1029/2004JF000151, 2005. </reference>
		<reference numeration="25" content_type="text"> Nitoiu, D.: Ground surface temperature history reconstruction from geothermal data and the influence of land disruptions on the subsurface temperature profiles, MSc Thesis, St. Francis Xavier University, 2005. </reference>
		<reference numeration="26" content_type="text"> Oke, T. R.: Boundary Layer Climates, Second Edition, Cambridge University Press, 1987. </reference>
		<reference numeration="27" content_type="text"> Pollack, H. N. and Smerdon, J. E.: Borehole climate reconstructions: Spatial structure and hemispheric averages, J. Geophys. Res., 109, D11106, doi:10.1029/2003JD004163, 2004. </reference>
		<reference numeration="28" content_type="text"> Pollack, H. N., Smerdon, J. E., and van Keken, P. E.: Variable seasonal coupling between air and ground temperatures: A simple representation in terms of subsurface thermal diffusivity, Geophys. Res. Lett., 32, L15405, doi:10.1029/2005GL023869, 2005. </reference>
		<reference numeration="29" content_type="text"> Putnam, S. N. and Chapman, D. S.: A geothermal climate change observatory: First year results from Emigrant Pass in northwest Utah, J. Geophys. Res., 101, 21 877&amp;ndash;21 890, 1996. </reference>
		<reference numeration="30" content_type="text"> Romanovsky, V. E. and Osterkamp, T. E.: Effects of unfrozen water on heat and mass transport processes in the active layer and permafrost, Permafrost Periglac. Process., 11, 219&amp;ndash;239, 2000. </reference>
		<reference numeration="31" content_type="text"> Schmidt, W. L., Gosnold, W. D., and Enz, J. W.: A decade of air–ground temperature exchange from Fargo, North Dakota, Global Planet. Change, 29, 311-325, 2001. </reference>
		<reference numeration="32" content_type="text"> Smerdon, J. E., Pollack, H. N., Enz, J. W., and Lewis, M. J.: Conduction dominated heat transport of the annual temperature signal in soil, J. Geophys. Res., 108(B9), 2431, doi:10.1029/2002JB002351, 2003. </reference>
		<reference numeration="33" content_type="text"> Smerdon, J. E., Pollack, H. N., Cermak, V., Enz, J. W., Kresl, M., Safanda, J., and Wehmiller, J. F.: Air-ground temperature coupling and subsurface propagation of annual temperature signals, J. Geophys. Res., 109, D21107, doi:10.1029/2004JD005056, 2004. </reference>
		<reference numeration="34" 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.-Atmos., 111, D07191, doi:10.1029/2004JD005578, 2006. </reference>
		<reference numeration="35" content_type="text"> Sokratov, S. A. and Barry, R. G.: Intraseasonal variation in the thermoinsulation effect of snow cover on soil temperature and energy balance, J. Geophys. Res., 107(D10), doi:10.1029/2001JD000489, 2002. </reference>
		<reference numeration="36" content_type="text"> Stevens, M. B., GonzÃ¡lez-Rouco, J. F., and Beltrami, H.: North American climate of the last millennium: Underground temperatures and model comparison, J. Geophys. Res., 2006JF000705, in press, 2007. </reference>
		<reference numeration="37" content_type="text"> Stieglitz, M., Dery, S. J., Romanovsky, V. E., and Osterkamp, T. E.: The role of snow cover in the warming of arctic permafrost, Geophys. Res. Lett., 30, 1721, doi:10.1029/2003GL017337, 2003. </reference>
		<reference numeration="38" content_type="text"> &amp;#x015E;erban, D., Nielsen , S., and Demetrescu, C.: Long wavelength ground surface temperature history from continuous temperature logs in the Transylvanian Basin, Global Planet. Change, 29, 201&amp;ndash;217, 2001. </reference>
		<reference numeration="39" content_type="text"> Trenberth, K. E. and Shea, D. J.: Relationships between precipitation and surface temperature, Geophys. Res. Lett., 32, L14703, doi:10.1029/2005GL022760, 2005. </reference>
		<reference numeration="40" content_type="text"> \cT\^i\cstea, D., DincÄƒ, I., Cazacu, G., S\^irbu, V., CÄƒlinescu, N., Neamu, G., and Teodoreanu, E.: Air temperature map, in Atlas Republica SocialistÄƒ RomÃ¢nia, Romanian Academy Publishing House, 1979. </reference>
		<reference numeration="41" content_type="text"> Yoshikawa, K., Bolton, W. R., Romanovsky, V. E., Fukunda, M., and Hinzman, L. D.: Impacts of wildfire on the permafrost in the boreal forests of Interior Alaska, J. Geophys. Res., 108, 8148, doi:10.1029/2001JD000438, 2003. </reference>
	</references>
</article>

