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<article language="en">
	<journal>
		<journal_title>Natural Hazards and Earth System Science</journal_title>
		<journal_url>www.nat-hazards-earth-syst-sci.net</journal_url>
		<issn>1561-8633</issn>
		<eissn>1684-9981</eissn>
		<volume_number>7</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/nhess-7-41-2007</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/7/41/2007/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/7/41/2007/nhess-7-41-2007.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/7/41/2007/nhess-7-41-2007.pdf</fulltext_pdf>
	<start_page>41</start_page>
	<end_page>56</end_page>
	<publication_date>2007-01-15</publication_date>
	<article_title content_type="html">Analysis of the environments of seven Mediterranean tropical-like storms using an axisymmetric, nonhydrostatic, cloud resolving model</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Fita</name>
			<email>lluis.fita@uib.es</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>R. Romero</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>A. Luque</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>K. Emanuel</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>C. Ramis</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Grup de Meteorologia, Departament de F&amp;#x00ED;sica, Universitat de les Illes Balears, Palma de Mallorca, Spain</affiliation>
		<affiliation numeration="2" content_type="html">Program in Atmospheres, Oceans, and Climate, Massachusetts Institute of Technology, Cambridge, Massachusetts, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Tropical-like storms on the Mediterranean Sea are occasionally observed on satellite
images, often with a clear eye surrounded by an axysimmetric cloud structure.
These storms sometimes attain hurricane intensity and can severely affect
coastal lands. A deep, cut-off, cold-core low is usually observed at mid-upper
tropospheric levels in association with the development of these tropical-like
systems. In this study we attempt to apply some tools previously used in studies of
tropical hurricanes to characterise the environments in which seven known Mediterranean
events developed. In particular, an axisymmetric, nonhydrostatic, cloud resolving model is
applied to simulate the tropical-like storm genesis and evolution. Results are compared to
surface observations when landfall occurred and with satellite microwave derived wind
speed measurements over the sea. Finally, sensitivities of the numerical simulations to
different factors (e.g. sea surface temperature, vertical humidity profile and size of the
initial precursor of the storm) are examined.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Bister, M. and Emanuel, K A.: Dissipative Heating and Hurricane Intensity, Meteor. Atmos. Physics, 50, 2662&amp;ndash;2682, 1998. </reference>
		<reference numeration="2" content_type="text"> Campins, J., Genovés, A., Jansà, A., Guijarro, J A., and Ramis, C.: A catalogue and a classification of surface cyclones for the western Mediterranean, Int. J. Climatol., 20, 969&amp;ndash;984, 2000. </reference>
		<reference numeration="3" content_type="text"> Emanuel, K.: Tropical Cyclones, Annu. Rev. Earth. Planet. Sci., 31, 75&amp;ndash;104, 2003. </reference>
		<reference numeration="4" content_type="text"> Emanuel, K A.: An Air-Sea Interaction Theory for Tropical Cyclones. Part I: Steady-State Maintenance, J.Atmos. Sci., 43, 585&amp;ndash;604, 1986. </reference>
		<reference numeration="5" content_type="text"> Emanuel, K A.: Genesis and maintenance of &quot;Mediterranean hurricanes&quot;, Adv. in Geos., 2, 217&amp;ndash;220, 2005. </reference>
		<reference numeration="6" content_type="text"> Grell, G., Dudhia, J., and Stauffer, D.: A description of the fifth-generation Penn State/NCAR mesoscale model (MM5), NCAR Technical Note, NCAR/TN-398+STR, 117pp, 1994. </reference>
		<reference numeration="7" content_type="text"> Homar, V., Romero, R., Stensrud, D., Ramis, C., and Alonso, S.: Numerical diagnosis of a small, quasi-tropical cyclone over the western Mediterranean: Dynamical vs. boundary factors, Q. J. R. Meteorol. Soc., 129, 1469&amp;ndash;1490, 2003. </reference>
		<reference numeration="8" content_type="text"> Hoskins, B J., McIntyre, M E., and W., R A.: On the use and significance of isentropic potential vorticity maps, Q. J. R. Meteo. Soc., 111, 877&amp;ndash;946, 1985. </reference>
		<reference numeration="9" content_type="text"> Jordan, C L.: Mean Soundings for the West Indies Area, J. Meteor., 15, 91&amp;ndash;97, 1958. </reference>
		<reference numeration="10" content_type="text"> Lagouvardos, K., Kotroni, V., Nickovic, S., Jovic, D., and Kallos, G.: Observations and model simulations of a winter sub-synoptic vortex over the central Mediterranean, Meteorol. Appl., 6, 371&amp;ndash;383, 1999. </reference>
		<reference numeration="11" content_type="text"> Pytharoulis, I., Craig, G C., and Ballard, S P.: The hurricane-like Mediterranean cyclone of January 1995, Meteorol. Appl., 7, 261&amp;ndash;279, 2000. </reference>
		<reference numeration="12" content_type="text"> Rasmussen, E. and Zick, C.: A subsynoptic vortex over the Mediterranean with some resemblance to polar lows, Tellus A, 39, 408&amp;ndash;425, 1987. </reference>
		<reference numeration="13" content_type="text"> Reiter, E R.: Handbook for Forecasters in the Mediterranean: Weather Phenomena of the Mediterranean Basin, Environmental Prediction Research Facility, Naval Postgraduate School, Monterey, CA, 1975. </reference>
		<reference numeration="14" content_type="text"> Romero, R. and Emanuel, K.: Space-time probability density of Mediterranean hurricane genesis in the light of an empirical tropical index, 5a Assamble Hispano-Portuguesa de Geodesia y Geofisica, (Spanish), 4, 2006. </reference>
		<reference numeration="15" content_type="text"> Rotunno, R. and Emanuel, K.: An Air-Sea Interaction Theory for Tropical Cyclones. Part II: Evolutionary Study Using a Nonhydrostatic Axisymmetric Numerical Model, J. Atmos. Sci., 44, 542&amp;ndash;561, 1987. </reference>
		<reference numeration="16" content_type="text"> Thorpe, A J.: Synoptic scale disturbances with circular symmetry, Mon. Wea. Rev., 114, 1384&amp;ndash;1389, 1986. </reference>
		<reference numeration="17" content_type="text"> Tudur\&apos;\i E. and Ramis, C.: The Enviromments of Significant Convective Events in the Western Mediterranean, Weather and Forecasting, 12, 294&amp;ndash;306, 1997. </reference>
	</references>
</article>

