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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>9</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/nhess-9-1541-2009</doi>
	<article_url>http://www.nat-hazards-earth-syst-sci.net/9/1541/2009/</article_url>
	<abstract_html>http://www.nat-hazards-earth-syst-sci.net/9/1541/2009/nhess-9-1541-2009.html</abstract_html>
	<fulltext_pdf>http://www.nat-hazards-earth-syst-sci.net/9/1541/2009/nhess-9-1541-2009.pdf</fulltext_pdf>
	<start_page>1541</start_page>
	<end_page>1549</end_page>
	<publication_date>2009-09-03</publication_date>
	<article_title content_type="html">Fog characteristics at the airport of Thessaloniki, Greece</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. N. Stolaki</name>
			<email>sstolaki@geo.auth.gr</email>
		</author>
		<author numeration="2" affiliations="2,3">
			<name>S. A. Kazadzis</name>
		</author>
		<author numeration="3" affiliations="4">
			<name>D. V. Foris</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>Th. S. Karacostas</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Meteorology and Climatology, School of Geology, A.U.Th., Greece</affiliation>
		<affiliation numeration="2" content_type="html">Finnish Meteorological Institute, Climate Change Unit, Finland</affiliation>
		<affiliation numeration="3" content_type="html">National Observatory of Athens, Institute for Environmental Research and Sustainable Development, Greece</affiliation>
		<affiliation numeration="4" content_type="html">Meteorological Applications Center, Greek Agricultural Insurance Organization, Greece</affiliation>
	</affiliations>
	<abstract content_type="html">A statistical approach in order to study fog event characteristics occuring
at the airport of Thessaloniki, Northern Greece is presented in this work.
To achieve this, the seasonal and diurnal characteristics of fog are
investigated using 35 years (1971–2005) of observations of meteorological
parameters such as: visibility, air temperature, dew point temperature, air
relative humidity, wind vector, precipitation, and cloud base height and
coverage. Hourly surface observations of fifteen (15) years (1991–2005) are
used to identify fog events induced by various physical mechanisms. Fog
events are classified into fog types through the application of objective
criteria that are derived upon fog formation processes and under the
influence of various physiographic features. The temporal variability of
different fog type occurrences are examined and the events are characterized
according to their duration and intensity.

&lt;br&gt;&lt;br&gt;
The results are somehow affected by regional and local factors. Fog is
mainly formed in winter time (~64%) with an enhanced likelihood to
appear also in late autumn (19%). The highest frequency of the fog events
occurs around sunrise or 1 to 2 h before of it. The mean duration of the
events is about 4.5 h. Most of them (75%) are dense (visibility &amp;lt;400 m). The overall fog phenomenon is a combination of various types, such
as: advection fog, radiation fog, cloud-base lowering fog and precipitation
fog. Advection fog (30%) and radiation fog (29%), which are the most
common types, occur predominantly in winter and early spring time. With
respect to the former type, it seems that, in many cases, already formed fog
is advected from the nearby &lt;i&gt;Anthemountas&lt;/i&gt; valley. Moreover, a considerable number of fog
events (22%) result from cloud-base lowering, and they frequently occur
in late autumn and mid winter.</abstract>
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</article>

