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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>8</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-13479-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/13479/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/13479/2008/acpd-8-13479-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/13479/2008/acpd-8-13479-2008.pdf</fulltext_pdf>
	<start_page>13479</start_page>
	<end_page>13505</end_page>
	<publication_date>2008-07-15</publication_date>
	<article_title content_type="html">Total and partial cloud amount detection during summermonths 2005 at  Westerland (Sylt, Germany)</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>N. H. Schade</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. Macke</name>
			<email>amacke@ifm-geomar.de</email>
		</author>
		<author numeration="3" affiliations="1">
			<name>H. Sandmann</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>C. Stick</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institut fÃ¼r Medizinische Klimatologie, Hermann-Rodewald-Str. 5, 24098 Kiel, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Leibniz-Institut fÃ¼r Meereswissenschaften, DÃ¼sternbrooker Weg 20, 24105 Kiel, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The detection of cloudiness is investigated by means of partial and total
cloud amount estimations from pyrgeometer radiation measurements and all-sky
imager observations. The measurements have been performed in Westerland, a
seaside resort on the North Sea island of Sylt, Germany, during summer 2005.
&lt;br&gt;&lt;br&gt;
An improvement to previous studies on this subject results from the fact that
for the first time partial cloud amount (PCA), defined as total cloud amounts
without high clouds, calculations from longwave downward radiation (LDR)
according to the APCADA-Algorithm (DÃ¼rr and Philipona, 2004) are
validated against both human observations from the German Weather Service DWD
at the nearby airport of Sylt and digital all-sky imaging.
&lt;br&gt;&lt;br&gt;
Differences between the resulting total cloud amounts (TCA&apos;s), defined as
total cloud amount for all-cloud situations, derived from the camera images
and from human observations are within &amp;plusmn;1 octa in 72% and within
&amp;plusmn;2 octa in 85% of the cases. Compared to human observations PCA
measurements according to APCADA underestimate the observed cloud cover in
47% of all cases and the differences are within &amp;plusmn;1 octa in 60% and
&amp;plusmn;2 octa in 74% of all cases. Since high cirrus clouds can not be
derived from LDR, separate comparisons for all cases without high clouds have
been performed showing an agreement within &amp;plusmn;1(2) octa in 73(90)% for
PCA and also for camera derived TCA. For this coastal mid-latitude site under
investigation we find similar though slightly smaller agreements to human
observations as reported in  DÃ¼rr and Philipona (2004). Though limited to
day-time the cloud cover retrievals from the sky imager are not much affected
by cirrus clouds and provide a more reliable cloud climatology for all-cloud
conditions than APCADA.</abstract>
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</article>

