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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>7</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-9259-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/9259/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/9259/2007/acpd-7-9259-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/9259/2007/acpd-7-9259-2007.pdf</fulltext_pdf>
	<start_page>9259</start_page>
	<end_page>9281</end_page>
	<publication_date>2007-06-29</publication_date>
	<article_title content_type="html">Sand/dust storms over Northeast Asia and associated large-scale circulations in spring 2006</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Y. Q. Yang</name>
			<email>yangyq@cma.gov.cn</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>Q. Hou</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>C. H. Zhou</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>H. L. Liu</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>Y. Q. Wang</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>T. Niu</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Centre for Atmosphere Watch {&amp;} Services (CAWAS), Chinese Academy of Meteorological Sciences, China Meteorological Administration (CMA), Beijing 100081, China</affiliation>
	</affiliations>
	<abstract content_type="html">This paper presents a study on the meteorological conditions that accompany
the sand/dust storms (SDS) of East Asia in spring 2006, based on the SDS
data collected both by WMO during 2000&amp;ndash;2006 and by 2456 Chinese surface
stations, and on the meteorological reanalysis data from NCEP-NCAR . The
evolution of 3-D structures of the general circulations prevailed in both
winter and spring as well as their annual anomalies were investigated by
comparing the years having most and least occurrences of SDS between 2000
and 2006. It is found that spring 2006 featured a noticeably increased
occurrence of SDS, compared with previous years. The general circulations
prevailed through both winter and spring, especially the 3-D structure of
the polar circulation, show the significant anomalies compared to a normal
year. This produced a range of corresponding weather phenomena, including
circumpolar vortices at the upper troposphere, mid-level westerly jets, and
lower zonal winds, which all favored the SDS production and transport in
2006. The study also reveals a fact that comparing with a normal year, the
transitional period from the winter of 2005 to the spring of 2006 has
witnessed a fast-developed high center at the upper troposphere of the
northern hemisphere and the circumpolar vortex area, which pushes the area
dominated by the circumpolar vortices further to mid-latitudes. The
circumpolar vortices shifted southwards, and prevailed over an extensive
area across the northeast hemisphere for a sustained period. The mid-high
latitude areas that sit in the south of the circumpolar vortices in Asia
have experienced significantly abnormal westerly jets at the mid-level of
troposphere. Zonal winds prevailed at the mid and lower levels of
troposphere. Sea level pressure registered an abnormal high at 4&amp;ndash;10 hPa,
compared with a normal year. The above-mentioned 3-D structures of general
circulation have created thermal and dynamic conditions that favor the
repeated genesis and momentous development of the Mongolian cyclones, which
in turn contributes to the frequent occurrences and long distance transport
of SDS.</abstract>
	<references>
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</article>

