A Case Study of a Quasistationary, Very Long Polar Stratospheric Cloud Layer Edge
A case study of the occurrence of polar stratospheric clouds (PSCs) on February 13th, 2017, in northern Sweden is reported in this paper. For the first time, a quasistationary edge of a bright and extended PSC layer (∼ 600-km long) on the eastern side of the Scandinavian mountain range was photograp...
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Veröffentlicht in: | Journal of the Meteorological Society of Japan 2021, Vol.99(2), pp.497-504 |
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description | A case study of the occurrence of polar stratospheric clouds (PSCs) on February 13th, 2017, in northern Sweden is reported in this paper. For the first time, a quasistationary edge of a bright and extended PSC layer (∼ 600-km long) on the eastern side of the Scandinavian mountain range was photographed and registered using lidar observations. Both lidar measurements and model simulations demonstrated that atmospheric conditions were fairly unchanged for several hours during the presence of the PSC. Strong winds across the Scandinavian mountain range were responsible for triggering the formation of mountain lee waves in the Kiruna area, which induced the formation of the quasistationary long and straight edge of the PSCs. |
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Strong winds across the Scandinavian mountain range were responsible for triggering the formation of mountain lee waves in the Kiruna area, which induced the formation of the quasistationary long and straight edge of the PSCs.</description><subject>mountain gravity waves</subject><subject>polar stratospheric clouds</subject><subject>stratosphere</subject><subject>troposphere</subject><issn>0026-1165</issn><issn>2186-9057</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNo9kEtrwzAMgM3YYF234-7-AXPnR-zExxK6BwS2ssfV2IncJqRNsdND_v2StfQiIfRJSB9Cj4wuOJPsudnFZsEpZ4RyeYVmnGWKaCrTazSjlCvCmJK36C7GZiqTVM3QeolzGwF_9cdqwJ3HFq-PNtaxt33d7W0YnvAvhAEX3X6DP7vWhpENtu_iYQuhLnHedscKF3aAgFfVBu7RjbdthIdznqOfl9V3_kaKj9f3fFmQUijRE-cylmWpTKlWmYDSK1cJ6aWjIJ2gTDklWOJZAs6nqdMUlLWJpxXXlQaaijkip71l6GIM4M0h1LvxYMOomXyYyYeZfJjRx8jnJ74Zf9vAhbahr8sWTrTWhv-H89SlW25tMLAXf3O1a5Q</recordid><startdate>2021</startdate><enddate>2021</enddate><creator>VOELGER, Peter</creator><creator>DALIN, Peter</creator><general>Meteorological Society of Japan</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>2021</creationdate><title>A Case Study of a Quasistationary, Very Long Polar Stratospheric Cloud Layer Edge</title><author>VOELGER, Peter ; DALIN, Peter</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c363t-bb818875709683ecf6bd35f5b0e5b3016b6314f14ebf77b90e6aa4f0d29d9e073</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>mountain gravity waves</topic><topic>polar stratospheric clouds</topic><topic>stratosphere</topic><topic>troposphere</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>VOELGER, Peter</creatorcontrib><creatorcontrib>DALIN, Peter</creatorcontrib><collection>CrossRef</collection><jtitle>Journal of the Meteorological Society of Japan</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>VOELGER, Peter</au><au>DALIN, Peter</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A Case Study of a Quasistationary, Very Long Polar Stratospheric Cloud Layer Edge</atitle><jtitle>Journal of the Meteorological Society of Japan</jtitle><date>2021</date><risdate>2021</risdate><volume>99</volume><issue>2</issue><spage>497</spage><epage>504</epage><pages>497-504</pages><issn>0026-1165</issn><eissn>2186-9057</eissn><abstract>A case study of the occurrence of polar stratospheric clouds (PSCs) on February 13th, 2017, in northern Sweden is reported in this paper. For the first time, a quasistationary edge of a bright and extended PSC layer (∼ 600-km long) on the eastern side of the Scandinavian mountain range was photographed and registered using lidar observations. Both lidar measurements and model simulations demonstrated that atmospheric conditions were fairly unchanged for several hours during the presence of the PSC. Strong winds across the Scandinavian mountain range were responsible for triggering the formation of mountain lee waves in the Kiruna area, which induced the formation of the quasistationary long and straight edge of the PSCs.</abstract><pub>Meteorological Society of Japan</pub><doi>10.2151/jmsj.2021-025</doi><tpages>8</tpages><oa>free_for_read</oa></addata></record> |
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subjects | mountain gravity waves polar stratospheric clouds stratosphere troposphere |
title | A Case Study of a Quasistationary, Very Long Polar Stratospheric Cloud Layer Edge |
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