On Spatiotemporal Characteristics of Sea Fog Occurrence over the Northern Atlantic from 1909 to 2008
In this paper, the International Comprehensive Ocean and Atmosphere Data Set （ICOADS） is utilized to investigate the horizontal distribution of sea fog occurrence frequency over the Northern Atlantic as well as the meteorological and oceanic condi- tions for sea fog formation. Sea fog over the North...
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| Veröffentlicht in: | Journal of Ocean University of China 2016-12, Vol.15 (6), p.958-966 |
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| description | In this paper, the International Comprehensive Ocean and Atmosphere Data Set （ICOADS） is utilized to investigate the horizontal distribution of sea fog occurrence frequency over the Northern Atlantic as well as the meteorological and oceanic condi- tions for sea fog formation. Sea fog over the Northern Atlantic mainly occurs over middle and high latitudes. Sea fog occurrence frequency over the western region of the Northern Atlantic is higher than that over the eastern region. The season for sea fog occur- rence over the Northern Atlantic is generally from April to August. When sea fogs occur, the prevailing wind direction in the study area is from southerly to southwesterly and the favorable wind speed is around 8 m s-1, It is most favorable for the formation of sea fogs when sea surface temperature （SST） is 5℃ to 15℃. When SST is higher than 25℃, it is difficult for the air to get saturated, and there is almost no report of sea fog. When sea fogs form, the difference between sea surface temperature and air temperature is mainly -1 to 3℃, and the difference of 0℃ to 2℃ is the most favorable conditions for fog formation. There are two types of sea fogs prevailing in this region： advection cooling fog and advection evaporating fog. |
| doi_str_mv | 10.1007/s11802-016-3077-7 |
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Sea fog over the Northern Atlantic mainly occurs over middle and high latitudes. Sea fog occurrence frequency over the western region of the Northern Atlantic is higher than that over the eastern region. The season for sea fog occur- rence over the Northern Atlantic is generally from April to August. When sea fogs occur, the prevailing wind direction in the study area is from southerly to southwesterly and the favorable wind speed is around 8 m s-1, It is most favorable for the formation of sea fogs when sea surface temperature （SST） is 5℃ to 15℃. When SST is higher than 25℃, it is difficult for the air to get saturated, and there is almost no report of sea fog. When sea fogs form, the difference between sea surface temperature and air temperature is mainly -1 to 3℃, and the difference of 0℃ to 2℃ is the most favorable conditions for fog formation. There are two types of sea fogs prevailing in this region： advection cooling fog and advection evaporating fog.</description><identifier>ISSN: 1672-5182</identifier><identifier>EISSN: 1993-5021</identifier><identifier>EISSN: 1672-5174</identifier><identifier>DOI: 10.1007/s11802-016-3077-7</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Advection ; Air temperature ; Earth and Environmental Science ; Earth Sciences ; Fog ; Gases ; Marine ; Meteorology ; Oceanic analysis ; Oceanography ; Sea surface temperature ; Wind speed ; 中高纬度地区 ; 北大西洋 ; 发生频率 ; 时空特征 ; 海洋表面温度 ; 海表面温度 ; 海雾 ; 空气温度</subject><ispartof>Journal of Ocean University of China, 2016-12, Vol.15 (6), p.958-966</ispartof><rights>Science Press, Ocean University of China and Springer-Verlag Berlin Heidelberg 2016</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c412t-68a29859f3273f398e13f5ec34fdca20c4e8d839f9cc88c78cf0366583cbb433</citedby><cites>FETCH-LOGICAL-c412t-68a29859f3273f398e13f5ec34fdca20c4e8d839f9cc88c78cf0366583cbb433</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/87473A/87473A.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11802-016-3077-7$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11802-016-3077-7$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,778,782,27911,27912,41475,42544,51306</link.rule.ids></links><search><creatorcontrib>Li, Pengyuan</creatorcontrib><creatorcontrib>Wang, Guanlan</creatorcontrib><creatorcontrib>Fu, Gang</creatorcontrib><creatorcontrib>Lu, Chungu</creatorcontrib><title>On Spatiotemporal Characteristics of Sea Fog Occurrence over the Northern Atlantic from 1909 to 2008</title><title>Journal of Ocean University of China</title><addtitle>J. Ocean Univ. China</addtitle><addtitle>Journal of Ocean University of China</addtitle><description>In this paper, the International Comprehensive Ocean and Atmosphere Data Set （ICOADS） is utilized to investigate the horizontal distribution of sea fog occurrence frequency over the Northern Atlantic as well as the meteorological and oceanic condi- tions for sea fog formation. Sea fog over the Northern Atlantic mainly occurs over middle and high latitudes. Sea fog occurrence frequency over the western region of the Northern Atlantic is higher than that over the eastern region. The season for sea fog occur- rence over the Northern Atlantic is generally from April to August. When sea fogs occur, the prevailing wind direction in the study area is from southerly to southwesterly and the favorable wind speed is around 8 m s-1, It is most favorable for the formation of sea fogs when sea surface temperature （SST） is 5℃ to 15℃. When SST is higher than 25℃, it is difficult for the air to get saturated, and there is almost no report of sea fog. When sea fogs form, the difference between sea surface temperature and air temperature is mainly -1 to 3℃, and the difference of 0℃ to 2℃ is the most favorable conditions for fog formation. There are two types of sea fogs prevailing in this region： advection cooling fog and advection evaporating fog.</description><subject>Advection</subject><subject>Air temperature</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Fog</subject><subject>Gases</subject><subject>Marine</subject><subject>Meteorology</subject><subject>Oceanic analysis</subject><subject>Oceanography</subject><subject>Sea surface temperature</subject><subject>Wind speed</subject><subject>中高纬度地区</subject><subject>北大西洋</subject><subject>发生频率</subject><subject>时空特征</subject><subject>海洋表面温度</subject><subject>海表面温度</subject><subject>海雾</subject><subject>空气温度</subject><issn>1672-5182</issn><issn>1993-5021</issn><issn>1672-5174</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kUtrGzEUhUVoIanbH9CdSDaFMq0eo9cymKQthHqR7IWsubIn2JItyXn8-8hMCKGLrq4W3zlH9x6EvlLygxKifhZKNWEdobLjRKlOnaAzagzvBGH0Q3tLxTpBNTtFn0q5J0RwIdUZGhYR3-5cHVOF7S5lt8HztcvOV8hjqaMvOAV8Cw5fpxVeeH_IGaIHnB4g47oG_DflNnLEl3XjYlPgkNMWU0MMrgkzQvRn9DG4TYEvr3OG7q6v7ua_u5vFrz_zy5vO95TVTmrHjBYmcKZ44EYD5UGA530YvGPE96AHzU0w3mvtlfaBcCmF5n657Dmfoe-T7aOLwcWVvU-HHFug3Q_r5-HpaWmBtQsReVx_hr5N9C6n_QFKtduxeNi0JSAdiqVaayNkL1hDL_5B35yp5qrdvxeqUXSifE6lZAh2l8ety8-WEnssyU4l2fYFeyzJHjVs0pTGxhXkd87_EZ2_Bq1TXO2b7i1JKmKUlIzxFzgpnYA</recordid><startdate>20161201</startdate><enddate>20161201</enddate><creator>Li, Pengyuan</creator><creator>Wang, Guanlan</creator><creator>Fu, Gang</creator><creator>Lu, Chungu</creator><general>Science Press</general><general>Springer Nature B.V</general><general>Laboratory of Physical 0ceanography,0cean-Atmosphere Interaction and Climate,Department of Marine Meteorology,0cean University of China,Qingdao 266100,P. 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China%National Science Foundation,Arlington,VA 22230,USA</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7T7</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H95</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>P64</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20161201</creationdate><title>On Spatiotemporal Characteristics of Sea Fog Occurrence over the Northern Atlantic from 1909 to 2008</title><author>Li, Pengyuan ; Wang, Guanlan ; Fu, Gang ; Lu, Chungu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c412t-68a29859f3273f398e13f5ec34fdca20c4e8d839f9cc88c78cf0366583cbb433</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Advection</topic><topic>Air temperature</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Fog</topic><topic>Gases</topic><topic>Marine</topic><topic>Meteorology</topic><topic>Oceanic analysis</topic><topic>Oceanography</topic><topic>Sea surface temperature</topic><topic>Wind speed</topic><topic>中高纬度地区</topic><topic>北大西洋</topic><topic>发生频率</topic><topic>时空特征</topic><topic>海洋表面温度</topic><topic>海表面温度</topic><topic>海雾</topic><topic>空气温度</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Li, Pengyuan</creatorcontrib><creatorcontrib>Wang, Guanlan</creatorcontrib><creatorcontrib>Fu, Gang</creatorcontrib><creatorcontrib>Lu, Chungu</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Journal of Ocean University of China</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Li, Pengyuan</au><au>Wang, Guanlan</au><au>Fu, Gang</au><au>Lu, Chungu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>On Spatiotemporal Characteristics of Sea Fog Occurrence over the Northern Atlantic from 1909 to 2008</atitle><jtitle>Journal of Ocean University of China</jtitle><stitle>J. Ocean Univ. China</stitle><addtitle>Journal of Ocean University of China</addtitle><date>2016-12-01</date><risdate>2016</risdate><volume>15</volume><issue>6</issue><spage>958</spage><epage>966</epage><pages>958-966</pages><issn>1672-5182</issn><eissn>1993-5021</eissn><eissn>1672-5174</eissn><abstract>In this paper, the International Comprehensive Ocean and Atmosphere Data Set （ICOADS） is utilized to investigate the horizontal distribution of sea fog occurrence frequency over the Northern Atlantic as well as the meteorological and oceanic condi- tions for sea fog formation. Sea fog over the Northern Atlantic mainly occurs over middle and high latitudes. Sea fog occurrence frequency over the western region of the Northern Atlantic is higher than that over the eastern region. The season for sea fog occur- rence over the Northern Atlantic is generally from April to August. When sea fogs occur, the prevailing wind direction in the study area is from southerly to southwesterly and the favorable wind speed is around 8 m s-1, It is most favorable for the formation of sea fogs when sea surface temperature （SST） is 5℃ to 15℃. When SST is higher than 25℃, it is difficult for the air to get saturated, and there is almost no report of sea fog. When sea fogs form, the difference between sea surface temperature and air temperature is mainly -1 to 3℃, and the difference of 0℃ to 2℃ is the most favorable conditions for fog formation. There are two types of sea fogs prevailing in this region： advection cooling fog and advection evaporating fog.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s11802-016-3077-7</doi><tpages>9</tpages></addata></record> |
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| identifier | ISSN: 1672-5182 |
| ispartof | Journal of Ocean University of China, 2016-12, Vol.15 (6), p.958-966 |
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| source | Springer Nature - Complete Springer Journals; Alma/SFX Local Collection |
| subjects | Advection Air temperature Earth and Environmental Science Earth Sciences Fog Gases Marine Meteorology Oceanic analysis Oceanography Sea surface temperature Wind speed 中高纬度地区 北大西洋 发生频率 时空特征 海洋表面温度 海表面温度 海雾 空气温度 |
| title | On Spatiotemporal Characteristics of Sea Fog Occurrence over the Northern Atlantic from 1909 to 2008 |
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