| http://dbpedia.org/ontology/abstract
|
熱帶對流層上部槽（英語：Tropical upper tropospheric trough，縮寫：TUTT）是一條位於熱帶高空（約200百帕面）的槽線，其可經由中緯度西風槽振幅延大而伸展到熱帶而成，亦可為高層反氣旋南側之高空東風倒槽。其將帶來強烈垂直风切变而影響熱帶氣旋或熱帶擾動的發展，但亦有情況是因帶來良好的高空輻散而助長熱帶氣旋的發展。在環境許可下，其會發展成擁有完整環流的高空冷心低壓，並有可能發展至地面而誘生出低層之熱帶擾動發展。
, A tropical upper tropospheric trough (TUTT … A tropical upper tropospheric trough (TUTT), also known as the mid-oceanic trough, is a trough situated in the upper-level (at about 200 hPa) tropics. Its formation is usually caused by the intrusion of energy and wind from the mid-latitudes into the tropics. It can also develop from the inverted trough adjacent to an upper level anticyclone. TUTTs are different from mid-latitude troughs in the sense that they are maintained by subsidence warming near the tropopause which balances radiational cooling. When strong, they can present a significant vertical wind shear to the tropics and subdue tropical cyclogenesis. When upper cold lows break off from their base, they tend to retrograde and force the development of, or enhance, surface troughs and tropical waves to their east. Under special circumstances, they can induce thunderstorm activity and lead to the formation of tropical cyclones.ead to the formation of tropical cyclones.
|
| http://dbpedia.org/ontology/wikiPageExternalLink
|
http://hkcoc.weather.com.hk/cycdict/key=hot.htm%238 +
, http://www.cs.uu.nl/wais/html/na-dir/meteorology/storms-faq/part1.html +
, https://books.google.com/books%3Fid=skfkXwAACAAJ%7Cyear=2010%7Cpublisher=La +
|
| http://dbpedia.org/ontology/wikiPageID
|
2474597
|
| http://dbpedia.org/ontology/wikiPageLength
|
5829
|
| http://dbpedia.org/ontology/wikiPageRevisionID
|
1031797543
|
| http://dbpedia.org/ontology/wikiPageWikiLink
|
http://dbpedia.org/resource/Tropical_cyclone +
, http://dbpedia.org/resource/Africa +
, http://dbpedia.org/resource/South_America +
, http://dbpedia.org/resource/Azores +
, http://dbpedia.org/resource/Southern_Hemisphere +
, http://dbpedia.org/resource/Wind_shear +
, http://dbpedia.org/resource/Tropopause +
, http://dbpedia.org/resource/175th_meridian_west +
, http://dbpedia.org/resource/Philippines +
, http://dbpedia.org/resource/North_America +
, http://dbpedia.org/resource/75th_meridian_west +
, http://dbpedia.org/resource/Gulf_of_Mexico +
, http://dbpedia.org/resource/Cumulus_clouds +
, http://dbpedia.org/resource/Trough_%28meteorology%29 +
, http://dbpedia.org/resource/Troposphere +
, http://dbpedia.org/resource/Category:Tropical_meteorology +
, http://dbpedia.org/resource/Tropical_cyclogenesis +
, http://dbpedia.org/resource/Tropics +
, http://dbpedia.org/resource/Upper_tropospheric_cyclonic_vortex +
, http://dbpedia.org/resource/Northern_Hemisphere +
|
| http://dbpedia.org/property/wikiPageUsesTemplate
|
http://dbpedia.org/resource/Template:Cite_book +
, http://dbpedia.org/resource/Template:Reflist +
, http://dbpedia.org/resource/Template:Main +
|
| http://purl.org/dc/terms/subject
|
http://dbpedia.org/resource/Category:Tropical_meteorology +
|
| http://purl.org/linguistics/gold/hypernym
|
http://dbpedia.org/resource/Trough +
|
| http://www.w3.org/ns/prov#wasDerivedFrom
|
http://en.wikipedia.org/wiki/Tropical_upper_tropospheric_trough?oldid=1031797543&ns=0 +
|
| http://xmlns.com/foaf/0.1/isPrimaryTopicOf
|
http://en.wikipedia.org/wiki/Tropical_upper_tropospheric_trough +
|
| owl:sameAs |
http://dbpedia.org/resource/Tropical_upper_tropospheric_trough +
, http://rdf.freebase.com/ns/m.07gksk +
, https://global.dbpedia.org/id/4wT3u +
, http://simple.dbpedia.org/resource/Tropical_Upper_Tropospheric_Trough +
, http://www.wikidata.org/entity/Q7846187 +
, http://zh.dbpedia.org/resource/%E7%86%B1%E5%B8%B6%E5%B0%8D%E6%B5%81%E5%B1%A4%E4%B8%8A%E9%83%A8%E6%A7%BD +
|
| rdf:type |
http://dbpedia.org/ontology/Crater +
|
| rdfs:comment |
熱帶對流層上部槽（英語：Tropical upper tropospheric trough，縮寫：TUTT）是一條位於熱帶高空（約200百帕面）的槽線，其可經由中緯度西風槽振幅延大而伸展到熱帶而成，亦可為高層反氣旋南側之高空東風倒槽。其將帶來強烈垂直风切变而影響熱帶氣旋或熱帶擾動的發展，但亦有情況是因帶來良好的高空輻散而助長熱帶氣旋的發展。在環境許可下，其會發展成擁有完整環流的高空冷心低壓，並有可能發展至地面而誘生出低層之熱帶擾動發展。
, A tropical upper tropospheric trough (TUTT … A tropical upper tropospheric trough (TUTT), also known as the mid-oceanic trough, is a trough situated in the upper-level (at about 200 hPa) tropics. Its formation is usually caused by the intrusion of energy and wind from the mid-latitudes into the tropics. It can also develop from the inverted trough adjacent to an upper level anticyclone. TUTTs are different from mid-latitude troughs in the sense that they are maintained by subsidence warming near the tropopause which balances radiational cooling. When strong, they can present a significant vertical wind shear to the tropics and subdue tropical cyclogenesis. When upper cold lows break off from their base, they tend to retrograde and force the development of, or enhance, surface troughs and tropical waves to their east. Under special ciical waves to their east. Under special ci
|
| rdfs:label |
Tropical upper tropospheric trough
, 熱帶對流層上部槽
|
