This HTML5 document contains 93 embedded RDF statements represented using HTML+Microdata notation.

The embedded RDF content will be recognized by any processor of HTML5 Microdata.

Namespace Prefixes

PrefixIRI
dctermshttp://purl.org/dc/terms/
dbohttp://dbpedia.org/ontology/
foafhttp://xmlns.com/foaf/0.1/
n5http://dbpedia.org/resource/File:
n22https://global.dbpedia.org/id/
n15http://si.dbpedia.org/resource/
dbthttp://dbpedia.org/resource/Template:
rdfshttp://www.w3.org/2000/01/rdf-schema#
dbpedia-nnhttp://nn.dbpedia.org/resource/
freebasehttp://rdf.freebase.com/ns/
dbpedia-pthttp://pt.dbpedia.org/resource/
dbpedia-simplehttp://simple.dbpedia.org/resource/
n12http://commons.wikimedia.org/wiki/Special:FilePath/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
owlhttp://www.w3.org/2002/07/owl#
dbpedia-zhhttp://zh.dbpedia.org/resource/
dbpedia-frhttp://fr.dbpedia.org/resource/
wikipedia-enhttp://en.wikipedia.org/wiki/
dbchttp://dbpedia.org/resource/Category:
dbphttp://dbpedia.org/property/
provhttp://www.w3.org/ns/prov#
xsdhhttp://www.w3.org/2001/XMLSchema#
dbpedia-idhttp://id.dbpedia.org/resource/
wikidatahttp://www.wikidata.org/entity/
goldhttp://purl.org/linguistics/gold/
dbrhttp://dbpedia.org/resource/

Statements

Subject Item
dbr:Monsoon_trough
rdf:type
dbo:AnatomicalStructure owl:Thing
rdfs:label
Palung muson Monsoon trough Creux de mousson Cavado de monção 季风槽
rdfs:comment
O cavado de monção é uma porção da Zona de Convergência Intertropical no Pacífico Ocidental, conforme representado por uma linha em um mapa meteorológico mostrando os locais de pressão mínima ao nível do mar, e, como tal, é uma zona de convergência entre os padrões de vento dos hemisférios sul e norte. Palung muson atau palung monsun merupakan bagian dari Daerah Pertemuan Angin Antar Tropis di wilayah barat Samudera Pasifik yang digambarkan dengan suatu bentuk garis pada peta cuaca yang diartikan sebagai lokasi tekanan permukaan laut yang rendah. Palung muson ini pun merupakan daerah pertemuan antarpola angin dari masing-masing belahan bumi selatan dan belahan bumi utara. The monsoon trough is a portion of the Intertropical Convergence Zone in the Western Pacific, as depicted by a line on a weather map showing the locations of minimum sea level pressure, and as such, is a convergence zone between the wind patterns of the southern and northern hemispheres. 季风槽（英語：Monsoon trough），氣象學名詞，是熱帶幅合帶的一部份，由跨赤道季風與偏東信風的幅合產生。季風槽中一般有降雨天氣，亦不時有熱帶氣旋在其中生成。 Un creux de mousson est une partie de la zone de basses pressions de la Zone de convergence intertropicale (ZCIT) qui s'étend vers les pôles en un creux barométrique. Il s'agit d'une zone de convergence entre la circulation atmosphérique de l'Hémisphère Sud et de l'Hémisphère Nord. Les creux de moussons ont de multiples implications. Ils peuvent amorcer le processus de cyclogénèse tropicale. Comme leurs noms l'indiquent, ils sont également impliqués dans la saison humide des climats sous l'influence de la mousson. Ils sont également impliqués dans des oscillations climatiques, notamment l'Oscillation de Madden-Julian.
rdfs:seeAlso
dbr:Wet_season
foaf:depiction
n12:Auguststreamlinesnavy.jpg n12:WorldwideTCpeaks.gif n12:Central_Calcutta_after_Rain.jpg n12:MonsoonDepression2004091600.jpg n12:Februarystreamlinesnavy.jpg
dcterms:subject
dbc:Tropical_meteorology dbc:Atmospheric_dynamics
dbo:wikiPageID
7125481
dbo:wikiPageRevisionID
1124747952
dbo:wikiPageWikiLink
dbr:Convergence_zone dbc:Tropical_meteorology n5:MonsoonDepression2004091600.jpg n5:Central_Calcutta_after_Rain.jpg dbr:Wet_season dbr:Regional_Specialized_Meteorological_Centre dbr:Bay_of_Bengal dbr:Southern_Hemisphere dbr:Cyclone_Komen dbr:Monsoon dbr:Weather_map dbc:Atmospheric_dynamics dbr:Intertropical_Convergence_Zone dbr:Hemisphere_of_the_Earth dbr:40th_parallel_north dbr:Surface_weather_analysis n5:Auguststreamlinesnavy.jpg dbr:Rainforest dbr:South_Pacific_convergence_zone dbr:Vorticity dbr:El_Niño n5:Februarystreamlinesnavy.jpg dbr:Thermal_low dbr:20th_parallel_north dbr:20th_parallel_south dbr:Subtropical_ridge dbr:10th_parallel_north dbr:Jet_stream dbr:Tropics dbr:South_American_convergence_zone n5:WorldwideTCpeaks.gif dbr:Latitude dbr:Tropical_cyclone dbr:Subtropics dbr:Madden–Julian_oscillation dbr:Shear_line_(meteorology) dbr:Trade_winds dbr:Outback dbr:Yangtze dbr:Tropical_cyclogenesis dbr:Joint_Typhoon_Warning_Center dbr:Rainband dbr:Thunderstorm dbr:Australia dbr:Satellite_imagery
owl:sameAs
dbpedia-zh:季风槽 n15:මෝසම්_දෙකිඳ dbpedia-simple:Monsoon_trough wikidata:Q3244298 dbpedia-id:Palung_muson dbpedia-pt:Cavado_de_monção n22:2z8c8 freebase:m.0h5gq9 dbpedia-nn:Monsuntråg dbpedia-fr:Creux_de_mousson
dbp:wikiPageUsesTemplate
dbt:Good_article dbt:Short_description dbt:See_also dbt:Use_dmy_dates dbt:Reflist dbt:Main
dbo:thumbnail
n12:Auguststreamlinesnavy.jpg?width=300
dbo:abstract
The monsoon trough is a portion of the Intertropical Convergence Zone in the Western Pacific, as depicted by a line on a weather map showing the locations of minimum sea level pressure, and as such, is a convergence zone between the wind patterns of the southern and northern hemispheres. Westerly monsoon winds lie in its equatorward portion while easterly trade winds exist poleward of the trough. Right along its axis, heavy rains can be found which usher in the peak of a location's respective rainy season. As it passes poleward of a location, hot and dry conditions develop. The monsoon trough plays a role in creating many of the world's rainforests. The term monsoon trough is most commonly used in monsoonal regions of the Western Pacific such as Asia and Australia. The migration of the ITCZ/monsoon trough into a landmass heralds the beginning of the annual rainy season during summer months. Depressions and tropical cyclones often form in the vicinity of the monsoon trough, with each capable of producing a year's worth of rainfall in a matter of days. 季风槽（英語：Monsoon trough），氣象學名詞，是熱帶幅合帶的一部份，由跨赤道季風與偏東信風的幅合產生。季風槽中一般有降雨天氣，亦不時有熱帶氣旋在其中生成。 Palung muson atau palung monsun merupakan bagian dari Daerah Pertemuan Angin Antar Tropis di wilayah barat Samudera Pasifik yang digambarkan dengan suatu bentuk garis pada peta cuaca yang diartikan sebagai lokasi tekanan permukaan laut yang rendah. Palung muson ini pun merupakan daerah pertemuan antarpola angin dari masing-masing belahan bumi selatan dan belahan bumi utara. Angin muson baratan terletak di bagian yang mengarah ke khatulistiwa, sedangkan angin pasat timuran berada di bagian palung yang mengarah ke wilayah kutub. Tepat di sepanjang poros dari palung muson ini, terdapat pertumbuhan awan-awan hujan yang sangat pesat, sehingga menjadikannya area bercurah hujan tinggi dan sebagai penanda puncak dari musim penghujan. Selain itu, palung muson ini sangat berperan terhadap pembentukan bioma hutan hujan tropis di pelbagai wilayah di dunia. Istilah palung muson ini lebih sering digunakan di wilayah yang dipengaruhi oleh pergerakan angin muson di sebelah barat Pasifik seperti wilayah Asia dan Australia. Pergerakan palung muson ke wilayah daratan biasanya menjadi pertanda dimulainya periode musim basah selama bulan-bulan musim panas di masing-masing belahan bumi, baik utara dan selatan. Tekanan udara rendah, bibit siklon tropis, serta siklon tropis itu sendiri biasanya terbentuk di sekitar palung muson yang dapat menyebabkan terjadinya curah hujan yang amat sangat tinggi dalam durasi yang singkat. Un creux de mousson est une partie de la zone de basses pressions de la Zone de convergence intertropicale (ZCIT) qui s'étend vers les pôles en un creux barométrique. Il s'agit d'une zone de convergence entre la circulation atmosphérique de l'Hémisphère Sud et de l'Hémisphère Nord. Les creux de moussons ont de multiples implications. Ils peuvent amorcer le processus de cyclogénèse tropicale. Comme leurs noms l'indiquent, ils sont également impliqués dans la saison humide des climats sous l'influence de la mousson. Ils sont également impliqués dans des oscillations climatiques, notamment l'Oscillation de Madden-Julian. O cavado de monção é uma porção da Zona de Convergência Intertropical no Pacífico Ocidental, conforme representado por uma linha em um mapa meteorológico mostrando os locais de pressão mínima ao nível do mar, e, como tal, é uma zona de convergência entre os padrões de vento dos hemisférios sul e norte. Os ventos de monção de oeste estão em sua porção equatorial, enquanto os vento alísios de leste existem em direção ao pólo da depressão. Bem ao longo de seu eixo, chuvas fortes podem ser encontradas, o que dá início ao pico da respectiva estação das chuvas de um local. À medida que passa em direção aos pólos de um local, desenvolvem-se condições quentes e secas. A depressão das monções desempenha um papel importante na criação de muitas das florestas tropicais do mundo. O termo cavado das monções é mais comumente usado em regiões de monções do Pacífico Ocidental, como Ásia e Austrália. A migração do cavado ITCZ/monção para uma massa de terra anuncia o início da estação chuvosa anual durante os meses de verão. Depressões e ciclones tropicais geralmente se formam nas proximidades do cavado das monções, cada um capaz de produzir o valor de um ano de chuva em questão de dias.
gold:hypernym
dbr:Portion
prov:wasDerivedFrom
wikipedia-en:Monsoon_trough?oldid=1124747952&ns=0
dbo:wikiPageLength
14489
foaf:isPrimaryTopicOf
wikipedia-en:Monsoon_trough