The Mindanao Current (MC) is a southward current in the western Pacific Ocean that transports mass and freshwater between ocean basins. It is a low-latitude western boundary current that follows the eastern coast of the Philippine island group and its namesake, Mindanao. The MC forms from the North Equatorial Current (NEC) that flows from east to west between 10-20°N. As it travels west, the NEC reaches its western limit: the coast of the Philippines. Once it encounters shallower waters near land, it “splits” into two branches: one moves northward and becomes the Kuroshio current and one moves southward and becomes the Mindanao Current. The process of splitting is called a bifurcation.
| Attributes | Values |
|---|
| rdf:type
| |
| rdfs:label
| - Corrent de Mindanao (ca)
- Corriente de Mindanao (es)
- Mindanaoko itsaslasterra (eu)
- Corrente di Mindanao (it)
- Mindanao Current (en)
|
| rdfs:comment
| - La corriente de Mindanao es una corriente oceánica a lo largo del lado oriental de la Filipinas meridionales. Es una corriente que fluye hacia el sur, estrecha, que empieza en la latitud con 13Sv incrementándose en fuerza hasta los 33Sv a 5.5°N. La corriente se divide antes de la costa del sureste de Mindanao donde una parte fluye ciclónicamente hacia el mar de Célebes más tarde alimentando la Contra-Corriente Ecuatorial del Norte mientras que otra parte alimenta directamente la Contra-Corriente Ecuatorial. (es)
- La corrente di Mindanao è una corrente oceanica che fluisce sul lato orientale della parte meridionale delle Filippine. Si tratta di una corrente caratterizzata da un flusso piuttosto stretto, che scorre in direzione sud a partire dal 14°N con una portata di 13Sv che aumenta fino a raggiungere 33Sv a 5.5°N. Prima di raggiungere la costa sudorientale di Mindanao, la corrente si divide in due parti; la prima fluisce con rotazione ciclonica nel Mare di Celebes e successivamente va ad alimentare la controcorrente equatoriale Nord (NECC), mentre l'altra parte va direttamente ad alimentare la NECC. (it)
- El Corrent de Mindanao és un corrent oceànic al llarg de la banda occidental de les Filipines del sud. És un corrent estret, que flueix cap al sud començant a 14°N amb 13Sv incrementant la força a 33Sv a 5.5°N. El corrent es divideix abans d'arribar a la costa del sud-est de Mindanao on una part flueix ciclònicament en l'interior de la Mar de Cèlebes; més tard alimentant el Contra Corrent Nord Equatorial (NECC) mentre una altra part alimenta el NECC directament. Hi ha un ramal que es desvia per l'Estret de Macassar. (ca)
- Mindanaoko itsaslasterra Filipinetako hegoaldeko uharteetako ekialdeko kostetatik gertu igarotzen den itsaslaster bat da. Itsaslasterra estua da, eta hegoalderantz higitzen da. Gutxi gorabehera 14° N latitudean sortzen da. Sorgunean 13 milioi metro kubiko garraiatzen ditu segundoko, baina haren indarra handituz joaten da hegoalderantz egin ahala, eta 5,5° N latitudean segundoko 13 milioi metro kubikoraino iristen da. (eu)
- The Mindanao Current (MC) is a southward current in the western Pacific Ocean that transports mass and freshwater between ocean basins. It is a low-latitude western boundary current that follows the eastern coast of the Philippine island group and its namesake, Mindanao. The MC forms from the North Equatorial Current (NEC) that flows from east to west between 10-20°N. As it travels west, the NEC reaches its western limit: the coast of the Philippines. Once it encounters shallower waters near land, it “splits” into two branches: one moves northward and becomes the Kuroshio current and one moves southward and becomes the Mindanao Current. The process of splitting is called a bifurcation. (en)
|
| foaf:depiction
| |
| dct:subject
| |
| Wikipage page ID
| |
| Wikipage revision ID
| |
| Link from a Wikipage to another Wikipage
| |
| Link from a Wikipage to an external page
| |
| sameAs
| |
| dbp:wikiPageUsesTemplate
| |
| thumbnail
| |
| has abstract
| - El Corrent de Mindanao és un corrent oceànic al llarg de la banda occidental de les Filipines del sud. És un corrent estret, que flueix cap al sud començant a 14°N amb 13Sv incrementant la força a 33Sv a 5.5°N. El corrent es divideix abans d'arribar a la costa del sud-est de Mindanao on una part flueix ciclònicament en l'interior de la Mar de Cèlebes; més tard alimentant el Contra Corrent Nord Equatorial (NECC) mentre una altra part alimenta el NECC directament. Hi ha un ramal que es desvia per l'Estret de Macassar. El Corrent Nord Equatorial per tant, es divideix en dos corrents, el Corrent de Mindanao, cap al sud, i el Corrent de Kuro Shio, cap al nord.La Latitud del punt de divisió del NEC depèn de l'estació de l'any i de la profunditat del corrent. Té una gran influència causada per l'existència dels vents Monsons. (ca)
- Mindanaoko itsaslasterra Filipinetako hegoaldeko uharteetako ekialdeko kostetatik gertu igarotzen den itsaslaster bat da. Itsaslasterra estua da, eta hegoalderantz higitzen da. Gutxi gorabehera 14° N latitudean sortzen da. Sorgunean 13 milioi metro kubiko garraiatzen ditu segundoko, baina haren indarra handituz joaten da hegoalderantz egin ahala, eta 5,5° N latitudean segundoko 13 milioi metro kubikoraino iristen da. Mindanaoko hego-ekialdeko kostara iritsi baino lehen, itsaslasterra erdibitu egiten da. Parte bat Celebesko itsasorantz abiatzen da, eta, gero, Iparraldeko Kontralaster Ekuatoriala elikatzen du. Beste partea, berriz, zuzenean elikatzen du Iparraldeko Kontralaster Ekuatoriala. (eu)
- La corriente de Mindanao es una corriente oceánica a lo largo del lado oriental de la Filipinas meridionales. Es una corriente que fluye hacia el sur, estrecha, que empieza en la latitud con 13Sv incrementándose en fuerza hasta los 33Sv a 5.5°N. La corriente se divide antes de la costa del sureste de Mindanao donde una parte fluye ciclónicamente hacia el mar de Célebes más tarde alimentando la Contra-Corriente Ecuatorial del Norte mientras que otra parte alimenta directamente la Contra-Corriente Ecuatorial. (es)
- The Mindanao Current (MC) is a southward current in the western Pacific Ocean that transports mass and freshwater between ocean basins. It is a low-latitude western boundary current that follows the eastern coast of the Philippine island group and its namesake, Mindanao. The MC forms from the North Equatorial Current (NEC) that flows from east to west between 10-20°N. As it travels west, the NEC reaches its western limit: the coast of the Philippines. Once it encounters shallower waters near land, it “splits” into two branches: one moves northward and becomes the Kuroshio current and one moves southward and becomes the Mindanao Current. The process of splitting is called a bifurcation. The Mindanao Current flows towards the equator and is most intense near the surface, reaching maximum speeds of . It can be observed until depths of near the Philippine coast and extends until offshore. The MC transports climatic signals and in doing so, influences the regional climate and the El Niño-Southern Oscillation (ENSO). Overall, the Mindanao Current is critical in the circulation within the whole Pacific basin. However, in comparison with other boundary currents in the North Pacific, the Mindanao Current has received limited attention and therefore little is known about it. (en)
- La corrente di Mindanao è una corrente oceanica che fluisce sul lato orientale della parte meridionale delle Filippine. Si tratta di una corrente caratterizzata da un flusso piuttosto stretto, che scorre in direzione sud a partire dal 14°N con una portata di 13Sv che aumenta fino a raggiungere 33Sv a 5.5°N. Prima di raggiungere la costa sudorientale di Mindanao, la corrente si divide in due parti; la prima fluisce con rotazione ciclonica nel Mare di Celebes e successivamente va ad alimentare la controcorrente equatoriale Nord (NECC), mentre l'altra parte va direttamente ad alimentare la NECC. (it)
|
| gold:hypernym
| |
| prov:wasDerivedFrom
| |
| page length (characters) of wiki page
| |
| foaf:isPrimaryTopicOf
| |
| is Link from a Wikipage to another Wikipage
of | |
| is foaf:primaryTopic
of | |
![[RDF Data]](/fct/images/sw-rdf-blue.png)
![[cxml]](/fct/images/cxml_doc.png)
![[csv]](/fct/images/csv_doc.png)
![[text]](/fct/images/ntriples_doc.png)
![[turtle]](/fct/images/n3turtle_doc.png)
![[ld+json]](/fct/images/jsonld_doc.png)
![[rdf+json]](/fct/images/json_doc.png)
![[rdf+xml]](/fct/images/xml_doc.png)
![[atom+xml]](/fct/images/atom_doc.png)
![[html]](/fct/images/html_doc.png)
