Dataran tinggi Tibet: Perbedaan antara revisi
Konten dihapus Konten ditambahkan
Rescuing 1 sources and tagging 0 as dead.) #IABot (v2.0.8 |
Fitur saranan suntingan: 1 pranala ditambahkan. |
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Baris 6:
|accessdate=23 Juli
|accessyear=2007
|archive-date=2006-01-12
|archive-url=https://web.archive.org/web/20060112023503/http://java.nationalgeographic.com/studentatlas/clickup/deserts.html
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}}</ref>
Baris 40 ⟶ 43:
|archive-url=https://web.archive.org/web/20080228081001/http://www.100gogo.com/canyon.htm
|dead-url=yes
}}</ref> Proses [[pengangkatan tektonik]] Daratan tinggi Tibet diperkirakan berdampak besar dalam [[perubahan iklim]], dan dianggap memengaruhi [[muson]] (angin musim) di Asia. Angin yang membawa udara hangat yang lembap dari selatan sepanjang [[Iklim India|musim monsun India]] (Juni-Oktober) menjadikan hujan banyak turun di [[India]] utara. Sementara itu, dataran tinggi Tibet menjadi sangat kering karena Pegunungan Himalaya membentuk [[daerah bayang-bayang hujan]]. Angin berhembus di dataran tinggi Tibet sambil menjatuhkan sedikit uap air yang tersisa. Akibatnya, udara yang bergerak semakin ke utara menjadi semakin kering sehingga terjadi [[padang pasir]] seperti [[Gurun Taklamakan]] dan [[Gurun Gobi]].<ref>{{cite web
|url=http://www.mala.bc.ca/~earles/tibet-uplift-feb03.htm
|title=Leaf morphology and the timing of the rise of the Tibetan Plateau
Baris 46 ⟶ 49:
|accessdate=23 Juli
|accessyear=2007
|archive-date=2003-07-21
|archive-url=https://web.archive.org/web/20030721043521/http://www.mala.bc.ca/~earles/tibet-uplift-feb03.htm
|dead-url=yes
}}</ref>
Baris 58 ⟶ 64:
* [http://web.ukonline.co.uk/michael.magee/awwls/00/wls104.html The End of Earth's Summer] {{Webarchive|url=https://web.archive.org/web/20020724112745/http://web.ukonline.co.uk/michael.magee/awwls/00/wls104.html |date=2002-07-24 }}
* [http://books.google.com/books?id=4q_XoMACOxkC&pg=PA62&dq=%22South+Tibet+Valley%22&output=html&sig=ygW6-rJibHfT5mnBGtcMEmpjZXQ Long Rivers and Distant Sources]
* [http://www.agu.org/sci_soc/EOSsokhabi.html "Roof of the Earth" Offers Clues About How Our Planet Was Shaped] {{Webarchive|url=https://web.archive.org/web/19970501040126/http://www.agu.org/sci_soc/EOSsokhabi.html |date=1997-05-01 }}
== Pranala luar ==
* {{en}} [http://www.plateauperspectives.org Plateau Perspectives] LSM internasional
* {{en}} [http://www.mala.bc.ca/~earles/tibet-uplift-feb03.htm Leaf morphology and the timing of the rise of the Tibetan Plateau] {{Webarchive|url=https://web.archive.org/web/20030721043521/http://www.mala.bc.ca/~earles/tibet-uplift-feb03.htm |date=2003-07-21 }}
* {{en}} [http://weather.msn.com/local.aspx?wealocations=wc:CHXX0331 Cuaca hari ini di timur Chang Tang] {{Webarchive|url=https://web.archive.org/web/20060319/http://weather.msn.com/local.aspx?wealocations=wc:CHXX0331 |date=2006-03-19 }}
* {{en}} [http://www.plateauperspectives.org/tibetan_PAs.htm Kawasan lindung di wilayah dataran tinggi Tibet] {{Webarchive|url=https://web.archive.org/web/20070510185558/http://www.plateauperspectives.org/tibetan_PAs.htm |date=2007-05-10 }}
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