The elevation of the Tibetan plateau is thought to cause its surface to serve as a heat source that drives the South Asian summer monsoon, potentially coupling uplift of the plateau to climate changes on geologic timescales.
Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/dominant-control-south-asian-monsoon-orographic-insulation-versus-plateau-heating
[2] http://admin.indiaenvironmentportal.org.in/category/author/william-r-boos
[3] http://admin.indiaenvironmentportal.org.in/category/author/zhiming-kuang
[4] http://admin.indiaenvironmentportal.org.in/category/journal/nature
[5] http://admin.indiaenvironmentportal.org.in/category/thesaurus/himalaya
[6] http://admin.indiaenvironmentportal.org.in/category/thesaurus/atmosphere-and-ozone-layer
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/monsoons
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/india
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/south-asia