5. Conclusions
In conclusion, projection of our snow leopard distribution model to the LGM, mid-Holocene and 2070 enabled us to identify climatically stable habitat and habitat that is threatened by climate change. The stable habitat, with a total area of about 1.1 million km2 , accounts for about 50% of the current snow leopard range. Three large patches, the Altai, Qilian, and Tian Shan-Pamir-Hindu Kush-Karakoram (TPHK) mountain ranges, which account for about 35% of the current snow leopard range, should function as effective snow leopard refugia. Existence of the refugia is largely due to the unique mountain environment in High Asia, which maintains a relatively constant arid or semi-arid climate. Aridity in these regions prevents development of forests and glaciers, and thus results in stable alpine steppe for snow leopards to inhabit. The stable alpine steppe may also function as climate refugia for other alpine animals. Climate refugia sheltered snow leopards during the past glacier-interglacial cycles. However, in the 21st century rapid warming in High Asia will shorten the window for snow leopards to adapt to climate change, increase habitat fragmentation, and increase human activity in the region. Protection and restoration of the fragile alpine steppe ecosystem will be an important conservation action to benefit snow leopards and other sympatric species.