Earths mean surface temperature has increased by about 08℃ since the early 20th century, with about twothirds of the increase occurring since 1980. The Intergovernmental Panel on Climate Change (IPCC) indicated that the Earths average surface temperature rose by 074℃±018℃ over the period of 1906-2005. The rate of warming over the last half of that period was almost doubles than that for the period as a whole (013±003℃ per decade, versus 007℃±002℃ per decade). During the 21st century, the global surface temperature is likely to rise a further 11℃ to 29℃ for their lowest emissions scenario and 24℃ to 64℃ for their highest. Observations as well as most climate model simulations are generally in accord with the hypothesis that the hydrologic cycle should intensify and become highly volatile with the greenhousegasinduced climate change, although uncertainties of these projections as well as the spatial and seasonal variability of the changes are much larger than that for temperature extremes. The likely effects of the warming include a more frequent occurrence of extreme weather events including heat waves, droughts and heavy rainfall, ocean acidification and species extinctions due to shifting temperature regimes. The effects are significant to humans including the threat to food security from decreasing crop yields and the loss of habitat from inundation, which will change humans living environment. Water resource is an important restricted factor for social and economic sustainable development in the Dry valleys of Hengduan Mountains. By using 24 meteorological stations in monthly precipitation (P) and temperature (t) observation data, on the basis of Taka hashis evaporation equation, the ground evaporation (E) and available precipitation (PE) related to water resources were calculated. The following conclusions were obtained. Short of precipitation and huge evaporation were typical feature in dry valleys in Hengduan Mountains, the annual average rainfall only about 7237 mm, the average annual evaporation capacity up to 4795 mm, more than 8489% of rainfall were evaporated, and only 1511% of annual precipitation were available. For the P, E and PE, the seasonal change was very obviously, from 1962 to 2009, the average value in summer were 4049 mm, 2399 mm and 2399 mm, accounted for 5594%, 5004% and 5594% to a year, respectively, and the proportion of 296%, 406% and 079%, respectively, in the winter. In the dry valley, atmospheric water decadal difference was very remarkable, the available of water resources was rich in the 1960s, relatively less in the 70s, gradually increased in the 80s and 90s, after entering this century appeared as reduced characteristic. In the dry valley, rainfall was likely to shift to reduced trend in the future and evaporation would remain the trend of increase, which make the amount of available water maintain the reduced trend, and the difficulty of water resources regulation would increase.〖JP〗〖HJ1〗〖HJ〗〖HQ〗