Titlebook: Water Resources Research in Northwest China; Yaning Chen Book 2014 Springer Science+Business Media Dordrecht 2014 Climate change Northwest

得罪人

Exordium,d strong winds. (3) The multicultural population is mainly distributed in the oases, where oasis agriculture is the mainstay. The ecosystems are extremely fragile due mainly to the internal factors of ecological processes and the interference of human activities.

Expiration

Conflict

燕麦

Hydrologic System in Northwest China, baseflow. In addition, in the Tizinafu River, the contribution of ice/snowmelt water varied from 25.96 to 68.87 % for spatial characteristics, and from 28.31 to 65.43 % for seasonal characteristics. The mean of the ice/snowmelt percentage is 43 %, which meant that ice/snowmelt water was the main su

anachronistic

Response of Runoff to Climate Change, runoff is 90.4, 55.7, 63.1 and 78.8 %, respectively. (3) It was discovered that runoff in the Aksu and Yarkand Rivers is increasing with rising precipitation and temperature levels, and that runoff in the Hotan River is likewise increasing, but the rate of increase there is minimal. As runoff’s res

蛰伏

LAY

promote

Glacier Change and Its Impact on Water Resources,ise, the melting of glaciers is accelerated and the meltwater runoff has increased to over 200 × 10. m., accounting for more than 25 % of the quantity of surface water 789 × 10. m.. Due to serious melting, glacier area reduced by 11.7 % in the recent 30 years and the volume loss is more rapid. Chang

拾落穗

Spatiotemporal Variation of Snow Cover from Space in Northern Xinjiang,injiang, China by using the cloud-removed MODIS snow cover product. Together, snow cover days (SCD), snow cover index (SCI), snow cover onset date (SCOD) and snow cover end date (SCED) provide important information on the snow cover conditions and can be applied in any region of interests. These inf