[1]ZHANG De-yu,FAN Hao-ming,ZHOU Li-li,et al.Response of Soil Erosion of Spring Thaw Period to Climate Change in Area of Nenjiang River[J].Research of Soil and Water Conservation,2009,16(06):112-115.
Copy
Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
16
Number of periods:
2009 06
Page number:
112-115
Column:
Public date:
2009-12-20
- Title:
-
Response of Soil Erosion of Spring Thaw Period to Climate Change in Area of Nenjiang River
- Author(s):
-
ZHANG De-yu, FAN Hao-ming, ZHOU Li-li, WU Min, LIU Jia, FENG Li-ying
-
College of Water Conservancy, Shenyang Agriculture University, Shenyang 110161, China
-
- Keywords:
-
climate change; spring thaw period; river runoff; sediment discharge; area of Nenjiang River
- CLC:
-
S157.1
- DOI:
-
-
- Abstract:
-
Based on hydrological data recorded by Dalai Hydrologic Station and the same period of meteorological data by the 16 stations in area of Nenjiang River, we analyzed the climate change of spring thaw period from 1963 to 1988 and its influence on soil erosion. Results show that the trend of temperature appeared a downward trend and increasing trend of precipitation amount, with the average temperature of spring thaw period increasing. The average temperature and precipitation amount has a positive role on the increasing of the river runoff, but the effect of precipitation on river runoff was even more significant than temperature. Passing on the average temperature, precipitation, runoff (including snowmelt runoff) and sediment discharge to partial correlation analysis, spring thaw period of precipitation and river runoff on the impact of sediment discharge was even more significant and positive correlation with the average temperature was negatively correlated, but no significant impact.