scholarly journals Response of radial growth to climate change for Larix olgensis along an altitudinal gradient on the eastern slope of Changbai Mountain, Northeast China

2016 ◽  
Vol 40 (1) ◽  
pp. 24-35 ◽  
Author(s):  
YU Jian ◽  
◽  
◽  
◽  
◽  
...  
Keyword(s):  
Climate Change ◽  
Northeast China ◽  
Radial Growth ◽  
Altitudinal Gradient ◽  
Changbai Mountain ◽  
Larix Olgensis ◽  
Eastern Slope

Radial growth ofPinus koraiensisand carbon sequastration potential of the old growth forest in Changbai Mountain, Northeast China

2016 ◽  
Vol 36 (9) ◽  
Author(s):  
于健 YU Jian ◽  
罗春旺 LUO Chunwang ◽  
徐倩倩 XU Qianqian ◽  
孟盛旺 MENG Shengwang ◽  
李俊清 LI Junqing ◽  
...  
Keyword(s):  
Northeast China ◽  
Radial Growth ◽  
Changbai Mountain ◽  
Old Growth ◽  
Old Growth Forest

scholarly journals Analyzing the Impact of Climate Change and Human Activities on Surface Runoff in the Changbai Mountain Area, Northeast China

Water ◽  
2021 ◽  
Vol 13 (23) ◽  
pp. 3473
Author(s):  
Shanjun Zhang ◽  
Jia Liu ◽  
Chuanzhe Li ◽  
Fuliang Yu ◽  
Lanshu Jing ◽  
...  
Keyword(s):  
Climate Change ◽  
Time Series ◽  
River Basin ◽  
Human Activities ◽  
Surface Runoff ◽  
Northeast China ◽  
Changbai Mountain ◽  
Mountain Area ◽  
Mountainous Regions ◽  
Runoff Changes

Climate change and human activities are two important factors affecting surface runoff. In water resource management and planning, it is generally important to separate the contribution of these factors when assessing runoff changes. The Changbai Mountain area is rich in water resources and is an important hydropower energy base for Northeast China. This study used Sen’s slope estimator to explore trends in runoff precipitation and evapotranspiration from 1960 to 2016, and the results showed a downward trend in runoff and an upward trend in precipitation and evaporation in most areas. The mutation point of the annual time series for the observed runoff was estimated, and the time series was divided into the base period (1960–1975) and impact period (1976–2016). Based on the Budyko framework, we performed attribution analysis of the runoff changes, and analyzed the difference between the mountainous region and the whole basin. We determined that the impacts of climate change and human activities, on average, accounted for decreases in the runoff by 60.15% and 39.85%, respectively, for the Second Songhua River Basin; 73.74% and 26.26%, respectively, for the Tumen River Basin; 84.76% and 15.24%, respectively, for the Yalu River Basin; human activities were the main causes of runoff changes in the Changbai Mountain area; climate change was the main cause of runoff changes in mountainous regions. The results of this study show that the reasons for the change in runoff in mountainous regions and the whole basin in the same area are different, which has some illuminating significance for water resources management of different elevation areas.

Sign in / Sign up

Export Citation Format

Share Document