Climate change and human occupations in the Lake Daihai basin, north-central China over the last 4500 years: A geo-archeological perspective

2017 ◽  
Vol 138 ◽  
pp. 367-377 ◽  
Author(s):  
Lichen Xu ◽  
Yan Liu ◽  
Qianli Sun ◽  
Jing Chen ◽  
Peng Cheng ◽  
...  
2009 ◽  
Vol 43 (1) ◽  
pp. 75-87 ◽  
Author(s):  
Qianli Sun ◽  
Sumin Wang ◽  
Jie Zhou ◽  
Zhongyuan Chen ◽  
Ji Shen ◽  
...  

2019 ◽  
Vol 58 ◽  
pp. 125632 ◽  
Author(s):  
Minhui He ◽  
Bao Yang ◽  
Sergio Rossi ◽  
Achim Bräuning ◽  
Vladimir Shishov ◽  
...  

2016 ◽  
Vol 7 (3) ◽  
pp. 578-597 ◽  
Author(s):  
Ruizhong Gao ◽  
Fengling Li ◽  
Xixi Wang ◽  
Tingxi Liu ◽  
Dandan Du

Rapid urbanization on streamflows may directly affect or be restricted by the sustainability of local water resources. This is particularly true for arid/semiarid areas such as the Wulanmulun River watershed in the rapidly-developing Ordos region of north central China. From 1997 to 2012, the gross domestic product (GDP) of the region increased fifty-fold, while the urban area grew by a factor of ten. This study fused multiple-source data on land use, hydrometeorology, and socioeconomics to examine temporal variations in the runoff due to climate change and urbanization. The results revealed that for the Wulanmulun River watershed, the runoff decreased consistently over the study period, with an inflection point around 2005. The average runoff from 2006 to 2012 was much smaller than that from 1997 to 2005, regardless of time scale; although the precipitation also fluctuated from 1997 to 2012, it exhibited no significant trend. From 1997–2005 to 2006–2012, both the urbanized area and GDP increased eight-fold while the population increased by 20%. Thus, urbanization rather than climate change is likely the major reason for the decrease in runoff after 2005. For the study watershed, low impact development practices (e.g. rain barrels) may need to be implemented during urbanization to achieve sustainable management of water resources.


PLoS ONE ◽  
2014 ◽  
Vol 9 (11) ◽  
pp. e112537 ◽  
Author(s):  
Yuan Jiang ◽  
Wentao Zhang ◽  
Mingchang Wang ◽  
Muyi Kang ◽  
Manyu Dong

2019 ◽  
Author(s):  
Chenliang Wu ◽  
◽  
Yuliang Duan ◽  
Trevor Cole ◽  
Jeffrey A. Nittrouer ◽  
...  

Forests ◽  
2021 ◽  
Vol 12 (5) ◽  
pp. 544
Author(s):  
Hang Ning ◽  
Ming Tang ◽  
Hui Chen

Dendroctonus armandi (Coleoptera: Curculionidae: Scolytidae) is a bark beetle native to China and is the most destructive forest pest in the Pinus armandii woodlands of central China. Due to ongoing climate warming, D. armandi outbreaks have become more frequent and severe. Here, we used Maxent to model its current and future potential distribution in China. Minimum temperature of the coldest month and precipitation seasonality are the two major factors constraining the current distribution of D. armandi. Currently, the suitable area of D. armandi falls within the Qinling Mountains and Daba Mountains. The total suitable area is 15.83 × 104 km2. Under future climate scenarios, the total suitable area is projected to increase slightly, while remaining within the Qinling Mountains and Daba Mountains. Among the climate scenarios, the distribution expanded the most under the maximum greenhouse gas emission scenario (representative concentration pathway (RCP) 8.5). Under all assumptions, the highly suitable area is expected to increase over time; the increase will occur in southern Shaanxi, northwest Hubei, and northeast Sichuan Provinces. By the 2050s, the highly suitable area is projected to increase by 0.82 × 104 km2. By the 2050s, the suitable climatic niche for D. armandi will increase along the Qinling Mountains and Daba Mountains, posing a major challenge for forest managers. Our findings provide information that can be used to monitor D. armandi populations, host health, and the impact of climate change, shedding light on the effectiveness of management responses.


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