Qingchen Chao

Dr. Qingchen Chao

National Climate Center, China Meteorological Administration, Beijing 100081, China

Research Focus & Metrics

Academic Career Length

15Years (2012-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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6 May 2022 in Carbon Neutrality
Verified
Journal Article
Open access
PDF file
YWYang Wang
Yang Wang
Qingchen ChaoQingchen Chao
Qingchen Chao
LZLin Zhao
Lin Zhao
RCRui Chang
Rui Chang
Decarbonization of the energy system is the key to China’s goal of achieving carbon neutrality by 2060. However, the potential of wind and photovoltaic (PV) to power China remains unclear, hindering the holistic layout of the renewable energy development plan. Here, we used the wind and PV power generation potential assessment system based on the Geographic Information Systems (GIS) method to investigate the wind and PV power generation potential in China. Firstly, the high spatial-temporal resolution climate data and the mainstream wind turbines and PV modules, were used to assess the theoretical wind and PV power generation. Then, the technical, policy and economic (i.e., theoretical power generation) constraints for wind and PV energy development were comprehensively considered to evaluate the wind and solar PV power generation potential of China in 2020. The results showed that, under the current technological level, the wind and PV installed capacity potential of China is about 56.55 billion kW, which is approximately 9 times of those required under the carbon neutral scenario. The wind and PV power generation potential of China is about 95.84 PWh, which is approximately 13 times the electricity demand of China in 2020. The rich areas of wind power generation are mainly distributed in the western, northern, and coastal provinces of China. While the rich areas of PV power generation are mainly distributed in western and northern China. Besides, the degree of tapping wind and PV potential in China is not high, and the installed capacity of most provinces in China accounted for no more than 1% of the capacity potential, especially in the wind and PV potential-rich areas.

12 June 2022 in Environmental Monitoring and Assessment
Verified
Journal Article
Closed access
PDF file
BLBingsheng Liu
Bingsheng Liu
YFYufeng Fan
Yufeng Fan
BXBin Xue
Bin Xue
Tao WangTao Wang
Tao Wang
Qingchen ChaoQingchen Chao
Qingchen Chao

11 July 2022 in Atmosphere
Verified
Journal Article
Open access
PDF file
DYDian Yuan
Dian Yuan
Er LuEr Lu
Er Lu
WDWei Dai
Wei Dai
Qingchen ChaoQingchen Chao
Qingchen Chao
HWHui Wang
Hui Wang
SLshuling li
shuling li
Harbin, located in northeast China (NEC), has obvious monsoon climate characteristics due to the influence of its geographical environment. Under the control of the polar continental air mass, winter in Harbin is exceedingly cold and long, with the frequent invasion of the cold and dry air from the north. Because of its intensely cold climate in winter, Harbin has created a local form of tourism with its own characteristics: the snow and ice landscape attracts a large number of tourists. Therefore, the anomalies of air temperature and precipitation in winter have an important impact on the livelihood of the local people and economy. In the winter of 2018/2019, the ice and snow tourism in Harbin was harshly affected by the extreme weather, and the direct cause is the anomalies of atmospheric circulation. There is a center of strong positive geopotential height anomalies over east China, which favors the movement of warm air northwards to the NEC, resulting in warmer-than-normal air temperature. Anomalous precipitation is largely controlled by the anomalies of local water vapor and air temperature. The aim of this study was to determine whether the warmer-than-normal temperature, which made the atmosphere more resistant to saturation, was the primary cause of the reduced snowfall. The relative importance of water vapor and air temperature anomalies to the anomalous precipitation was compared. The results suggest that the warmer-than-normal temperature affected all levels, but its impact on the near-surface level was greater. At the middle and upper levels (above 850 hPa), in addition to the warmer-than-normal temperature, the amount of water vapor was less than normal. These conditions both reduced the amount of snow; however, by comparison, the dryness of the air contributed more significantly.

13 June 2022 in Carbon Neutrality
Verified
Journal Article
Open access
PDF file
YWYang Wang
Yang Wang
Qingchen ChaoQingchen Chao
Qingchen Chao
LZLin Zhao
Lin Zhao
RCRui Chang
Rui Chang

1 December 2012 in Journal of Meteorological Research
Verified
Journal Article
Closed access
PDF file
Qingchen ChaoQingchen Chao
Qingchen Chao
JCJiping Chao
Jiping Chao

11 July 2021 in International Journal of Climatology
Verified
Journal Article
Closed access
YGYanjun Guo
Yanjun Guo
GWGuofu Wang
Guofu Wang
Qingchen ChaoQingchen Chao
Qingchen Chao