Articles | Volume 14, issue 11
https://doi.org/10.5194/essd-14-5093-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/essd-14-5093-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Data description paper
| 
22 Nov 2022
Data description paper |
| 22 Nov 2022
| 22 Nov 2022
A newly integrated ground temperature dataset of permafrost along the China–Russia crude oil pipeline route in Northeast China
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Da Xing'anling Observation and Research Station of Frozen-Ground
Engineering and Environment, Northwest Institute of Eco-Environment and
Resources, Chinese Academy of Sciences, Jagdaqi, Inner Mongolia 165000,
China
School of Engineering Science, University of Chinese Academy of
Sciences, Beijing 100049, China
Wei Ma
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Da Xing'anling Observation and Research Station of Frozen-Ground
Engineering and Environment, Northwest Institute of Eco-Environment and
Resources, Chinese Academy of Sciences, Jagdaqi, Inner Mongolia 165000,
China
School of Engineering Science, University of Chinese Academy of
Sciences, Beijing 100049, China
Fei Wang
CORRESPONDING AUTHOR
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Faculty of Civil Engineering and Mechanics, Jiangsu University,
Zhenjiang 212013, China
Huijun Jin
CORRESPONDING AUTHOR
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Da Xing'anling Observation and Research Station of Frozen-Ground
Engineering and Environment, Northwest Institute of Eco-Environment and
Resources, Chinese Academy of Sciences, Jagdaqi, Inner Mongolia 165000,
China
School of Civil Engineering and Permafrost Institute, Northeast
Forestry University, Harbin 150040, China
Alexander Fedorov
Melnikov Permafrost Institute, Russian Academy of Sciences, Yakutsk
677010, Russia
Dun Chen
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Da Xing'anling Observation and Research Station of Frozen-Ground
Engineering and Environment, Northwest Institute of Eco-Environment and
Resources, Chinese Academy of Sciences, Jagdaqi, Inner Mongolia 165000,
China
Gang Wu
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Da Xing'anling Observation and Research Station of Frozen-Ground
Engineering and Environment, Northwest Institute of Eco-Environment and
Resources, Chinese Academy of Sciences, Jagdaqi, Inner Mongolia 165000,
China
School of Engineering Science, University of Chinese Academy of
Sciences, Beijing 100049, China
Yapeng Cao
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Da Xing'anling Observation and Research Station of Frozen-Ground
Engineering and Environment, Northwest Institute of Eco-Environment and
Resources, Chinese Academy of Sciences, Jagdaqi, Inner Mongolia 165000,
China
School of Engineering Science, University of Chinese Academy of
Sciences, Beijing 100049, China
Yu Zhou
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Da Xing'anling Observation and Research Station of Frozen-Ground
Engineering and Environment, Northwest Institute of Eco-Environment and
Resources, Chinese Academy of Sciences, Jagdaqi, Inner Mongolia 165000,
China
School of Engineering Science, University of Chinese Academy of
Sciences, Beijing 100049, China
Yanhu Mu
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Da Xing'anling Observation and Research Station of Frozen-Ground
Engineering and Environment, Northwest Institute of Eco-Environment and
Resources, Chinese Academy of Sciences, Jagdaqi, Inner Mongolia 165000,
China
School of Engineering Science, University of Chinese Academy of
Sciences, Beijing 100049, China
Yuncheng Mao
School of Civil Engineering, Northwest Minzu University, Lanzhou
730000, China
Jun Zhang
School of Civil Engineering, Henan Polytechnic University, Jiaozuo
454000, China
Kai Gao
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Da Xing'anling Observation and Research Station of Frozen-Ground
Engineering and Environment, Northwest Institute of Eco-Environment and
Resources, Chinese Academy of Sciences, Jagdaqi, Inner Mongolia 165000,
China
School of Engineering Science, University of Chinese Academy of
Sciences, Beijing 100049, China
Xiaoying Jin
School of Civil Engineering and Permafrost Institute, Northeast
Forestry University, Harbin 150040, China
Ruixia He
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Da Xing'anling Observation and Research Station of Frozen-Ground
Engineering and Environment, Northwest Institute of Eco-Environment and
Resources, Chinese Academy of Sciences, Jagdaqi, Inner Mongolia 165000,
China
Xinyu Li
School of Civil Engineering, Harbin Institute of Technology, Harbin
150090, China
Yan Li
State Key Laboratory of Frozen Soil Engineering, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Da Xing'anling Observation and Research Station of Frozen-Ground
Engineering and Environment, Northwest Institute of Eco-Environment and
Resources, Chinese Academy of Sciences, Jagdaqi, Inner Mongolia 165000,
China
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Cited
4 citations as recorded by crossref.
- Mechanical Response of a Buried Pipeline to Permafrost Thawing Based on Sequential Coupling Method F. Wang et al. 10.3390/atmos14040620
- Distribution and Degradation Processes of Isolated Permafrost near Buried Oil Pipelines by Means of Electrical Resistivity Tomography and Ground Temperature Monitoring: A Case Study of Da Xing’anling Mountains, Northeast China G. Wu et al. 10.3390/rs15030707
- Study of Methane Emission and Geological Sources in Northeast China Permafrost Area Related to Engineering Construction and Climate Disturbance Based on Ground Monitoring and AIRS Z. Xu et al. 10.3390/atmos14081298
- A newly integrated ground temperature dataset of permafrost along the China–Russia crude oil pipeline route in Northeast China G. Li et al. 10.5194/essd-14-5093-2022
3 citations as recorded by crossref.
- Mechanical Response of a Buried Pipeline to Permafrost Thawing Based on Sequential Coupling Method F. Wang et al. 10.3390/atmos14040620
- Distribution and Degradation Processes of Isolated Permafrost near Buried Oil Pipelines by Means of Electrical Resistivity Tomography and Ground Temperature Monitoring: A Case Study of Da Xing’anling Mountains, Northeast China G. Wu et al. 10.3390/rs15030707
- Study of Methane Emission and Geological Sources in Northeast China Permafrost Area Related to Engineering Construction and Climate Disturbance Based on Ground Monitoring and AIRS Z. Xu et al. 10.3390/atmos14081298
Latest update: 17 Apr 2024
Short summary
A permafrost monitoring network was established along the China–Russia crude oil pipeline (CRCOP) route at the eastern flank of the northern Da Xing'anling Mountains in Northeast China. The resulting datasets fill the gaps in the spatial coverage of mid-latitude mountain permafrost databases. Results show that permafrost warming has been extensively observed along the CRCOP route, and local disturbances triggered by the CRCOPs have resulted in significant permafrost thawing.
A permafrost monitoring network was established along the China–Russia crude oil pipeline...
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