Articles | Volume 13, issue 7
https://doi.org/10.5194/essd-13-3453-2021
© Author(s) 2021. 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-13-3453-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Data description paper
| 
16 Jul 2021
Data description paper |
| 16 Jul 2021
| 16 Jul 2021
A 1 km resolution soil organic carbon dataset for frozen ground in the Third Pole
Dong Wang
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
Southern Marine Science and Engineering Guangdong Laboratory,
Guangzhou 511458, China
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
School of Geographical Sciences, Nanjing University of Information
Science & Technology, Nanjing 210000, China
Cuicui Mu
Key Laboratory of Western China's Environmental Systems (Ministry
of Education), College of Earth and Environmental Sciences, Lanzhou
University, Lanzhou 730000, China
Ren Li
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
Xianhua Wei
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
College of Geography and Environmental Science, Northwest Normal
University, Lanzhou 730070, China
Guojie Hu
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
Xiaofan Zhu
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
Junmin Hao
School of Civil Engineering, Lanzhou University of Technology,
Lanzhou 730050, China
Jie Ni
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
Xiangfei Li
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
Wensi Ma
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
Amin Wen
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
Chengpeng Shang
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
Yune La
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
Xin Ma
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
Xiaodong Wu
Cryosphere Research Station on the Qinghai–Tibetan Plateau, State
Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resource, Chinese Academy of Sciences, Lanzhou, Gansu
730000, China
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30 citations as recorded by crossref.
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- Can normalized difference vegetation index and climate data be used to estimate soil carbon, nitrogen, and phosphorus and their ratios in the Xizang grasslands? S. Wang et al. 10.3389/feart.2023.1340020
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30 citations as recorded by crossref.
- Effects of land use and land cover change on soil organic carbon storage in the Hexi regions, Northwest China Y. Li et al. 10.1016/j.jenvman.2022.114911
- The Spatial Ecological Environment Design of the Waterfront Public Areas of Rural Rivers Z. Ge & Z. Xin 10.2478/eces-2023-0024
- Carbon dynamics shift in changing cryosphere and hydrosphere of the Third Pole T. Gao et al. 10.1016/j.earscirev.2024.104717
- Impacts of Permafrost Degradation on Carbon Stocks and Emissions under a Warming Climate: A Review H. Jin & Q. Ma 10.3390/atmos12111425
- Uncertainties of soil organic carbon stock estimation caused by paleoclimate and human footprint on the Qinghai Plateau X. Liu et al. 10.1186/s13021-022-00203-z
- Storage, patterns, and environmental controls of soil organic carbon stocks in the permafrost regions of the Northern Hemisphere T. Wu et al. 10.1016/j.scitotenv.2022.154464
- The current and future of terrestrial carbon balance over the Tibetan Plateau T. Wang et al. 10.1007/s11430-022-1073-y
- Surface air temperature changes over the Tibetan Plateau: Historical evaluation and future projection based on CMIP6 models R. Chen et al. 10.1016/j.gsf.2022.101452
- Sedimentary organic carbon storage of thermokarst lakes and ponds across Tibetan permafrost region Z. Wei et al. 10.1016/j.scitotenv.2022.154761
- Improved permafrost stability by revegetation in extremely degraded grassland of the Qinghai-Tibetan Plateau Y. Jia et al. 10.1016/j.geoderma.2023.116350
- Temperature sensitivity of methanogenesis and anaerobic methane oxidation in thermokarst lakes modulated by surrounding vegetation on the Qinghai-Tibet Plateau Q. Xu et al. 10.1016/j.scitotenv.2023.167962
- Can normalized difference vegetation index and climate data be used to estimate soil carbon, nitrogen, and phosphorus and their ratios in the Xizang grasslands? S. Wang et al. 10.3389/feart.2023.1340020
- On the Spin‐Up Strategy for Spatial Modeling of Permafrost Dynamics: A Case Study on the Qinghai‐Tibet Plateau H. Ji et al. 10.1029/2021MS002750
- Characteristics of Freeze–Thaw Cycles in an Endorheic Basin on the Qinghai-Tibet Plateau Based on SBAS-InSAR Technology H. Zhou et al. 10.3390/rs14133168
- Thermal regime variations of the uppermost soil layer in the central Tibetan Plateau R. Chen et al. 10.1016/j.catena.2022.106224
- Evaluation and mapping soil organic carbon in seasonally frozen ground on the Tibetan Plateau R. Yang et al. 10.1016/j.catena.2023.107631
- In situ observations of soil hydraulic properties and soil moisture in a high, cold mountainous area of the northeastern Qinghai-Tibet Plateau J. Tian et al. 10.1007/s11430-022-1120-5
- A dataset of lake-catchment characteristics for the Tibetan Plateau J. Liu et al. 10.5194/essd-14-3791-2022
- Divergent Trajectory of Soil Autotrophic and Heterotrophic Respiration upon Permafrost Thaw G. Wang et al. 10.1021/acs.est.1c07575
- Spatial distributions and key drivers of microbial necromass carbon in permafrost deposits across the Tibetan Plateau M. He et al. 10.1360/TB-2023-1076
- Mineral and Climatic Controls Over Soil Organic Matter Stability Across the Tibetan Alpine Permafrost Region K. Fang et al. 10.1029/2021GB007118
- Spatiotemporal Patterns and Regional Differences in Soil Thermal Conductivity on the Qinghai–Tibet Plateau W. Liu et al. 10.3390/rs15041168
- Characteristics of methane emissions from alpine thermokarst lakes on the Tibetan Plateau G. Yang et al. 10.1038/s41467-023-38907-6
- Digital Mapping of Soil Organic Carbon Using UAV Images and Soil Properties in a Thermo-Erosion Gully on the Tibetan Plateau M. Ding et al. 10.3390/rs15061628
- Permafrost, active layer, and meteorological data (2010–2020) at the Mahan Mountain relict permafrost site of northeastern Qinghai–Tibet Plateau T. Wu et al. 10.5194/essd-14-1257-2022
- Frozen carbon is gradually thawing: Assessing interannual dynamics of thawed soil organic carbon stocks in the Tibetan Plateau permafrost area from 1901−2020 T. Shen et al. 10.1016/j.agrformet.2023.109793
- Climate-induced shifts in composition and protection regulate temperature sensitivity of carbon decomposition through soil profile X. Mao et al. 10.1016/j.soilbio.2022.108743
- Divergent changes in particulate and mineral-associated organic carbon upon permafrost thaw F. Liu et al. 10.1038/s41467-022-32681-7
- An improved estimate of soil carbon pool and carbon fluxes in the Qinghai-Tibetan grasslands using data assimilation with an ecosystem biogeochemical model R. Zhao et al. 10.1016/j.geoderma.2022.116283
- 青藏高原东北部高寒山区土壤水文属性数据和土壤水定位观测网 杰. 田 et al. 10.1360/N072022-0336
Latest update: 23 Apr 2024
Short summary
The Third Pole regions are important components in the global permafrost, and the detailed spatial soil organic carbon data are the scientific basis for environmental protection as well as the development of Earth system models. Based on multiple environmental variables and soil profile data, this study use machine-learning approaches to evaluate the SOC storage and spatial distribution at a depth interval of 0–3 m in the frozen ground area of the Third Pole region.
The Third Pole regions are important components in the global permafrost, and the detailed...
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