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1
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Sun G, Mu M. Impacts of two types of errors on the predictability of terrestrial carbon cycle. Ecosphere 2021. [DOI: 10.1002/ecs2.3315] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/11/2022] Open
Affiliation(s)
- Guodong Sun
- State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG) Institute of Atmospheric Physics Chinese Academy of Sciences Beijing100029China
- University of Chinese Academy of Sciences Beijing100049China
| | - Mu Mu
- Institute of Atmospheric Sciences Fudan University Shanghai200438China
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2
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Huang W, Liu C, Cao J, Chen J, Feng S. Changes of hydroclimatic patterns in China in the present day and future. Sci Bull (Beijing) 2020; 65:1061-1063. [PMID: 36659156 DOI: 10.1016/j.scib.2020.03.033] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/21/2020] [Revised: 02/27/2020] [Accepted: 02/28/2020] [Indexed: 01/21/2023]
Affiliation(s)
- Wei Huang
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China.
| | - Chang Liu
- Department of Geosciences, University of Arkansas, Fayetteville, AR 72701, USA
| | - Jinqiu Cao
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
| | - Jianhui Chen
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
| | - Song Feng
- Department of Geosciences, University of Arkansas, Fayetteville, AR 72701, USA
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3
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Li F, Liu J, Chen G, Kong L, Zhang X. A rapid late Holocene lake ecosystem shift driven by climate change: evidence from the first cladoceran record from an alpine lake in northern China. Sci Bull (Beijing) 2020; 65:253-256. [PMID: 36659085 DOI: 10.1016/j.scib.2019.12.010] [Citation(s) in RCA: 8] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/14/2019] [Revised: 12/04/2019] [Accepted: 12/06/2019] [Indexed: 01/21/2023]
Affiliation(s)
- Fanyi Li
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
| | - Jianbao Liu
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China; Key Laboratory of Alpine Ecology, Center for Excellence in Tibetan Plateau Earth Sciences, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China.
| | - Guangjie Chen
- Yunnan Key Laboratory of Plateau Geographical Processes and Environmental Change, School of Tourism and Geography, Yunnan Normal University, Kunming 650000, China
| | - Lingyang Kong
- Yunnan Key Laboratory of Plateau Geographical Processes and Environmental Change, School of Tourism and Geography, Yunnan Normal University, Kunming 650000, China
| | - Xiaosen Zhang
- Institute of Loess Plateau, Shanxi University, Taiyuan 030006, China
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4
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Zhu Y, Jia X, Qiao J, Shao M. What is the mass of loess in the Loess Plateau of China? Sci Bull (Beijing) 2019; 64:534-539. [PMID: 36659743 DOI: 10.1016/j.scib.2019.03.021] [Citation(s) in RCA: 17] [Impact Index Per Article: 3.4] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/21/2019] [Revised: 03/12/2019] [Accepted: 03/13/2019] [Indexed: 01/21/2023]
Abstract
The Loess Plateau of China (LP) has the largest and thickest loess deposits in the world. Quantifying the amount of loess in the LP is crucial for investigating the accumulation and erosion of loess, and determining the regional soil and water resource capacity. We used loess thickness data, a pedotransfer function for bulk density (BD), and the clay content data observed in 242 sites across the LP to derive the BD of loess and then estimate the loess mass and its distribution across the LP. The results indicated that the average BD of loess between the surface and bedrock is 1.58 g cm-3, varying from 1.18 to 1.87 g cm-3. The total loess mass is approximately 5.45 × 1013 t, and the average loess mass over an area of 1 m2 is 169 t, ranging from 1.36 to 585 t. The greatest mass of loess is in the south-central of the LP while the lowest mass of loess is in the northwest and river valley areas. Our estimate of loess mass provides key data for calculating water, carbon, and nutrient storages in the LP, which improves our understanding of soil-water processes and ecohydrological systems in this landscape.
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Affiliation(s)
- Yuanjun Zhu
- State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling 712100, China; Institute of Soil and Water Conservation, Chinese Academy of Sciences & Ministry of Water Resources, Yangling 712100, China; College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100190, China.
| | - Xiaoxu Jia
- Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100190, China
| | - Jiangbo Qiao
- State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling 712100, China
| | - Ming'an Shao
- State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling 712100, China; Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; Institute of Soil and Water Conservation, Chinese Academy of Sciences & Ministry of Water Resources, Yangling 712100, China; College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100190, China
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5
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Huang W, Yan J, Liu C, Xie T. Changes in climate regimes over China based on a high-resolution dataset. Sci Bull (Beijing) 2019; 64:377-379. [PMID: 36659727 DOI: 10.1016/j.scib.2019.03.001] [Citation(s) in RCA: 6] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/21/2019] [Revised: 02/10/2019] [Accepted: 02/18/2019] [Indexed: 01/21/2023]
Affiliation(s)
- Wei Huang
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China; Central Asia Center for Atmospheric Science Research, China Meteorological Administration, Urumqi 830002, China.
| | - Jingjing Yan
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
| | - Chang Liu
- Department of Geosciences, University of Arkansas, Fayetteville, AR 72703, USA
| | - Tingting Xie
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
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6
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Chen J, Zhang Z, Liu J, Rao Z, Huang W, Zhang X, Chen S. "North-South" dipolar mode of precipitation changes in eastern China extends to the Last Deglaciation. Sci Bull (Beijing) 2018; 63:1604-1605. [PMID: 36658849 DOI: 10.1016/j.scib.2018.12.005] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/21/2023]
Affiliation(s)
- Jianhui Chen
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China.
| | - Zhiping Zhang
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
| | - Jianbao Liu
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China; Key Laboratory of Alpine Ecology and Biodiversity (LAEB), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; Center for Excellence in Tibetan Plateau Earth System Sciences, Chinese Academy of Sciences, Beijing 100101, China.
| | - Zhiguo Rao
- College of Resources and Environmental Sciences, Hunan Normal University, Changsha 410081, China
| | - Wei Huang
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
| | - Xu Zhang
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China; Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven 27570, Germany
| | - Shengqian Chen
- Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
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