Zobrazeno 1 - 10
of 85
pro vyhledávání: '"Qiuzhen Yin"'
Autor:
Zhengquan Yao, Xuefa Shi, Qiuzhen Yin, Samuel Jaccard, Yanguang Liu, Zhengtang Guo, Sergey A. Gorbarenko, Kunshan Wang, Tianyu Chen, Zhipeng Wu, Qingyun Nan, Jianjun Zou, Hongmin Wang, Jingjing Cui, Anqi Wang, Gongxu Yang, Aimei Zhu, Aleksandr Bosin, Yuriy Vasilenko, Yonggui Yu
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-10 (2024)
Abstract The polar oceans play a vital role in regulating atmospheric CO2 concentrations (pCO2) during the Pleistocene glacial cycles. However, despite being the largest modern reservoir of respired carbon, the impact of the subarctic Pacific remains
Externí odkaz:
https://doaj.org/article/47a0d2ae19804079aac116a6d645f67c
Autor:
Yi Zhong, Yanguang Liu, Hu Yang, Qiuzhen Yin, David J. Wilson, Zhengyao Lu, Samuel L. Jaccard, Torben Struve, Peter D. Clift, Stefanie Kaboth‐Bahr, Juan C. Larrasoaña, André Bahr, Xun Gong, Debo Zhao, Yanan Zhang, Wenyue Xia, Qingsong Liu
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 4, Pp n/a-n/a (2024)
Abstract Airborne mineral dust is sensitive to climatic changes, but its response to orbital forcing is still not fully understood. Here, we present a reconstruction of dust input to the Subarctic Pacific Ocean covering the past 190 kyr. The dust com
Externí odkaz:
https://doaj.org/article/5e33f454fac741dda0195b935bc55c13
Autor:
Tao Li, Gaojun Li, Tianyu Chen, Youbin Sun, Qiuzhen Yin, Zhipeng Wu, Laura F. Robinson, Le Li, Zeke Zhang, Xianqiang Meng, Liang Zhao, Junfeng Ji, Jun Chen
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 3, Pp n/a-n/a (2023)
Abstract It is generally accepted that the glacial‐interglacial variations of the East Asian winter monsoon (EAWM) are controlled by the volume of the Northern Hemisphere ice sheets (NHIS), but the fact that they exhibit different evolution pattern
Externí odkaz:
https://doaj.org/article/68621605c7c44c4d91bfdddb3481f4dc
Autor:
Hai Cheng, Hanying Li, Lijuan Sha, Ashish Sinha, Zhengguo Shi, Qiuzhen Yin, Zhengyao Lu, Debo Zhao, Yanjun Cai, Yongyun Hu, Qingzhen Hao, Jun Tian, Gayatri Kathayat, Xiyu Dong, Jingyao Zhao, Haiwei Zhang
Publikováno v:
The Innovation, Vol 3, Iss 6, Pp 100338- (2022)
The widely accepted “Milankovitch theory” explains insolation-induced waxing and waning of the ice sheets and their effect on the global climate on orbital timescales. In the past half century, however, the theory has often come under scrutiny, e
Externí odkaz:
https://doaj.org/article/866b7b5438b54a89ac37a31c5765f0d1
Autor:
Youbin Sun, Qiuzhen Yin, Michel Crucifix, Steven C. Clemens, Pablo Araya-Melo, Weiguo Liu, Xiaoke Qiang, Qingsong Liu, Hui Zhao, Lianji Liang, Hongyun Chen, Ying Li, Li Zhang, Guocheng Dong, Ming Li, Weijian Zhou, Andre Berger, Zhisheng An
Publikováno v:
Nature Communications, Vol 10, Iss 1, Pp 1-11 (2019)
The mid-Pleistocene transition is recognized as a shift in paleoclimatic periodicity from 41- to 100-kyr cycles. Here the authors present a unique mid-Pleistocene transition of coupled monsoon-vegetation changes from 23- to 100-kyr cycles, which indi
Externí odkaz:
https://doaj.org/article/f048d36392404ff98ddfe0be1ab434f8
Publikováno v:
Climate of the Past, Vol 4, Iss 2, Pp 79-90 (2008)
Deep-sea and ice-core records show that interglacial periods were overall less "warm" before about 420 000 years ago than after, with relatively higher ice volume and lower greenhouse gases concentration. This is particularly the case for the intergl
Externí odkaz:
https://doaj.org/article/14505197d1d948eba064d3559e89e90e
Autor:
Rui Zhang, Qiuzhen Yin, Weihua Nai, Zhixiang Wang, Hao Lu, Chunju Huang, Yansheng Gu, Lin Li, Yusong Wang, Linjing Liu
Publikováno v:
Journal of Earth Science. 34:173-180
Publikováno v:
Climate Dynamics, Vol. 58, no.1-2, p. 1-11 (2022)
Understanding the sea ice variability and the mechanisms involved during warm periods of the Earth is essential for a better understanding of the sea ice changes at the present and in the future. Based on simulations with the model LOVECLIM, this stu
Publikováno v:
QUATERNARY INTERNATIONAL
Quaternary International, Vol. 607, no. 607, p. 100-112 (2021)
Quaternary International, Vol. 607, no. 607, p. 100-112 (2021)
To better understand interglacial paleosol development by quantifying the paleosol development processes on the Chinese Loess Plateau (CLP), we need a soil genesis model calibrated for long timescales. Here, we calibrate a process-based soil genesis
Publikováno v:
Global and Planetary Change, Vol. 222, no.104040, p. 104040 (2023)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2740cf6480f0cc0067e74d738b16c5e6
https://hdl.handle.net/2078.1/272779
https://hdl.handle.net/2078.1/272779