Zobrazeno 1 - 10
of 169
pro vyhledávání: '"Baotian Pan"'
Autor:
Xiaolu Dong, Xianyan Wang, Long Yang, Zhijun Zhao, Ronald Van Balen, Xiaodong Miao, Tao Liu, Jef Vandenberghe, Baotian Pan, Martin Gibling, Huayu Lu
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-13 (2024)
Abstract Both regular flow and infrequent outburst floods shape the mountain landscape, but their relative contributions have been widely debated, in part due to the paucity of quantitative data on historical outburst floods. In June 2000, an outburs
Externí odkaz:
https://doaj.org/article/2218a125d5e443acaf10d8f6c44b2b2c
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 10, Pp n/a-n/a (2024)
Abstract El Niño‐Southern Oscillation (ENSO) is the most dominant interannual signal of climate variability and profoundly affects river flooding globally, especially in East Asia. However, ENSO also has ∼2,000 and ∼1,000‐year cycles, but du
Externí odkaz:
https://doaj.org/article/06f834fb579a4c468922223937bd9e2a
Autor:
Da Li, Donghui Shangguan, Tianding Han, Asim Qayyum Butt, Baotian Pan, Bo Cao, Meixia Wang, Rongjun Wang, Yaojun Li
Publikováno v:
Remote Sensing, Vol 16, Iss 16, p 3027 (2024)
Lake-terminating glaciers are among the most severely retreating glacier types in high mountain areas. However, the characteristic of being covered by glacial lakes after retreat makes it hard to estimate their actual ice loss in recent years, as doe
Externí odkaz:
https://doaj.org/article/fdc21a7f57184df88868fcff44c3c249
Publikováno v:
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-9 (2023)
The formation of the Chinese Loess Plateau resulted from a combination of surface processes rather than from aridification of the Asian interior alone, according to zircon U-Pb geochronological analysis
Externí odkaz:
https://doaj.org/article/0963fd4cc4f642758dfba76036760d9f
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Rates of river incision are widely used to track changes in rock uplift rate and climate over time and space. However, the relationship between the spatiotemporal variation of river incision and past tectonic or climatic processes is still unclear. H
Externí odkaz:
https://doaj.org/article/2203967e119048708a841b93ecec4e14
Autor:
Zijuan Dong, Baotian Pan, Zhenbo Hu, Qinhong Mo, David Bridgland, Menghao Li, Xiaohua Li, Yanan Yang, Dianbao Chen
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Downstream fining of riverbed gravels is generally linked with the processes of hydraulic sorting and abrasion. Hydraulic sorting is when larger gravel clasts stop moving in response to decreasing flow energy, whereas, finer grains will continue to b
Externí odkaz:
https://doaj.org/article/7dd591eaeea4493584b982a5f21b4c1c
Publikováno v:
Frontiers in Earth Science, Vol 9 (2022)
The North Qilian Shan, located in the northeastern front of the Tibetan Plateau, is an ideal region to study the expansion process of the plateau, which is not clearly revealed due to the lack of direct evidence and an accurate age control. In the Ji
Externí odkaz:
https://doaj.org/article/be1c3a40b4cc4ba18d8565ffb935d0f1
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Glaciers have melted rapidly in the Yarlung Zangbo River Basin due to recent climate change, which has accelerated the expansion of glacial lakes. We performed a systematic survey of glacial lakes in the Yarlung Zangbo River Basin using the Google Ea
Externí odkaz:
https://doaj.org/article/13cb9e02e07149d8a2df5ea33d4fac4d
Autor:
Hansheng Wang, Peng Gao, Rui Yang, Junsheng Nie, Bo Cao, Aifeng Zhou, Baotian Pan, Lin Chen, Tingjiang Peng
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
A clear understanding of the uplift history of the Tibetan Plateau is the key for correctly understanding its uplift mechanisms and impacts on the Asian environment. However, consensus has not been reached regarding the uplift history of the Tibetan
Externí odkaz:
https://doaj.org/article/e52d7ead4b97412b89171b313525af5d
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Although the interactions between biotic and geomorphic processes usually occur on small spatial and short temporal scales, many of the mechanisms remain to be investigated. This study provides the first direct evidence of the interaction between bio
Externí odkaz:
https://doaj.org/article/ae93b0731fab4cfb8ca47e491ddb3cfe