Zihan Jiang

Shandong Normal University

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Trends

Author Order

Document Type

Co-Authors

Ninglian Wang

Northwest University

Li Zhang

Lanzhou University

Qian Zhang

Xi'an Jiaotong University

Chaolu Yi

Tibet University

Gang Hu

Institute of Geology, China Earthquake Administration

Domenico Capolongo

University of Bari Aldo Moro

Jinhua Liu

Hangzhou Normal University

Hanyue Xu

Shandong Normal University

Enshan Yang

Shandong Normal University

Cooperative Institutions

Chinese Academy of Sciences

University of Chinese Academy of Sciences

Shandong Normal University

Institute of Tibetan Plateau Research

Center for Excellence in Tibetan Plateau Earth Sciences

Northwest Institute of Eco-Environment and Resources

Institute of Earth Environment

Northwest University

Science and Technology on Surface Physics and Chemistry Laboratory

Northwest University

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Field

Glaciations and palaeoclimate of the last millennium in the Drongtso Lungpa Co Valley, southeastern Tibetan Plateau, based on cosmogenic 10Be exposure dating and glacier modelling

Journal of Asian Earth Sciences (2023)

Zihan Jiang Gang Hu Chaolu Yi Ninglian Wang Jinhua Liu

Ice core

Cosmogenic nuclide

Surface exposure dating

10.1016/j.jseaes.2023.105777

Cite

Citations (7)

Palaeoclimate Reconstruction of the Central Gangdise Mountains, Southern Tibetan Plateau, Based on Glacier Modelling

Land (2022)

Zihan Jiang Qian Zhang Hanyue Xu Ninglian Wang Li Zhang

Palaeoglacier modelling is an important approach for reconstructing the palaeoclimate. The timing of glaciations in the central part of the Gangdise Mountains has been constrained previously, but the palaeoclimate remains unclear. In this paper, the palaeo-temperature and precipitation of the early marine isotope stage (MIS) 2, the Last Glacial Maximum (LGM), and the early Holocene were reconstructed using coupled mass balance and ice flow models. The results show that a series of temperature changes (ΔT) and precipitation factors (Fp) resulted in optimum palaeoglacial extents. The modelled palaeoglaciers during the early MIS 2, the LGM, and the early Holocene cover areas of ~18.1 km2, ~17.4 km2, and ~16.3 km2, respectively, with ice volumes of ~2.18 km3, ~1.99 km3, and ~1.95 km3, respectively. Previous studies on ice cores, pollen samples, and lake sediments were referenced to narrow the range of palaeo-temperatures and precipitations. The reconstructed temperatures during the early MIS 2, LGM, and early Holocene were constrained to 2.4–2.9 °C, 2.15–3.05 °C, and 0.95–1.5 °C lower than today, respectively. Their precipitation levels were 60–80%, 50–80%, and 100–150% of the present-day level, respectively.

Ice core

Last Glacial Maximum

Marine isotope stage

Paleoclimatology

10.3390/land11081314

Cite

Citations (4)

Palaeoglacier and palaeoclimate reconstruction since the Neoglacial of the central Gangdise Mountains, southern Tibetan Plateau

Palaeogeography Palaeoclimatology Palaeoecology (2024)

Qian Zhang Zihan Jiang Enshan Yang Li Zhang Chaolu Yi

Ice core

Paleoclimatology

10.1016/j.palaeo.2024.112078

Cite

Citations (2)