Chaolu Yi

Biographic Data

ID	4019122
NAME	Chaolu Yi
GIVEN NAMES	Chaolu
FAMILY NAME	Yi
SIGNATURE	YI C
AFFILIATIONS	Institute of Tibetan Plateau Research
VERIFIED	No
TOTAL WORKS	22
TOTAL CITATIONS	2
WORKS AS AUTHOR	22
WORKS AS EDITOR	0
FIRST PUBLICATION YEAR	2002
LATEST PUBLICATION YEAR	2021
H-INDEX	1

Extensive glaciations between MIS 8 and MIS 5 on the eastern side of the Guliya ice cap, West Kunlun Mountains
Open AccessXuezhen Zeng, Xiangke Xu et al.ARTICLEQuaternary International2021
Glacial events during the last glacial termination in the Pagele valley, Qiongmu Gangri peak, southern Tibetan Plateau, and their links to oceanic and atmospheric circulation
Open AccessXiangke Xu, Tandong Yao et al.ARTICLEQuaternary Research2020
During the last glacial termination, a warming trend was generally interrupted by rapid millennium-scale cold reversals, such as the Greenland (Isotope) Stadial 1 (GS-1) and GS-2a events. To understand how glaciers on the Tibetan Plateau (TP) responded to these rapid climate events, this study constrained the timing and extent of three glacial events during the late-glacial period. Specifically, using a cosmogenic 10 Be exposure dating method, we…
Glacier status during the period 1973–2014 in the Hunza Basin, Western Karakoram
Open AccessMuhammad Ateeq Qureshi, Chaolu Yi et al.ARTICLEQuaternary International2017
Extensive glacial advances during the Last Glacial Maximum near the eastern Himalayan syntaxis
Open AccessGang Hu, Chaolu Yi et al.ARTICLEQuaternary International2017
Timing and configuration of the Gongga II glaciation in the Hailuogou valley, eastern Tibetan Plateau
Open AccessXiangke Xu, Chaolu YiARTICLEQuaternary International2017
Reconstruction of Little Ice Age glacier area and equilibrium line attitudes in the central and western Himalaya
Open AccessBaojin Qiao, Chaolu YiARTICLEQuaternary International2017
Cosmogenic 10 Be surface exposure dating of ‘Little Ice Age’ glacial events in the Mount Jaggang area, central Tibet
Open AccessGuocheng Dong, Weijian Zhou et al.ARTICLEThe Holocene2017Cited by: 2References: 12
The timing and extent of ‘Little Ice Age’ (LIA) glacial advances on the Tibetan Plateau (TP) are critical for understanding climate during the past millennium. However, the lack of LIA chronologies in central Tibet makes it difficult to fully understand the nature of LIA throughout the TP. In this study, two presumed LIA moraines in the east of Mount Jaggang, Xainza range, the central TP, were examined and dated using 10 Be surface exposure datin…
Distribution and formation of monohydrocalcite from surface sediments in Nam Co Lake, Tibet
Open AccessMinghui Li, Junbo Wang et al.ARTICLEQuaternary International2012
Late Quaternary deposition and incision sequences of the Golmud River and their environmental implications
Open AccessYixin Chen, Yingkui Li et al.ARTICLEQuaternary International2011
Quaternary paleoenvironmental change and landscape development in Tibet and the bordering mountains
Open AccessChaolu Yi, Jason M Dortch et al.ARTICLEQuaternary International2011
Properties and periglacial processes in alpine meadow soils, western Nyainqentanglha Mountains, Tibet
Open AccessLiqiang Wang, Chaolu YiARTICLEQuaternary International2011
Multiple implications of rare earth elements for Holocene environmental changes in Nam Co, Tibet
Open AccessMinghui Li, Liping Zhu et al.ARTICLEQuaternary International2011
Climate change since 11.5 ka on the Diancang Massif on the southeastern margin of the Tibetan Plateau
Open AccessJiangqiang Yang, Wei Zhang et al.ARTICLEQuaternary Research2010
The Diancang Massif is located in a region linking the Tibetan and Yungui Plateaus. Climatically, it is in a transition belt between the south and middle subtropical zones, controlled by Indian monsoon and westerlies. Thus, this study provides more evidences on the evolution of Indian monsoon since the Holocene. We reconstruct the history of climate on the Diancang Massif since 11.5 ka, using integrated correlation of glacial activities, early hu…
Evaporite minerals and geochemistry of the upper 400m sediments in a core from the Western Qaidam Basin, Tibet
Open AccessMinghui Li, Xiaomin Fang et al.ARTICLEQuaternary International2010
Quaternary paleoenvironmental change in Tibet and the bordering mountains
Open AccessChaolu Yi, Lewis A OwenARTICLEQuaternary International2006
A lateglacial rock avalanche event, Tianchi Lake, Tien Shan, Xinjiang
Open AccessChaolu Yi, Ling Zhu et al.ARTICLEQuaternary International2006
Late Pleistocene glaciation of the Diancang and Gongwang Mountains, southeast margin of the Tibetan plateau
Open AccessJianqiang Yang, Wei Zhang et al.ARTICLEQuaternary International2006
Fabric analysis of till clasts in the upper Urumqi River, Tian Shan, China
Open AccessDewen Li, Chaolu Yi et al.ARTICLEQuaternary International2006
Formation of proglacial dunes in front of the Puruogangri Icefield in the central Qinghai–Tibet Plateau
Open AccessXiaoze Li, Chaolu Yi et al.ARTICLEQuaternary International2006
AMS radiocarbon dating of late Quaternary glacial landforms, source of the Urumqi River, Tien Shan—a pilot study of 14C dating on inorganic carbon
Open AccessChaolu Yi, Kexin Liu et al.ARTICLEQuaternary International2004
ESR dating of the sediments of the Last Glaciation at the source area of the Urumqi River, Tian Shan Mountains, China
Open AccessChaolu Yi, Keqing Jiao et al.ARTICLEQuaternary International2002
Quaternary glaciation of Puruogangri—the largest modern ice field in Tibet
Open AccessChaolu Yi, Xiaoze Li et al.ARTICLEQuaternary International2002