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Differential ice volume and orbital modulation of Quaternary moisture patterns between Central and East Asia

Earth and planetary science letters, 2020-01, Vol.530, p.115901, Article 115901

2020

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A persistent Holocene wetting trend in arid central Asia, with wettest conditions in the late Holocene, revealed by multi-proxy analyses of loess-paleosol sequences in Xinjiang, China

Quaternary science reviews, 2016-08, Vol.146, p.134-146

2016

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Variations in the westerlies in Central Asia since 16 ka recorded by a loess section from the Tien Shan Mountains

Palaeogeography, palaeoclimatology, palaeoecology, 2018-09, Vol.504, p.156-161

2018

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Variations in the Iron Mineralogy of a Loess Section in Tajikistan During the Mid‐Pleistocene and Late Pleistocene: Implications for the Climatic Evolution in Central Asia

Geochemistry, geophysics, geosystems : G3, 2018-04, Vol.19 (4), p.1244-1258

2018

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Seasonality of Response to Millennial‐Scale Climate Events of the Last Glacial: Evidence From Loess Records Over Mid‐Latitude Asia

Geochemistry, geophysics, geosystems : G3, 2021-10, Vol.22 (10), p.n/a

2021

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Holocene aeolian dust accumulation rates across the Chinese Loess Plateau

Global and planetary change, 2022-01, Vol.208, p.103720, Article 103720

2022

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Dust Sources of Last Glacial Chinese Loess Based on the Iron Mineralogy of Fractionated Source Samples

Geophysical research letters, 2019-02, Vol.46 (4), p.2103-2110

2019

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Source of the aeolian sediments in the Yarlung Tsangpo valley and its potential dust contribution to adjacent oceans

Earth surface processes and landforms, 2022-06, Vol.47 (7), p.1860-1871

2022

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Paleoclimatic changes and modulation of East Asian summer monsoon by high-latitude forcing over the last 130,000 years as revealed by independently dated loess-paleosol sequences on the NE Tibetan Plateau

Quaternary science reviews, 2020-06, Vol.237, p.106283, Article 106283

2020

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Spatial-temporal differentiation of eolian sediments in the Yarlung Tsangpo catchment, Tibetan Plateau, and response to global climate change since the Last Glaciation

Geomorphology (Amsterdam, Netherlands), 2020-05, Vol.357, p.107104, Article 107104

2020

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A Tianshan Mountains loess-paleosol sequence indicates anti-phase climatic variations in arid central Asia and in East Asia

Earth and planetary science letters, 2018-07, Vol.494, p.153-163

2018

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General Holocene warming trend in arid Central Asia indicated by soil isoprenoid tetraethers

Global and planetary change, 2022-08, Vol.215, p.103879, Article 103879

2022

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Differentiating detrital and pedogenic contributions to the magnetic properties of aeolian deposits in the southern Tibetan Plateau: Implications for paleoclimatic reconstruction

Catena (Giessen), 2023-01, Vol.220, p.106736, Article 106736

2023

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Asynchronous Holocene Climate Optimum across mid-latitude Asia

Palaeogeography, palaeoclimatology, palaeoecology, 2019-03, Vol.518, p.206-214

2019

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Millennial-scale climate oscillations over the last two climatic cycles revealed by a loess–paleosol sequence from central Asia

Journal of Asian earth sciences, 2022-12, Vol.240, p.105435, Article 105435

2022

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Increased late Holocene dust activity revealed by loess accumulation rates in Central Asia

Global and planetary change, 2024-05, Vol.236, p.104416, Article 104416

2024

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Southward shift of the Westerlies during Heinrich Event 2: Evidence from loess deposits in Central Asia

Palaeogeography, palaeoclimatology, palaeoecology, 2023-11, Vol.630, p.111815, Article 111815

2023

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Spatiotemporal differences in Holocene climate change in the Yarlung Tsangpo catchment, southern Tibetan Plateau, reconstructed from two sandy loess sequences

Palaeogeography, palaeoclimatology, palaeoecology, 2023-04, Vol.616, p.111473, Article 111473

2023

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Bond events in the Tarim Basin: The loess record

Quaternary international, 2023-01, Vol.643, p.73-80

2023

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Transformation of lakebed into a major soluble-salt-bearing dust source for Asia since the mid-pleistocene

Global and planetary change, 2023-11, Vol.230, p.104282, Article 104282

2023

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No evidence for an anti-phased Holocene moisture regime in mountains and basins in Central Asian: Records from Ili loess, Xinjiang

Palaeogeography, palaeoclimatology, palaeoecology, 2021-06, Vol.572, p.110407, Article 110407

2021

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Urban particle size distributions during two contrasting dust events originating from Taklimakan and Gobi Deserts

Environmental pollution (1987), 2015-12, Vol.207, p.107-122

2015

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Middle to late Holocene climate change in the monsoon-dominated southeastern Tibetan Plateau and its relationship with human activity

Palaeogeography, palaeoclimatology, palaeoecology, 2024-07, Vol.645, p.112209, Article 112209

2024

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Holocene forcing of aeolian dust activity over the Tibetan Plateau and its surroundings

Global and planetary change, 2024-04, Vol.235, p.104400, Article 104400

2024

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The magnetic susceptibility recorded millennial-scale variability in central Asia during last glacial and interglacial

Geophysical journal international, 2018-12, Vol.215 (3), p.1781-1788

2018

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Differential ice volume and orbital modulation of Quaternary moisture patterns between Central and East Asia

A persistent Holocene wetting trend in arid central Asia, with wettest conditions in the late Holocene, revealed by multi-proxy analyses of loess-paleosol sequences in Xinjiang, China

Variations in the westerlies in Central Asia since 16 ka recorded by a loess section from the Tien Shan Mountains

Variations in the Iron Mineralogy of a Loess Section in Tajikistan During the Mid‐Pleistocene and Late Pleistocene: Implications for the Climatic Evolution in Central Asia

Seasonality of Response to Millennial‐Scale Climate Events of the Last Glacial: Evidence From Loess Records Over Mid‐Latitude Asia

Holocene aeolian dust accumulation rates across the Chinese Loess Plateau

Dust Sources of Last Glacial Chinese Loess Based on the Iron Mineralogy of Fractionated Source Samples

Source of the aeolian sediments in the Yarlung Tsangpo valley and its potential dust contribution to adjacent oceans

Paleoclimatic changes and modulation of East Asian summer monsoon by high-latitude forcing over the last 130,000 years as revealed by independently dated loess-paleosol sequences on the NE Tibetan Plateau

Spatial-temporal differentiation of eolian sediments in the Yarlung Tsangpo catchment, Tibetan Plateau, and response to global climate change since the Last Glaciation

A Tianshan Mountains loess-paleosol sequence indicates anti-phase climatic variations in arid central Asia and in East Asia

General Holocene warming trend in arid Central Asia indicated by soil isoprenoid tetraethers

Differentiating detrital and pedogenic contributions to the magnetic properties of aeolian deposits in the southern Tibetan Plateau: Implications for paleoclimatic reconstruction

Asynchronous Holocene Climate Optimum across mid-latitude Asia

Millennial-scale climate oscillations over the last two climatic cycles revealed by a loess–paleosol sequence from central Asia

Increased late Holocene dust activity revealed by loess accumulation rates in Central Asia

Southward shift of the Westerlies during Heinrich Event 2: Evidence from loess deposits in Central Asia

Spatiotemporal differences in Holocene climate change in the Yarlung Tsangpo catchment, southern Tibetan Plateau, reconstructed from two sandy loess sequences

Bond events in the Tarim Basin: The loess record

Transformation of lakebed into a major soluble-salt-bearing dust source for Asia since the mid-pleistocene

No evidence for an anti-phased Holocene moisture regime in mountains and basins in Central Asian: Records from Ili loess, Xinjiang

Urban particle size distributions during two contrasting dust events originating from Taklimakan and Gobi Deserts

Middle to late Holocene climate change in the monsoon-dominated southeastern Tibetan Plateau and its relationship with human activity

Holocene forcing of aeolian dust activity over the Tibetan Plateau and its surroundings

The magnetic susceptibility recorded millennial-scale variability in central Asia during last glacial and interglacial

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