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Sensitivity of climate to late Cenozoic uplift in southern Asia and the American west: Numerical experiments

https://doi.org/10.1029/jd094id15p18393
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What this work says

Outgoing claims: the papers this work cites, builds on, or argues with.

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The dynamical influence of large‐scale heat sources and sinks on the quasi‐stationary mean motions of the atmosphere
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Reduction of systematic forecast errors in the ECMWF model through the introduction of an envelope orography
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A Model Intercomparison for Homogeneous Flow over Large-Scale Orography
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Explanations of the tertiary global cooling trend
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The role of geographic variables in explaining paleoclimates: Results from Cretaceous climate model sensitivity studies
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Late Cenozoic uplift in southern Asia and the American West: Rationale for general circulation modeling experiments
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Forcing of late Cenozoic northern hemisphere climate by plateau uplift in southern Asia and the American west
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A Numerical Method for Predicting the Perturbations of the Middle Latitude Westerlies
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On the Influence of the Earth's Orography on the General Character of the Westerlies
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Stationary Waves of the Ice Age Climate
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Dependence of Warm and Cold Climate Depiction on Climate Model Resolution
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The Effects of Mountains on the General Circulation of the Atmosphere as Identified by Numerical Experiments
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The Role of Mountains in the South Asian Monsoon Circulation
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On Determining the Statistical Significance of Climate Experiments with General Circulation Models
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The Steady Linear Response of a Spherical Atmosphere to Thermal and Orographic Forcing
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January and July Simulations with a Spectral General Circulation Model
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The Response of a Spectral General Circulation Model to Refinements in Radiative Processes
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A General Circulation Model Study of January Climate Anomaly Patterns Associated with Interannual Variation of Equatorial Pacific Sea Surface Temperatures
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The Simulation of Stationary and Transient Geopotential-Height Eddies in January and July with a Spectral General Circulation Model
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The Dynamics of Warm and Cold Climates
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The Effects of Cumulus Moisture Transports on the Simulation of Climate with a General Circulation Model
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Orographically Forced Planetary Waves in the Northern Hemisphere Winter: Steady State Model with Wave-Coupled Lower Boundary Formulation
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Forced Planetary Waves in the Northern Hemisphere Winter: Wave-Coupled Orographic and Thermal Forcings
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Linear Simulation of the Stationary Eddies in a GCM. Part II: The “Mountain” Model
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Planetary Waves Kinematically Forced by Himalayan Orography
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Note on the Theory of Topographically Forced Planetary Waves in the Atmosphere
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The Large-Scale Circulation and Heat Sources over the Tibetan Plateau and Surrounding Areas during the Early Summer of 1979. Part II: Heat and Moisture Budgets
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Effects of Large-Scale Orography on January Atmospheric Circulation: A Numerical Experiment
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A Numerical Method for Predicting the Perturbations of the Middle Latitude Westerlies
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On the Influence of the Earth’s Orography on the General Character of the Westerlies
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Thermal and dynamical effects of orography on the general circulation of the atmosphere

What points at this work

Incoming claims: where this work appears in other papers’ reference lists and arguments.

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Revisit Debate on Paleogene and Neogene East Asian Monsoon
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Identifying trends in climate: an application to the cenozoic
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Vegetation-precipitation controls on Central Andean topography
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A climate threshold at the eastern edge of the Tibetan plateau
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Distinct impacts of the Mongolian and Tibetan Plateaus on the evolution of the East Asian monsoon
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Miocene climate change on the Chinese Loess Plateau: Possible links to the growth of the northern Tibetan Plateau and global cooling
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Precipitation δ18O over the Himalaya‐Tibet orogen from ECHAM5‐wiso simulations: Statistical analysis of temperature, topography and precipitation
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Mineralogical and Geochemical Discrimination of the Occurrence and Genesis of Palygorskite in Eocene Sediments on the Northeastern Tibetan Plateau
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Comparison of the climate effects of surface uplifts from the northern Tibetan Plateau, the Tianshan, and the Mongolian Plateau on the East Asian climate
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Orogenesis and Climate
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Terrain Evolution of China Seas and Land Since the Indo‐China Movement and Characteristics of the Stepped Landform
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Self‐adjustment in rivers: Evidence for least action as the primary control of alluvial‐channel form and process
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Late M iocene magnetostratigraphy of J ianzha B asin in the northeastern margin of the T ibetan P lateau and changes in the E ast A sian summer monsoon
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Magnetostratigraphy of the Dali Basin in Yunnan and implications for late Neogene rotation of the southeast margin of the Tibetan Plateau
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Signatures of Tibetan Plateau heating on Indian summer monsoon rainfall variability
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Effects of the Tibetan Plateau on the onsetof the summer monsoon in South Asia: The role of the air‐sea interaction
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Quantifying the role of paleoclimate and Andean Plateau uplift on river incision
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Impacts of regional uplift of the Tibetan Plateau on local summer precipitation and downstream moisture budget: A simulation study
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Monsoons and the dynamics of deserts
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Modelling the Asian summer monsoon rainfall and Eurasian winter/spring snow mass
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Paleoclimate Modeling, Pre-Quaternary
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Introduction to the Uplift-Climate Connection
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Late Cenozoic Vegetation Change, Atmospheric CO2, and Tectonics
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The Uplift-Climate Connection: A Synthesis
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Mountains and Midlatitude Aridity
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The Effects of Uplift on Ocean-Atmosphere Circulation
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Testing the Climatic Effects of Orography and CO2 with General Circulation and Biome Models
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Effects of the Tibetan Plateau on the Climate of China
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Concluding Remarks and Bibliography
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Sensitivity of East Asian climate to the progressive uplift and expansion of the Tibetan Plateau under the mid-Pliocene boundary conditions
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The role of land-sea distribution and orography in the Asian monsoon. Part II: Orography
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Paleoclimate modeling in China: A review
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Asynchronous responses of East Asian and Indian summer monsoons to mountain uplift shown by regional climate modelling experiments
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Impact of Mongolian Plateau versus Tibetan Plateau on the westerly jet over North Pacific Ocean
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Impacts of dynamic and thermal forcing by the Tibetan Plateau on the precipitation distribution in the Asian arid and monsoon regions
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Enhanced soil respiration, vegetation and monsoon precipitation at Lantian, East Asia during Pliocene warmth
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A framework for regional modeling of past climates
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Major Ion Geochemistry of Nam Co Lake and its Sources, Tibetan Plateau
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Abrupt deglaciation on the northeastern Tibetan Plateau: evidence from Lake Qinghai
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Chronological dating and tectonic implications of late Cenozoic volcanic rocks and lacustrine sequence in Oiyug Basin of southern Tibet
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Late Eocene pollen records and palaeoenvironmental changes in northern Tibetan Plateau
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New eolian red clay sequence on the western Chinese Loess Plateau linked to onset of Asian desertification about 25 Ma ago
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Evolution of the monsoon and dry climate in East Asia during late Cenozoic: A review
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Influence of the Tibetan Plateau uplift on the Asian monsoon-arid environment evolution
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Formation and evolution of sand deserts in Xinjiang, Northwest China: II. The palaeo-environmental reconstruction
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Emergence and extinction of Dipterocarpaceae in western India with reference to climate change: Fossil wood evidences
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Early Paleogene precipitation patterns over East Asia: Was there a monsoon after all?
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Atacamite and nantokite in Kaerqueka copper deposit of Qimantag area: Evidence for Cenozoic climate evolution of the Qaidam Basin
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First Record of Middle Eocene Elephant Ancestors’ Footprints in the Gonjo Basin, East Tibet Plateau
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Holigarna (Anacardiaceae) from the Early Eocene of Western India and its Palaeogeographical and Palaeoclimatological Significance
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Effects of mountain uplift on global monsoon precipitation
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Earth's glacial record and its tectonic setting
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History of terrigenous sedimentation during the past 10 m.y. in the North Atlantic (ODP Legs 104 and 105 and DSDP Leg 81)
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Global change at the Paleocene-Eocene boundary: climatic and evolutionary consequences of tectonic events
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A comparison of Eocene climate model results to quantified paleoclimatic interpretations
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A coupled environmental system formed at about 2.5 Ma in East Asia
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Paleoclimate of the Kimmeridgian/Tithonian (Late Jurassic) world: II. Sensitivity tests comparing three different paleotopographic settings
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Neogene evolution of the Himalayan-Tibetan region: constraints from ODP site 758, northern ninetyeast ridge; bearing on climatic change
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Late Cenozoic environmental changes and uplift on the northern side of the central Himalaya: a reappraisal from field data
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Expansion of C4 grasses in the Late Miocene of Northern Pakistan: evidence from stable isotopes in paleosols
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Evolution of the Norwegian Current and the Scandinavian Ice Sheets during the past 2.6 m.y.: evidence from ODP Leg 104 biogenic carbonate and terrigenous records
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Development of vegetation and continental aridity in northwestern Africa during the Late Pliocene: the pollen record of ODP site 658
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Climate change on tectonic time scales
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Changes in climate and biota on geologic time scales
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Pliocene environments and climates in the western United States
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Modeling pliocene warmth
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Entering the glaciation with A 2-D coupled climate model
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Towards an orbital time scale for chinese loess deposits
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Stepwise coupling of monsoon circulations to global ice volume variations during the late Cenozoic
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Effect of altered Arctic sea ice and Greenland ice sheet cover on the climate of the GENESIS general circulation model
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Late quaternary uplift rates of marine terraces on the Pacific coast of North America, southern Oregon to Baja California sur
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5.6 Plateau Uplift, Regional Warping, and Subsidence
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Plateau Uplift, Regional Warping, and Subsidence
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Utilization of Paleoclimate Results to Validate Projections of a Future Greenhouse Warming
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Mountain Weather: Observation and Modeling
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Impact of massive topography on the dust cycle surrounding the Tibetan Plateau
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Influence of the Tibetan Plateau on the coupling of the North Pacific–North Atlantic pressure systems
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Micromorphological studies of the complex early Oligocene Himalayan foreland palaeosols in relation to Asian monsoon climate
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Evolution of Paleogene weathering intensity in the Qaidam Basin, northeastern Tibetan Plateau: Insights from clay geochemistry
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Multiple forcing on Late Miocene East Asian Summer Monsoon Precipitation Variability in NE Tibetan Plateau
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Goethite in the Red Clay sequences on the western Chinese Loess Plateau and its responses to the middle Miocene Climate Transition
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Cenozoic cooling, Antarctic nutrient pump, and the evolution of whales
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What controlled Mid–Late Miocene long-term aridification in Central Asia? — Global cooling or Tibetan Plateau uplift: A review
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The global monsoon across time scales: Mechanisms and outstanding issues
inferred← citeshttps://doi.org/10.1016/j.earscirev.2019.04.014openalex-snapshot
Formation and evolution of Gobi Desert in central and eastern Asia
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103114openalex-snapshot
Asian Summer Monsoon changes the pollen flow on the Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.earscirev.2024.104964openalex-snapshot
Numerical modelling of coupled climate, tectonics, and surface processes on the eastern Himalayan syntaxis
inferred← citeshttps://doi.org/10.1016/j.earscirev.2025.105298openalex-snapshot
Tectonics dominates exhumation along the Himalayan arc
inferred← citeshttps://doi.org/10.1016/j.epsl.2005.06.036openalex-snapshot
Stepwise expansion of desert environment across northern China in the past 3.5 Ma and implications for monsoon evolution
inferred← citeshttps://doi.org/10.1016/j.epsl.2006.09.049openalex-snapshot
Cenozoic topographic and climatic response to changing tectonic boundary conditions in Western North America
inferred← citeshttps://doi.org/10.1016/j.epsl.2008.07.038openalex-snapshot
Late Neogene evolution of the East Asian monsoon revealed by terrestrial mollusk record in Western Chinese Loess Plateau: From winter to summer dominated sub-regime
inferred← citeshttps://doi.org/10.1016/j.epsl.2009.10.018openalex-snapshot
Integrated climate model-oxygen isotope evidence for a North American monsoon during the Late Cretaceous
inferred← citeshttps://doi.org/10.1016/j.epsl.2010.09.043openalex-snapshot
Middle to late Miocene Middle Eastern climate from stable oxygen and carbon isotope data, southern Alborz mountains, N Iran
inferred← citeshttps://doi.org/10.1016/j.epsl.2010.11.012openalex-snapshot
Empirical relationship between leaf wax n-alkane δD and altitude in the Wuyi, Shennongjia and Tianshan Mountains, China: Implications for paleoaltimetry
inferred← citeshttps://doi.org/10.1016/j.epsl.2011.10.005openalex-snapshot
Isotopic constraints on intensified aridity in Central Asia around 12 Ma
inferred← citeshttps://doi.org/10.1016/j.epsl.2011.12.042openalex-snapshot
On the causes of mid-Pliocene warmth and polar amplification
inferred← citeshttps://doi.org/10.1016/j.epsl.2014.01.003openalex-snapshot
Leaf wax stable isotopes from Northern Tibetan Plateau: Implications for uplift and climate since 15 Ma
inferred← citeshttps://doi.org/10.1016/j.epsl.2017.12.034openalex-snapshot
Changes in Tibetan Plateau latitude as an important factor for understanding East Asian climate since the Eocene: A modeling study
inferred← citeshttps://doi.org/10.1016/j.gca.2005.12.012openalex-snapshot
Pleistocene chemical weathering history of Asian arid and semi-arid regions recorded in loess deposits of China and Tajikistan
inferred← citeshttps://doi.org/10.1016/j.geomorph.2024.109448openalex-snapshot
Pulsed uplift of the South Tianshan since the Late Miocene indicated by the linear inversion on river longitudinal profiles
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2004.01.003openalex-snapshot
Late Miocene and mid-Pliocene enhancement of the East Asian monsoon as viewed from the land and sea
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2008.08.003openalex-snapshot
Surface-water freshening: A cause for the onset of North Pacific stratification from 2.75 Ma onward?
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2011.09.008openalex-snapshot
Magnetostratigraphic and paleoenvironmental records for a Late Cenozoic sedimentary sequence drilled from Lop Nor in the eastern Tarim Basin
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2014.02.006openalex-snapshot
Tibet forcing Quaternary stepwise enhancement of westerly jet and central Asian aridification: Carbonate isotope records from deep drilling in the Qaidam salt playa, NE Tibet
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2014.05.009openalex-snapshot
Cenozoic record of aeolian sediment accumulation and aridification from Lanzhou, China, driven by Tibetan Plateau uplift and global climate
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2015.02.002openalex-snapshot
Evidence of late early Miocene aridification intensification in the Xining Basin caused by the northeastern Tibetan Plateau uplift
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2017.06.006openalex-snapshot
Isotopic composition of gypsum hydration water in deep Core SG-1, western Qaidam basin (NE Tibetan Plateau), implications for paleoclimatic evolution
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2018.07.002openalex-snapshot
High-resolution simulation of Asian monsoon response to regional uplift of the Tibetan Plateau with regional climate model nested with global climate model
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2019.03.005openalex-snapshot
Comparison of climate change from Cenozoic surface uplift and glacial-interglacial episodes in the Himalaya-Tibet region: Insights from a regional climate model and proxy data
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103707openalex-snapshot
Controls of precipitation and vegetation variability on the NE Tibetan Plateau during the late Pliocene warmth (~3.5–3.0 Ma)
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2023.104052openalex-snapshot
The spatial–temporal evolution of the Asian summer monsoon during the late Miocene and potential CO2 forcing: A data–model comparison
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2023.104346openalex-snapshot
Resolving Cenozoic climate pattern debate in East Asia: Insights from orbital-scale oscillations
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104550openalex-snapshot
Middle Pleistocene weakening of the Indian summer monsoon driven by global cooling
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104899openalex-snapshot
Uplift-enhanced Neogene silicate weathering intensity over the northern East Asian summer monsoon region
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105125openalex-snapshot
Tectonic and orbital controls on late Miocene East Asian monsoon variability and aridification in the northeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105324openalex-snapshot
Aridity/humidity fluctuations in the westerlies – Asian monsoon transitional zone since ∼3.4 Ma
inferred← citeshttps://doi.org/10.1016/j.gr.2014.12.007openalex-snapshot
Late Cenozoic genus Fupingopollenites development and its implications for the Asian summer monsoon evolution
inferred← citeshttps://doi.org/10.1016/j.gr.2015.01.007openalex-snapshot
A Late-Eocene palynological record from the Hoh Xil Basin, northern Tibetan Plateau, and its implications for stratigraphic age, paleoclimate and paleoelevation
inferred← citeshttps://doi.org/10.1016/j.gr.2016.05.012openalex-snapshot
Mesozoic litho- and magneto-stratigraphic evidence from the central Tibetan Plateau for megamonsoon evolution and potential evaporites
inferred← citeshttps://doi.org/10.1016/j.jaridenv.2014.01.021openalex-snapshot
Natural ecosystem response and recovery after the 8.2 ka cold event: Evidence from slope sediments on the northeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.jop.2017.08.005openalex-snapshot
Distributional patterns of anemophilous tree pollen indicating the pathways of Indian monsoon through Qinghai–Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.jseaes.2009.12.005openalex-snapshot
Grain size profiles in the Chengdu Clay, eastern margin of the Tibetan Plateau: Implications for significant drying of Asia since ∼500 ka B.P.
inferred← citeshttps://doi.org/10.1016/j.jseaes.2011.04.018openalex-snapshot
Reconciling the Intertropical Convergence Zone, Himalayan/Tibetan tectonics, and the onset of the Asian monsoon system
inferred← citeshttps://doi.org/10.1016/j.jseaes.2011.05.020openalex-snapshot
Late Neogene environmental changes in the central Himalaya related to tectonic uplift and orbital forcing
inferred← citeshttps://doi.org/10.1016/j.jseaes.2011.09.014openalex-snapshot
Eocene monsoons
inferred← citeshttps://doi.org/10.1016/j.jseaes.2012.10.009openalex-snapshot
Major changes in East Asian climate in the mid-Pliocene: Triggered by the uplift of the Tibetan Plateau or global cooling?
inferred← citeshttps://doi.org/10.1016/j.jseaes.2013.07.003openalex-snapshot
Late early Oligocene East Asian summer monsoon in the NE Tibetan Plateau: Evidence from a palynological record from the Lanzhou Basin, China
inferred← citeshttps://doi.org/10.1016/j.jseaes.2014.05.008openalex-snapshot
Timing and extent of Holocene glaciations in the monsoon dominated Dunagiri valley (Bangni glacier), Central Himalaya, India
inferred← citeshttps://doi.org/10.1016/j.jseaes.2015.11.022openalex-snapshot
Miocene woods from the Qaidam Basin on northern Qinghai-Tibet Plateau with implications for paleoenvironmental change
inferred← citeshttps://doi.org/10.1016/j.jseaes.2017.07.008openalex-snapshot
Vegetation and climatic changes during the Middle Miocene in the Wushan Basin, northeastern Tibetan Plateau: Evidence from a high-resolution palynological record
inferred← citeshttps://doi.org/10.1016/j.jseaes.2023.105634openalex-snapshot
Miocene lake evolution in the western Qaidam Basin, northern Tibetan Plateau: Evidence from aquatic-plant pollen
inferred← citeshttps://doi.org/10.1016/j.jseaes.2024.106277openalex-snapshot
A paleomagnetic study of the late paleocene sedimentary succession in the xigaze forearc basin, southern tibet, and its tectonic implications
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2021.105150openalex-snapshot
Rock magnetic evidence of tectonic control on the sedimentation and diagenesis in the Andaman Sea over ~1 million years
inferred← citeshttps://doi.org/10.1016/j.orggeochem.2011.03.019openalex-snapshot
Effect of precipitation regime on δD values of soil n-alkanes from elevation gradients – Implications for the study of paleo-elevation
inferred← citeshttps://doi.org/10.1016/j.palaeo.2006.03.037openalex-snapshot
Reconstructing the Late Miocene climate and oceanic heat flux using the AGCM ECHAM4 coupled to a mixed-layer ocean model with adjusted flux correction
inferred← citeshttps://doi.org/10.1016/j.palaeo.2006.07.009openalex-snapshot
The elevation history of the Tibetan Plateau and its implications for the Asian monsoon
inferred← citeshttps://doi.org/10.1016/j.palaeo.2006.07.016openalex-snapshot
Magnetostratigraphy of the Neogene Sikouzi section at Guyuan, Ningxia, China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2006.08.003openalex-snapshot
What triggers the transition of palaeoenvironmental patterns in China, the Tibetan Plateau uplift or the Paratethys Sea retreat?
inferred← citeshttps://doi.org/10.1016/j.palaeo.2007.09.021openalex-snapshot
Glacio-epochs and the supercontinent cycle after ∼3.0 Ga: Tectonic boundary conditions for glaciation
inferred← citeshttps://doi.org/10.1016/j.palaeo.2007.11.012openalex-snapshot
Stable isotopic variations in modern herbivore tooth enamel, plants and water on the Tibetan Plateau: Implications for paleoclimate and paleoelevation reconstructions
inferred← citeshttps://doi.org/10.1016/j.palaeo.2008.04.016openalex-snapshot
A 20 Ma pollen record of East-Asian summer monsoon evolution from Guyuan, Ningxia, China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2010.11.019openalex-snapshot
Late Eocene sea retreat from the Tarim Basin (west China) and concomitant Asian paleoenvironmental change
inferred← citeshttps://doi.org/10.1016/j.palaeo.2011.07.010openalex-snapshot
Pakistan mammal tooth stable isotopes show paleoclimatic and paleoenvironmental changes since the early Oligocene
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.07.011openalex-snapshot
Paleoclimatic estimation reveals a weak winter monsoon in southwestern China during the late Miocene: Evidence from plant macrofossils
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.06.006openalex-snapshot
A Rb/Sr record of the weathering response to environmental changes in westerly winds across the Tarim Basin in the late Miocene to the early Pleistocene
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.08.014openalex-snapshot
Late Cenozoic sporopollen records in the Yangtze River Delta, East China and implications for East Asian summer monsoon evolution
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.12.022openalex-snapshot
Middle Miocene to earliest Pliocene sedimentological and geochemical records of climate change in the western Qaidam Basin on the NE Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2014.10.030openalex-snapshot
The impact of regional uplift of the Tibetan Plateau on the Asian monsoon climate
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.01.001openalex-snapshot
Late Miocene stepwise aridification in the Asian interior and the interplay between tectonics and climate
inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.09.025openalex-snapshot
Rock magnetic record of late Neogene red clay sediments from the Chinese Loess Plateau and its implications for East Asian monsoon evolution
inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.12.022openalex-snapshot
Effects of the uplifts of the main and marginal Tibetan Plateau on the Asian climate under modern and ~30 Ma boundary conditions
inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.05.040openalex-snapshot
Impacts of the uplift of four mountain ranges on the arid climate and dust cycle of inland Asia
inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.09.009openalex-snapshot
Miocene pollen assemblages from the Zeku Basin, northeastern Tibetan Plateau, and their palaeoecological and palaeoaltimetric implications
inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.10.025openalex-snapshot
Global warming and rainfall: Lessons from an analysis of Mid-Miocene climate data
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109604openalex-snapshot
Iron oxide characteristics of the Chinese loess-red clay sequences and their implications for the evolution of the East Asian summer monsoon since the Late Oligocene
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109903openalex-snapshot
Aridification recorded by lithofacies and grain size in a continuous Pliocene-Quaternary lacustrine sediment record in the western Qaidam Basin, NE Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109949openalex-snapshot
Rock magnetic record of core SG-3 since 1 Ma in the western Qaidam Basin and its paleoclimate implications for the NE Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110437openalex-snapshot
Intensified fire activity induced by aridification facilitated Late Miocene C4 plant expansion in the northeastern Tibetan Plateau, China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110578openalex-snapshot
Isotopic fingerprints of mountain uplift and global cooling in paleoclimatic and paleoecological records from the northern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110609openalex-snapshot
Miocene East Asia summer monsoon precipitation variability and its possible driving forces
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111436openalex-snapshot
East Asian hydroclimate responses to the Eocene-Oligocene transition in the Weihe Basin, central China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111516openalex-snapshot
Landform evolution in Asia during the Cenozoic revealed by formation of drainages of Wei River and Indus River
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.112007openalex-snapshot
Effects of global warming and Tibetan Plateau uplift on East Asian climate during the mid-Cretaceous
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.112009openalex-snapshot
Northward expansion of Cenozoic Asian humid climate recorded by sporopollen
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112174openalex-snapshot
Beidellite as a monomineral index of weathering reveals Eocene climate change in the Qaidam Basin, northeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112225openalex-snapshot
Late Miocene tectonic forcing of climate transition in the northeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112669openalex-snapshot
Bivalve faunal changes in Xunhua Basin shed light on the Late Miocene uplift, cooling and aridification of NE Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.112783openalex-snapshot
Early Oligocene Asian monsoon: Evidence from the Fuping flora of Baise, Guangxi, low-latitude China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.114108openalex-snapshot
Fault activity-induced topographic evolution in the Eastern Himalayan Syntaxis
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.114135openalex-snapshot
Late Miocene pollen record and quantitative paleoclimate and paleoelevation reconstructions for the Jianzha Basin, northeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.palwor.2013.06.001openalex-snapshot
Pollen and fossil wood's linkage with Mi-1 Glaciation in northeastern Tibetan Plateau, China
inferred← citeshttps://doi.org/10.1016/j.palwor.2018.01.003openalex-snapshot
A new fossil wood from the highly diverse early Eocene equatorial forest of Gujarat (western India)
inferred← citeshttps://doi.org/10.1016/j.quageo.2009.02.006openalex-snapshot
OSL chronology of loess deposits in East China and its implications for East Asian monsoon history
inferred← citeshttps://doi.org/10.1016/j.quaint.2008.07.008openalex-snapshot
Influences of subtropical jet and Tibetan Plateau on precipitation pattern in Asia: Insights from regional climate modeling
inferred← citeshttps://doi.org/10.1016/j.quaint.2009.11.039openalex-snapshot
Uplift events of the Qinghai–Tibetan Plateau and environmental evolution of the southwest monsoon since 2.7Ma, recorded in a long lake sediment core from Heqing, China
inferred← citeshttps://doi.org/10.1016/j.quaint.2010.01.002openalex-snapshot
Differences between East Asian and Indian monsoon climate records during MIS3 attributed to differences in their driving mechanisms: Evidence from the loess record in the Sichuan basin, southwestern China and other continental and marine climate records
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