Prosjekter
Publikasjoner
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Vitenskapelig artikkelRevisiting the physical processes controlling the tropical atmospheric circulation changes during the Mid-Piacenzian Warm Period– Quaternary International 2024
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Vitenskapelig artikkelResolving Cenozoic climate pattern debate in East Asia: Insights from orbital-scale oscillations– Global and Planetary Change 2024
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Vitenskapelig artikkelA Model-Data Comparison of the Hydrological Response to Miocene Warmth: Leveraging the MioMIP1 Opportunistic Multi-Model Ensemble– Paleoceanography and Paleoclimatology 2024
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Vitenskapelig artikkelInfluence of plate reference frames on deep-time climate simulations– Global and Planetary Change 2024
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Vitenskapelig artikkelThe emergence of modern zoogeographic regions in Asia examined through climate–dental trait association patterns– Nature Communications 2023
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Vitenskapelig artikkelThe hydrological cycle and ocean circulation of the Maritime Continent in the Pliocene: results from PlioMIP2– Climate of the Past 2023
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Vitenskapelig artikkelBehaviourally modern humans in coastal southern Africa experienced an increasingly continental climate during the transition from Marine Isotope Stage 5 to 4– Frontiers in Earth Science 2023
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Vitenskapelig artikkelGlobal and Zonal-Mean Hydrological Response to Early Eocene Warmth– Paleoceanography and Paleoclimatology 2023
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Vitenskapelig artikkelThe Relationship Between the Global Mean Deep-Sea and Surface Temperature During the Early Eocene– Paleoceanography and Paleoclimatology 2023
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Vitenskapelig artikkelOn the climatic influence of CO2 forcing in the Pliocene– Climate of the Past 2023
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Vitenskapelig artikkelAn early Miocene (∼20 Ma) paleogeographic reconstruction for paleoclimate modelling– Palaeogeography, Palaeoclimatology, Palaeoecology 2023
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Vitenskapelig artikkelSensitivity of coastal southern African climate to changes in coastline position and associated land extent over the last glacial– Quaternary Science Reviews 2023
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Vitenskapelig artikkelUnraveling the mechanisms and implications of a stronger mid-Pliocene Atlantic Meridional Overturning Circulation (AMOC) in PlioMIP2– Climate of the Past 2023
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Vitenskapelig artikkelModelling the 2021 East Asia super dust storm using FLEXPART and FLEXDUST and its comparison with reanalyses and observations– Frontiers in Environmental Science 2023
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Vitenskapelig artikkelTibetan Plateau Made Central Asian Drylands Move Northward, Concentrate in Narrow Latitudinal Bands, and Increase in Intensity During the Cenozoic– Geophysical Research Letters 2022
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Vitenskapelig artikkelDistinct effects of Tibetan Plateau growth and global cooling on the eastern and central Asian climates during the Cenozoic– Global and Planetary Change 2022
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Vitenskapelig artikkelRecognizing the Role of Tropical Seaways in Modulating the Pacific Circulation– Geophysical Research Letters 2022
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Vitenskapelig artikkelMid-Pliocene El Niño/Southern Oscillation suppressed by Pacific intertropical convergence zone shift– Nature Geoscience 2022
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Vitenskapelig artikkelImpact of Mountains in Southern China on the Eocene Climates of East Asia– Journal of Geophysical Research (JGR): Atmospheres 2022
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Vitenskapelig artikkelPreceding winter Okhotsk Sea ice as a precursor to the following winter extreme precipitation in South China– Atmospheric Science Letters 2022
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Vitenskapelig artikkelAfrican Hydroclimate During the Early Eocene From the DeepMIP Simulations– Paleoceanography and Paleoclimatology 2022
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Vitenskapelig artikkelPast terrestrial hydroclimate sensitivity controlled by Earth system feedbacks– Nature Communications 2022
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Vitenskapelig artikkelWidespread glacier advances across the Tian Shan during Marine Isotope Stage 3 not supported by climate-glaciation simulations– Fundamental Research 2022
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Vitenskapelig artikkelDivergent Evolution of Glaciation Across High-Mountain Asia During the Last Four Glacial-Interglacial Cycles– Geophysical Research Letters 2021
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Vitenskapelig artikkelSimulating Miocene Warmth: Insights From an Opportunistic Multi-Model Ensemble (MioMIP1)– Paleoceanography and Paleoclimatology 2021
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Vitenskapelig artikkelEffects of Tibetan Plateau Growth, Paratethys Sea Retreat and Global Cooling on the East Asian Climate by the Early Miocene– Geochemistry Geophysics Geosystems 2021
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Vitenskapelig artikkelComplex network of synchronous climate events in East Asian tree-ring data– Climatic Change 2021
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Vitenskapelig oversiktsartikkelThe Eocene-Oligocene transition: A review of marine and terrestrial proxy data, models and model-data comparisons– Climate of the Past 2021
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Vitenskapelig artikkelMid-Pliocene West African Monsoon rainfall as simulated in the PlioMIP2 ensemble– Climate of the Past 2021
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Vitenskapelig artikkelMid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2– Climate of the Past 2021
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Vitenskapelig artikkelEvaluating the large-scale hydrological cycle response within the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2) ensemble– Climate of the Past 2021
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Vitenskapelig artikkelDocumented and Simulated Warm Extremes during the Last 600 Years over Monsoonal China– Atmosphere 2021
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Vitenskapelig artikkelA modeling study of the tripole pattern of East China precipitation over the past 425 ka– Journal of Geophysical Research (JGR): Atmospheres 2021
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Vitenskapelig artikkelThe Eocene-Oligocene transition: a review of marine and terrestrial proxy data, models and model-data comparisons– Climate of the Past 2021
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Vitenskapelig artikkelDeepMIP: model intercomparison of early Eocene climatic optimum (EECO) large-scale climate features and comparison with proxy data– Climate of the Past 2021
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Vitenskapelig artikkelLarge-scale features of Last Interglacial climate: results from evaluating the lig127k simulations for the Coupled Model Intercomparison Project (CMIP6)–Paleoclimate Modeling Intercomparison Project (PMIP4)– Climate of the Past 2021
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Vitenskapelig artikkelA multi-model CMIP6-PMIP4 study of Arctic sea ice at 127 ka: sea ice data compilation and model differences– Climate of the Past 2021
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Vitenskapelig artikkelLarge-scale features and evaluation of the PMIP4-CMIP6 midHolocene simulations– Climate of the Past 2020
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Vitenskapelig artikkelRapid waxing and waning of Beringian ice sheet reconcile glacial climate records from around North Pacific– Climate of the Past 2020
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Vitenskapelig artikkelLarge shift of the Pacific Walker Circulation across the Cenozoic– National Science Review 2020
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Vitenskapelig artikkelDeciphering the evolution and forcing mechanisms of glaciation over the Himalayan-Tibetan orogen during the past 20,000 years– Earth and Planetary Science Letters 2020
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Vitenskapelig artikkelComparison of past and future simulations of ENSO in CMIP5/PMIP3 and CMIP6/PMIP4 models– Climate of the Past 2020
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Vitenskapelig artikkelOverview of the Norwegian Earth System Model (NorESM2) and key climate response of CMIP6 DECK, historical, and scenario simulations– Geoscientific Model Development 2020
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Vitenskapelig artikkelDrier tropical and subtropical Southern Hemisphere in the mid-Pliocene Warm Period– Scientific Reports 2020
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Vitenskapelig artikkelThe Pliocene Model Intercomparison Project Phase 2: large-scale climate features and climate sensitivity– Climate of the Past 2020
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Vitenskapelig artikkelLessons from a high-CO2 world: an ocean view from ∼ 3 million years ago– Climate of the Past 2020
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Vitenskapelig artikkelEvaluation of Arctic warming in mid-Pliocene climate simulations– Climate of the Past 2020
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Vitenskapelig artikkelPlioMIP2 simulations with NorESM-L and NorESM1-F– Climate of the Past 2020
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Vitenskapelig artikkelTWO CLIMATE MODEL SIMULATION OF MIS 5E CLIMATE IN CHINA– Quaternary Sciences 2019
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Vitenskapelig artikkelOrbitally induced variation of tropical cyclone genesis potential Over the western north Pacific during the Mid-Piacenzian warm period: A modeling perspective– Paleoceanography and Paleoclimatology 2019
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Vitenskapelig artikkelSome illustrations of large tectonically driven climate changes in Earth history– Tectonics 2019
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Vitenskapelig artikkelModeling the late Pliocene global monsoon response to individual boundary conditions– Climate Dynamics 2019
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Vitenskapelig artikkelReconstructing early Eocene (~55 Ma) paleogeographic boundary conditions for use in paleoclimate modelling– Science China. Earth Sciences 2019
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Vitenskapelig artikkelPotential impacts of enhanced tropical cyclone activity on the El Ni?o?Southern Oscillation and East Asian monsoon in the mid-Piacenzian warm period– Atmospheric and Oceanic Science Letters 2019
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Vitenskapelig artikkelVegetation and Ocean Feedbacks on the Asian Climate Response to the Uplift of the Tibetan Plateau– Journal of Geophysical Research (JGR): Space Physics 2019
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Vitenskapelig artikkelEvolution of tropical cyclone genesis regions during the Cenozoic era– Nature Communications 2019
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Vitenskapelig artikkelEquilibrium simulations of Marine Isotope Stage 3 climate– Climate of the Past 2019
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Vitenskapelig artikkelReexamination of the Late Pliocene Climate over China Using a 25-km Resolution General Circulation Model– Journal of Climate 2019
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Vitenskapelig artikkelInstability of Northeast Siberian ice sheet during glacials– Climate of the Past 2018
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Vitenskapelig artikkelGlobal Cooling Contributed to the Establishment of a Modern-Like East Asian Monsoon Climate by the Early Miocene– Geophysical Research Letters 2018
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Vitenskapelig artikkelEffects of the uplifts of the main and marginal Tibetan Plateau on the Asian climate under modern and ~30 Ma boundary conditions– Palaeogeography, Palaeoclimatology, Palaeoecology 2018
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Vitenskapelig artikkelInvestigating Sensitivity of East Asian Monsoon to Orbital Forcing During the Late Pliocene Warm Period– Journal of Geophysical Research (JGR): Space Physics 2018
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Vitenskapelig artikkelClimate Constraints on Glaciation Over High-Mountain Asia During the Last Glacial Maximum– Geophysical Research Letters 2018
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Vitenskapelig artikkelDo climate simulations support the existence of East Asian monsoon climate in the Late Eocene?– Palaeogeography, Palaeoclimatology, Palaeoecology 2018
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Vitenskapelig artikkelHigh-resolution simulation of Asian monsoon response to regional uplift of the Tibetan Plateau with regional climate model nested with global climate model– Global and Planetary Change 2018
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Vitenskapelig artikkelChanges in Tibetan Plateau latitude as an important factor for understanding East Asian climate since the Eocene: A modeling study– Earth and Planetary Science Letters 2018
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Vitenskapelig artikkelAtlantic deep water circulation during the last interglacial– Scientific Reports 2018
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KonferanseforedragThe Atlantic deep water circulation during the last interglacial– Ocean Sciences Meeting 2018 2018
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Vitenskapelig artikkelWhat enhanced the aridity in Eocene Asian inland: Global cooling or early Tibetan Plateau uplift?– Palaeogeography, Palaeoclimatology, Palaeoecology 2018
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Vitenskapelig artikkelDominating roles of ice sheets and insolation in variation of tropical cyclone genesis potential over the North Atlantic during the last 21,000 years– Geophysical Research Letters 2017
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Vitenskapelig artikkelDivergent responses of tropical cyclone genesis factors to strong volcanic eruptions at different latitudes– Climate Dynamics 2017
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Vitenskapelig artikkelVariations in large-scale tropical cyclone genesis factors over the western North Pacific in the PMIP3 last millennium simulations– Climate Dynamics 2017
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Vitenskapelig artikkelComparison of the climate effects of surface uplifts from the northern Tibetan Plateau, the Tianshan, and the Mongolian Plateau on the East Asian climate– Journal of Geophysical Research (JGR): Atmospheres 2017
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Vitenskapelig artikkelExploring the MIS M2 glaciation occurring during a warm and high atmospheric CO2 Pliocene background climate– Earth and Planetary Science Letters 2017
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Vitenskapelig artikkelTropical cyclone genesis factors in a simulation of the last two millennia: Results from community earth system model– Journal of Climate 2016
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Vitenskapelig artikkelEnhanced intensity of global tropical cyclones during the mid-Pliocene warm period– Proceedings of the National Academy of Sciences of the United States of America 2016
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Vitenskapelig artikkelStrengthened African summer monsoon in the mid-Piacenzian– Advances in Atmospheric Sciences 2016
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Vitenskapelig artikkelArctic sea ice simulation in the PlioMIP ensemble– Climate of the Past 2016
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KonferanseforedragMid-Pliocene simulations with the new version of the Norwegian Earth System Model– PlioMIP Phase II 2016
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Vitenskapelig artikkelInvestigating uncertainty in the simulation of the Antarctic ice sheet during the mid-Piacenzian– Journal of Geophysical Research (JGR): Biogeosciences 2016
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Vitenskapelig artikkelDrivers and mechanisms for enhanced summer monsoon precipitation over East Asia during the mid-Pliocene in the IPSL-CM5A– Climate Dynamics 2016
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Vitenskapelig artikkelUsing results from the PlioMIP ensemble to investigate the Greenland Ice Sheet during the mid-Pliocene Warm Period– Climate of the Past 2015
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Vitenskapelig artikkelSimulated warm periods of climate over China during the last two millennia: The Sui-Tang warm period versus the Song-Yuan warm period– Journal of Geophysical Research (JGR): Biogeosciences 2015
