Monsoon changes for 6000 years ago: Results of 18 simulations from the Paleoclimate Modeling Intercomparison Project (PMIP)
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Climate-driven ecosystem succession in the Sahara: the past 6000 years.Shortwave forcing and feedbacks in Last Glacial Maximum and Mid-Holocene PMIP3 simulations.Simulation of intense monsoons under glacial conditionsUsing the past to constrain the future: how the palaeorecord can improve estimates of global warmingEvaluation of CMIP5 palaeo-simulations to improve climate projectionsMid-Holocene and last glacial maximum climate simulations with the IPSL model: part II: model-data comparisonsRelative impacts of insolation changes, meltwater fluxes and ice sheets on African and Asian monsoons during the HoloceneTropical Pacific climate at the mid-Holocene and the Last Glacial Maximum simulated by a coupled ocean-atmosphere general circulation modelRegional energy budget control of the intertropical convergence zone and application to mid-Holocene rainfallClimate model benchmarking with glacial and mid-Holocene climatesMid-Holocene monsoons: a multi-model analysis of the inter-hemispheric differences in the responses to orbital forcing and ocean feedbacksComparison of palaeoclimate simulations enhances confidence in modelsMid-Holocene and glacial-maximum vegetation geography of the northern continents and AfricaPollen-based biomes for Beringia 18,000, 6000 and 0 14C yr bp +Very high resolution rainfall patterns measured by TRMM precipitation radar: seasonal and diurnal cyclesBiome changes in Asia since the mid-Holocene – an analysis of different transient Earth system model simulationsMulti vegetation model evaluation of the Green Sahara climate regimeSeasonally asymmetric transition of the Asian monsoon in response to ice age boundary conditionsCoherent pan-Asian climatic and isotopic response to orbital forcing of tropical insolationReconstruction of Indian summer monsoon winds and precipitation over the past 10,000 years using equatorial pacific SST proxy recordsA probabilistic approach to the use of pollen indicators for plant attributes and biomes: an application to European vegetation at 0 and 6 kaSome mechanisms of mid-Holocene climate change in Europe, inferred from comparing PMIP models to dataWhat have we learnt from palaeoclimate simulations?LATE-QUATERNARY VEGETATION DYNAMICS IN NORTH AMERICA: SCALING FROM TAXA TO BIOMESMid-Holocene climates of the Americas: a dynamical response to changed seasonalityDetermining the drivers of long-term aridity variability: a southern African case studyEvidence for progressive Holocene aridification in southern Africa recorded in Namibian hyrax middens: Implications for African Monsoon dynamics and the ‘‘African Humid Period’’Holocene climate instability during the termination of the African Humid PeriodBayesian palaeoclimate reconstruction
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Monsoon changes for 6000 years ago: Results of 18 simulations from the Paleoclimate Modeling Intercomparison Project (PMIP)
description
article
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im April 1999 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована у квітні 1999
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ലേഖനം
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name
Monsoon changes for 6000 years ...... Intercomparison Project (PMIP)
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Monsoon changes for 6000 years ...... deling Intercomparison Project
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type
label
Monsoon changes for 6000 years ...... Intercomparison Project (PMIP)
@en
Monsoon changes for 6000 years ...... deling Intercomparison Project
@nl
prefLabel
Monsoon changes for 6000 years ...... Intercomparison Project (PMIP)
@en
Monsoon changes for 6000 years ...... deling Intercomparison Project
@nl
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Monsoon changes for 6000 years ...... Intercomparison Project (PMIP)
@en
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A. J. Broccoli
B. McAvaney
C. D. Hewitt
D. Pollard
G. Vettoretti
I. C. Prentice
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P304
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10.1029/1999GL900126
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P577
1999-04-01T00:00:00Z