Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis
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Climate Change and Drought Events in the Geochemical Records of the Lacustrine Deposits in the Southeastern Tibetan PlateauReconstruction of fire regimes through integrated paleoecological proxy data and ecological modelingWidespread exploitation of the honeybee by early Neolithic farmers.Climate refugia: joint inference from fossil records, species distribution models and phylogeography.Twenty-first century approaches to ancient problems: Climate and society.Rainfall regimes of the Green Sahara.Postglacial range expansion and the role of ecological factors in driving adaptive evolution of Musa basjoo var. formosanaNon-native plants add to the British flora without negative consequences for native diversity.Changes in biomass allocation buffer low CO2 effects on tree growth during the last glaciation.Ocean (de)oxygenation from the Last Glacial Maximum to the twenty-first century: insights from Earth System models.Shortwave forcing and feedbacks in Last Glacial Maximum and Mid-Holocene PMIP3 simulations.Comment on "Climate sensitivity estimated from temperature reconstructions of the Last Glacial Maximum".Underlying causes of Eurasian midcontinental aridity in simulations of mid-Holocene climate.Climatic and biotic velocities for woody taxa distributions over the last 16 000 years in eastern North America.Evaluation of climate models using palaeoclimatic dataWhat drives LGM precipitation over the western Mediterranean? A study focused on the Iberian Peninsula and northern MoroccoEvaluation of CMIP5 palaeo-simulations to improve climate projectionsMid-Holocene and Last Glacial Maximum climate simulations with the IPSL model—part I: comparing IPSL_CM5A to IPSL_CM4Mid-Holocene and last glacial maximum climate simulations with the IPSL model: part II: model-data comparisonsRegional energy budget control of the intertropical convergence zone and application to mid-Holocene rainfallDistribution and vegetation reconstruction of the deserts of northern China during the mid-HoloceneClimate-driven expansion of blanket bogs in Britain during the HoloceneClimate model benchmarking with glacial and mid-Holocene climatesConsistent large-scale temperature responses in warm and cold climatesMid-Holocene monsoons: a multi-model analysis of the inter-hemispheric differences in the responses to orbital forcing and ocean feedbacksPrecipitation changes in the Mediterranean basin during the Holocene from terrestrial and marine pollen records: a model–data comparisonMulti vegetation model evaluation of the Green Sahara climate regimeImpacts of surface boundary conditions on regional climate model simulations of European climate during the Last Glacial MaximumWarm Mediterranean mid-Holocene summers inferred from fossil midge assemblagesClimate reconstructions based on postglacial macrofossil assemblages from four river systems in southwestern AlbertaMid-Holocene frozen ground in China from PMIP3 simulationsPatterns and dynamics of European vegetation change over the last 15,000 yearsPaleoclimate modeling in China: A reviewA framework for evaluating the influence of climate, dispersal limitation, and biotic interactions using fossil pollen associations across the late QuaternaryWhat have we learnt from palaeoclimate simulations?Changes in biological productivity along the northwest African margin over the past 20,000 yearsTrees tracking a warmer climate: The Holocene range shift of hazel (Corylus avellana) in northern Europe
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Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis
description
im September 2010 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована у вересні 2010
@uk
name
Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis
@en
Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis
@nl
type
label
Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis
@en
Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis
@nl
prefLabel
Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis
@en
Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis
@nl
P2093
P2860
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P1433
P1476
Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis
@en
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A. E. Viau
A. Henderson
B. A. S. Davis
I. C. Prentice
J. Williams
K. Gajewski
M. Scholze
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P2888
P304
P356
10.1007/S00382-010-0904-1
P577
2010-09-30T00:00:00Z