Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variabilityClimate reconstructions: Low-frequency ambition and high-frequency ratificationClimate: past ranges and future changesContinental-scale temperature variability during the past two millenniaPlague dynamics are driven by climate variation.Climatic warming disrupts recurrent Alpine insect outbreaks.Uniform climate sensitivity in tree-ring stable isotopes across species and sites in a mid-latitude temperate forest.Modeling the epidemiological history of plague in Central Asia: palaeoclimatic forcing on a disease system over the past millennium.No growth stimulation of Canada's boreal forest under half-century of combined warming and CO2 fertilizationWeakening of annual temperature cycle over the Tibetan Plateau since the 1870s.Ensemble reconstruction constraints on the global carbon cycle sensitivity to climate.2500 years of European climate variability and human susceptibility.Causes and consequences of past and projected Scandinavian summer temperatures, 500-2100 AD.Filling the Eastern European gap in millennium-long temperature reconstructionsOld World megadroughts and pluvials during the Common EraComplex climate controls on 20th century oak growth in Central-West Germany.Persistent positive North Atlantic oscillation mode dominated the Medieval Climate Anomaly.Three centuries of insect outbreaks across the European Alps.Digitizing historical plague.Comparison of δ(13)C and δ(18)O from cellulose, whole wood, and resin-free whole wood from an old high elevation Pinus uncinata in the Spanish central Pyrenees.Growth responses to climate in a multi-species tree-ring network in the Western Carpathian Tatra Mountains, Poland and Slovakia.1200 years of regular outbreaks in alpine insects.Timing and duration of European larch growing season along altitudinal gradients in the Swiss Alps.Sensitivity of whole wood stable carbon and oxygen isotope values to milling procedures.Multi-proxy dating the ‘Millennium Eruption’ of Changbaishan to late 946 CECooling and societal change during the Late Antique Little Ice Age from 536 to around 660 ADA noodle, hockey stick, and spaghetti plate: a perspective on high-resolution paleoclimatologyThe twentieth century was the wettest period in northern Pakistan over the past millenniumMulti-proxy dating of Iceland’s major pre-settlement Katla eruption to 822–823 CEExtra-tropical Northern Hemisphere land temperature variability over the past 1000 yearsA 350 year drought reconstruction from Alpine tree ring stable isotopesReassessing the evidence for tree-growth and inferred temperature change during the Common Era in Yamalia, northwest SiberiaTree rings and volcanic coolingEffect of scaling and regression on reconstructed temperature amplitude for the past millenniumNew tree-ring evidence for the Late Glacial period from the northern pre-Alps in eastern SwitzerlandSite-specific climatic signals in stable isotope records from Swedish pine forestsSpruce tree-ring proxy signals during cold and warm periodsClimate signals in δ 13 C of wood lignin methoxyl groups from high-elevation larch treesRanking of tree-ring based temperature reconstructions of the past millenniumModified climate with long term memory in tree ring proxies
P50
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P50
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German academic
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German academic
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German academic
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académico alemán
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geograaf
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أكاديمي ألماني
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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Jan Esper
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1968-01-01T00:00:00Z
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lccn-n2001007261