Search results for "Roman Warm Period"

showing 4 items of 4 documents

2500 Years of European Climate Variability and Human Susceptibility

2011

Climate variations influenced the agricultural productivity, health risk, and conflict level of preindustrial societies. Discrimination between environmental and anthropogenic impacts on past civilizations, however, remains difficult because of the paucity of high-resolution paleoclimatic evidence. We present tree ring-based reconstructions of central European summer precipitation and temperature variability over the past 2500 years. Recent warming is unprecedented, but modern hydroclimatic variations may have at times been exceeded in magnitude and duration. Wet and warm summers occurred during periods of Roman and medieval prosperity. Increased climate variability from similar to 250 to 6…

010506 paleontology010504 meteorology & atmospheric sciencesMeteorologyClimate Changemedia_common.quotation_subjectLast MillenniumCollapseClimatic ProcessesClimate changeCivilizationHistory 18th CenturyHistory 21st Century01 natural sciencesTreesHistory 17th CenturyQuercusReconstructionsDendrochronologyHumansAgricultural productivityEpidemicsRoman Warm PeriodSeriesHistory AncientHoloceneHistory 15th Century0105 earth and related environmental sciencesmedia_commonMultidisciplinaryDroughtHoloceneTemperatureRecordsAgricultureHistory 19th CenturyDemiseHistory 20th Century15. Life on landHistory MedievalRoman EmpireEuropeGeographyHistory 16th Century13. Climate actionAfricaSeasonsPhysical geographyProsperityScience
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A review of climate reconstructions from terrestrial climate archives covering the first millennium AD in northwestern Europe

2018

AbstractLarge changes in landscape, vegetation, and culture in northwestern (NW) Europe during the first millennium AD seem concurrent with climatic shifts. Understanding of this relation requires high-resolution palaeoclimate reconstructions. Therefore, we compiled available climate reconstructions from sites across NW Europe (extent research area: 10°W–20°E, 45°–60°N) through review of literature and the underlying data, to identify supraregional climatic changes in this region. All reconstructions cover the period from AD 1 to 1000 and have a temporal resolution of ≤50 yr. This resulted in 22 climate reconstructions/proxy records based on different palaeoclimate archives: chironomids (1)…

010506 paleontologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesStalagmiteSeasonalitymedicine.disease_causemedicine.disease01 natural sciencesSphagnum MossesProxy (climate)Arts and Humanities (miscellaneous)PollenPaleoclimatologymedicineGeneral Earth and Planetary SciencesPhysical geographyTestate amoebaeRoman Warm PeriodGeology0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary Research
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Climate change and human impact in central Spain during Roman times: High-resolution multi-proxy analysis of a tufa lake record (Somolinos, 1280m asl)

2012

The Roman Period is considered a crucial phase in the evolution of Holocene landscapes, due to the coincidence of major climatic, environmental, economic and cultural changes. However, there is still debate as to the regional expression of these changes, and to the mechanisms involved, particularly in the topographically and climatically complex region of the Mediterranean. In order to improve our understanding of the synergies between societal and environmental change during this period in central Spain, we present a comprehensive case study based on the integration of multi-proxy palaeoenvironmental, archaeological and historical data. High-resolution, interdisciplinary research has been …

Mediterranean climateEnvironmental changeLand-use changePalaeoenvironmentClimate changeCentral SpainAridGeographyRoman Warm PeriodPalaeolimnologyAridificationLand use land-use change and forestryMarl lakePhysical geographyRoman Warm PeriodGeomorphologyHoloceneEarth-Surface ProcessesCATENA
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A 5500-year oxygen isotope record of high arctic environmental change from southern Spitsbergen

2017

The oxygen isotope composition of chironomid head capsules in a sediment core spanning the past 5500 years from Lake Svartvatnet in southern Spitsbergen was used to reconstruct the oxygen isotope composition of lake water (δ18Olw) and local precipitation. The δ18Olw values display shifts from the baseline variability consistent with the timing of recognized historical climatic episodes, such as the Roman Warm Period, the Dark Ages Cold Period and the ‘Little Ice Age’. The highest values of the record, ca. 3‰ above modern δ18Olw values, occur at ca. 1900–1800 cal. yr BP. Three negative excursions increasing in intensity toward the present, at 3400–3200, 1250–1100, and 350–50 cal. yr BP, are…

TEMPERATURE VARIABILITY1171 GeosciencesSpitsbergen010506 paleontologyArcheology010504 meteorology & atmospheric sciencesEnvironmental change"Little Ice Age'NORTH-ATLANTIC CLIMATE01 natural sciencesIsotopes of oxygenSVALBARD ICE CORESvalbardArcticSea iceEAST GREENLAND CURRENTPrecipitationRoman Warm Periodclimate0105 earth and related environmental sciencesEarth-Surface Processes‘Little Ice Age’Global and Planetary ChangegeographyHOLOCENE GLACIER FLUCTUATIONSgeography.geographical_feature_categoryEcologyLATE-PLEISTOCENEoxygen isotopesBaseline (sea)LAKE-WATER DELTA-O-18North AtlanticPaleontologytemperatureGlacierPALEOCLIMATE RECONSTRUCTIONOceanographyArctic13. Climate actionta1181SEA-ICEGeologyHIGH-RESOLUTIONHolocene
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