Search results for "Climate reconstruction"

showing 5 items of 5 documents

Comparison of quantitative Holocene temperature reconstructions using multiple proxies from a northern boreal lake

2017

Four biotic proxies (plant macrofossils, pollen, chironomids and diatoms) are employed to quantitatively reconstruct variations in mean July air temperatures ( Tjul) at Lake Loitsana (northern Finland) during the Holocene. The aim is to evaluate the robustness and biases in these temperature reconstructions and to compare the timing of highest Tjul in the individual reconstructions. The reconstructed Tjul values are evaluated in relation to local-scale/site-specific processes associated with the Holocene lake development at Loitsana as these factors have been shown to significantly influence the fossil assemblages found in the Lake Loitsana sediments. While pollen-based temperatures follow…

1171 GeosciencesInsolation010506 paleontologyArcheology010504 meteorology & atmospheric sciencesecological driversCLIMATE RECONSTRUCTIONSta1171CENTRAL NORWAYchironomidsWetlandEASTERN-EUROPEAN RUSSIANorthern finlandmedicine.disease_cause01 natural sciencesdiatomsPollenpiilevätmedicineTREE-LINE AREAsurviaissääsketplant macrofossils1172 Environmental sciencesHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesGlobal and Planetary Changegeographygeography.geographical_feature_categoryEcologySUB-ARCTIC FINLANDPaleontologyMacrofossilFINNISH LAPLANDpaleolimnologiaBoreal13. Climate actionpollenClimatologyta1181paleoklimatologiaPALEOCLIMATE RECONSTRUCTIONSCHIRONOMIDAE INSECTAnorthern boreal FennoscandiaPhysical geographymakrofossiilitsiitepölyanalyysiGeologyThe Holocene
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Pre‐instrumental summer precipitation variability in northwestern Greece from a high‐elevation Pinus heldreichii network

2021

The spatiotemporal variability of precipitation is of vital importance to Mediterranean ecology and economy, but pre‐instrumental changes are not well understood. Here, we present a millennial‐length June–July precipitation reconstruction derived from a network of 22 Pinus heldreichii high‐elevation sites in the Pindus Mountains of northwestern Greece. Tree‐ring width chronologies from these sites cohere exceptionally well over the past several hundred years (r1467–2015 = 0.64) revealing coherence at inter‐annual to centennial timescales across the network. The network mean calibrates significantly against instrumental June–July precipitation over the past 40 years (r1976–2015 = 0.71), even…

Mediterranean climateAtmospheric Science551.6biologyElevationPindus MountainsMediterraneanbiology.organism_classificationClimatologyValia CaldaPinus heldreichiiEnvironmental sciencePrecipitationtree‐ringsclimate reconstructionpine
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Reassessing the evidence for tree-growth and inferred temperature change during the Common Era in Yamalia, northwest Siberia

2013

AbstractThe development of research into the history of tree growth and inferred summer temperature changes in Yamalia spanning the last 2000 years is reviewed. One focus is the evolving production of tree-ring width (TRW) and tree-ring maximum-latewood density (MXD) larch (Larix sibirica) chronologies, incorporating different applications of Regional Curve Standardisation (RCS). Another focus is the comparison of independent data representing past tree growth in adjacent Yamalia areas: Yamal and Polar Urals, and the examination of the evidence for common growth behaviour at different timescales. The sample data we use are far more numerous and cover a longer time-span at Yamal compared to …

Summer temperatureArcheologyGlobal and Planetary ChangebiologyYamalDendroclimatologyClimate reconstructionGeologyDendroclimatologyMedieval Warm Periodbiology.organism_classificationTree (graph theory)Larix sibiricaClimatologyLarchPolar UralsIndependent dataMedieval warm periodGeologyEcology Evolution Behavior and SystematicsChronologySampling biasQuaternary Science Reviews
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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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Multiscale variation in drought controlled historical forest fire activity in the boreal forests of eastern Fennoscandia

2017

Forest fires are a key disturbance in boreal forests, and characteristics of fire regimes are among the most important factors explaining the variation in forest structure and species composition. The occurrence of fire is connected with climate, but earlier, mostly local-scale studies in the northern European boreal forests have provided little insight into fire-climate relationship before the modern fire suppression period. Here, we compiled annually resolved fire history, temperature, and precipitation reconstructions from eastern Fennoscandia from the mid-16th century to the end of the 19th century, a period of strong human influence on fires. We used synchrony of fires over the network…

climate variability0106 biological sciences010504 meteorology & atmospheric sciencesBayesian inferencescale-derivative analysisREGIMESClimate changeCROSS-SCALE ANALYSISdroughtBayesian inference010603 evolutionary biology01 natural sciencesDendrochronologyEcology Evolution Behavior and Systematicsclimate reconstruction0105 earth and related environmental sciencesNORTHERN EUROPE4112 ForestryCLIMATE-CHANGELANDSCAPEEcologyTREE-RING DATATaigaAGE DISTRIBUTIONFINLAND15. Life on landLOW-SEVERITY FIREVariation (linguistics)Geography13. Climate actionscale space multiresolution correlation analysisAge distributionPhysical geographyTree ring datafire synchronyPICEA-ABIES STANDSforest fireEcological Monographs
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