0000000000594125

AUTHOR

Olga Solomina

showing 4 related works from this author

Reply to 'Limited Late Antique cooling'

2017

010504 meteorology & atmospheric sciencesAntiqueGeneral Earth and Planetary SciencesAncient history010502 geochemistry & geophysics01 natural sciences0105 earth and related environmental sciencesNature Geoscience
researchProduct

Continental-scale temperature variability during the past two millennia

2013

Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia. The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multi-decadal to centennial scales, temperature variability shows distinctly different regional patterns, with more similarity within each hemisphere than between them. There were no globally synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period or Little Ice Age, but all reconstructi…

010506 paleontologyPALAEOCLIMATE AND PALAEOCENOGRAPHYPaleoclimate010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Climate change[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]910 Geography & travel01 natural sciencesCiencias de la Tierra y relacionadas con el Medio AmbienteInvestigación ClimatológicaCentennial550 Earth sciences & geology540 ChemistryPaleoclimatologyIce ageEarth temperaturePaleoclimatologySouthern Hemisphere0105 earth and related environmental sciencesCLIMATE SCIENCEAtmospherePaleoclimate; Temperature; Little Ice Age; Medieval Warm PeriodsTemperatureNorthern HemisphereClimatic changesScale (music)ClimatologyMedieval Warm PeriodsLittle Ice AgePeriod (geology)570 Life sciences; biologyGeneral Earth and Planetary SciencesCIENCIAS NATURALES Y EXACTASGeologyNature Geoscience
researchProduct

Regional coherency of boreal forest growth defines Arctic driftwood provenancing

2016

Arctic driftwood represents a unique proxy archive at the interface of marine and terrestrial environments. Combined wood anatomical and dendrochronological analyses have been used to detect the origin of driftwood and may allow past timber floating activities, as well as past sea ice and ocean current dynamics to be reconstructed. However, the success of driftwood provenancing studies depends on the length, number, and quality of circumpolar boreal reference chronologies. Here, we introduce a Eurasian-wide high-latitude network of 286 ring width chronologies from the International Tree Ring Data Bank (ITRDB) and 160 additional sites comprising the three main boreal conifers Pinus, Larix, a…

010506 paleontologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesEcologybiologyEcologyTaigaOcean currentPlant ScienceCircumpolar starDriftwoodbiology.organism_classification01 natural sciencesBorealArcticSea icePhysical geographyLarchGeology0105 earth and related environmental sciencesDendrochronologia
researchProduct

Diverse growth trends and climate responses across Eurasia’s boreal forest

2016

The area covered by boreal forests accounts for similar to 16% of the global and 22% of the Northern Hemisphere landmass. Changes in the productivity and functioning of this circumpolar biome not o ...

0106 biological sciences010504 meteorology & atmospheric sciencesbiologyRenewable Energy Sustainability and the EnvironmentEcologyGlobal warmingBiomeTaigaPublic Health Environmental and Occupational HealthScots pineNorthern HemisphereCircumpolar star500 Sciencebiology.organism_classification010603 evolutionary biology01 natural sciencesLatitudeGeographyProductivity (ecology)Climatology550 Earth sciences & geology550 Earth sciences & geology0105 earth and related environmental sciencesGeneral Environmental ScienceEnvironmental Research Letters
researchProduct