Olga N Solomina

ORCID: 0000-0002-3307-1951
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About
Contact & Profiles
Research Areas
  • Geology and Paleoclimatology Research
  • Tree-ring climate responses
  • Cryospheric studies and observations
  • Climate change and permafrost
  • Plant Water Relations and Carbon Dynamics
  • Climate variability and models
  • Marine and environmental studies
  • Landslides and related hazards
  • Boron Compounds in Chemistry
  • Geological Studies and Exploration
  • Soil and Environmental Studies
  • Solid-state spectroscopy and crystallography
  • Inorganic Fluorides and Related Compounds
  • Organic and Inorganic Chemical Reactions
  • Winter Sports Injuries and Performance
  • Archaeology and ancient environmental studies
  • Hydrology and Drought Analysis
  • Lichen and fungal ecology
  • Methane Hydrates and Related Phenomena
  • Arctic and Antarctic ice dynamics
  • Pleistocene-Era Hominins and Archaeology
  • Forest ecology and management
  • Molecular Spectroscopy and Structure
  • Geological and Geochemical Analysis
  • Plant Ecology and Soil Science

Institute of Geography
2015-2024

National Research University Higher School of Economics
2020-2024

Ural Branch of the Russian Academy of Sciences
2024

Czech Academy of Sciences, Institute of Physiology
2024

Research Institute for Geo-Hydrological Protection
2021

National Research Council
2021

Geophysical Survey
2020

Russian Academy of Sciences
2000-2020

Syktyvkar State University
2019

Lamont-Doherty Earth Observatory
2014-2017

The spatial context is critical when assessing present-day climate anomalies, attributing them to potential forcings and making statements regarding their frequency severity in a long-term perspective. Recent international initiatives have expanded the number of high-quality proxy-records developed new statistical reconstruction methods. These advances allow more rigorous regional past temperature reconstructions and, turn, possibility evaluating models on policy-relevant, spatio-temporal...

10.1088/1748-9326/11/2/024001 article EN cc-by Environmental Research Letters 2016-01-28

Abstract The long-term relationship between temperature and hydroclimate has remained uncertain due to the short length of instrumental measurements inconsistent results from climate model simulations. This lack understanding is particularly critical with regard projected drought flood risks. Here we assess warm-season co-variability patterns over Europe back 850 CE using measurements, tree-ring based reconstructions, We find that temperature–hydroclimate in both reconstructed data turns...

10.1088/1748-9326/ab2c7e article EN cc-by Environmental Research Letters 2019-06-26

The area covered by boreal forests accounts for ∼16% of the global and 22% Northern Hemisphere landmass. Changes in productivity functioning this circumpolar biome not only have strong effects on species composition diversity at regional to larger scales, but also Earth's carbon cycle. Although temporal inconsistency response tree growth temperature has been reported from some locations higher northern latitudes, a systematic dendroecological network assessment is still missing most zone....

10.1088/1748-9326/11/7/074021 article EN cc-by Environmental Research Letters 2016-07-01

Abstract. Reanalysis data show an increasing trend in Arctic precipitation over the 20th century, but changes are not homogenous across seasons or space. The observed hydroclimate expected to continue and possibly accelerate coming only affecting pan-Arctic natural ecosystems human activities, also lower latitudes through atmospheric ocean circulations. However, a lack of spatiotemporal observational makes reliable quantification change difficult, especially long-term context. To understand...

10.5194/cp-14-473-2018 article EN cc-by Climate of the past 2018-04-10

Shrinking of intermontane basins and expansion their flanking ranges by reverse faulting backthrusting in two counter-dipping systems is a typical mechanism crustal shortening mountain building Central Asia. This realized along the Kurai Fault Zone (southeastern Gorny Altai). Motions on fault maintained thrusting Range Kubadru Uplift Basin sediments caused growth foreberg before front. Forberg separates narrow Aktash from Basin. The paleoearthquakes were generated faults that delineate...

10.1080/00206814.2024.2333000 article EN International Geology Review 2024-04-01

A selective review of lichenometry as used to date Holocene moraines in five diverse regions Alaska and southeastern Kamchatka suggests that growth curves for this North Pacific area may be improved by attention several factors. These included lichen identification, control point number distribution, radiocarbon calibration, alternative curve models, compatibility rate with climate. Support points presented published areas will benefit from supplementary at beyond the break great segments...

10.1657/1523-0430(2003)035[0129:laatmi]2.0.co;2 article EN Arctic Antarctic and Alpine Research 2003-05-01

The retreat of 293 glaciers in the Tien Shan Mountains (Kyrgyz Republic) from their maximum extent during Little Ice Age (LIA) is estimated using aerial photographs 1980 to 1985 and maps at a scale 1:25000, constructed period 1956–1990. Two indices changes are used: linear distance glacier terminus its moraine difference absolute elevation moraine. Historical information about front positions 1880s 1930s was used as an indirect control remote sensing data. age moraines key regions by...

10.1111/j.0435-3676.2004.00225.x article EN Geografiska Annaler Series A Physical Geography 2004-06-01

The mapping and measurement of glaciers their changes are useful in predicting sea‐level regional water supply, studying hazards climate change [ Haeberli et al. , 1998],and the hydropower industry Existing inventories cover only about 67,000 world's estimated 160,000 based on data collected over 50 years or more [e.g., 1998]. available have proven that small ice bodies disappearing at an accelerating rate Antarctic sheet its fringing shelves undergoing unexpected, rapid change. According to...

10.1029/00eo00187 article EN Eos 2000-06-13

Abstract. Tree ring, ice core and glacial geologic histories for the past several centuries offer an opportunity to characterize climate variability identify key parameters forcing glacier expansion in Kamchatka over 400 years. A newly developed larch ring-width chronology (AD 1632–2004) is presented that sensitive summer temperature variability. Individual low growth years record are associated with known proposed volcanic events from Northern Hemisphere. The comparison of ring width minima...

10.5194/cp-3-119-2007 article EN cc-by-nc-sa Climate of the past 2007-02-22
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