Diana Vladimirova

ORCID: 0000-0002-1678-0174
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About
Contact & Profiles
Research Areas
  • Cryospheric studies and observations
  • Geology and Paleoclimatology Research
  • Arctic and Antarctic ice dynamics
  • Atmospheric and Environmental Gas Dynamics
  • Methane Hydrates and Related Phenomena
  • Climate change and permafrost
  • Isotope Analysis in Ecology
  • Polar Research and Ecology
  • Winter Sports Injuries and Performance
  • Icing and De-icing Technologies
  • Climate variability and models
  • Aeolian processes and effects
  • Hydrocarbon exploration and reservoir analysis
  • Geochemistry and Geologic Mapping
  • Tree-ring climate responses
  • Aerospace Engineering and Energy Systems
  • Atmospheric aerosols and clouds
  • Calibration and Measurement Techniques
  • Astro and Planetary Science
  • Environmental and Cultural Studies in Latin America and Beyond
  • Advanced Electrical Measurement Techniques
  • Peatlands and Wetlands Ecology
  • Delphi Technique in Research
  • Fluorine in Organic Chemistry
  • Pleistocene-Era Hominins and Archaeology

British Antarctic Survey
2022-2024

St Petersburg University
2016-2024

Natural Environment Research Council
2022

Institute of Geography
2020-2021

Institute of Geography
2020

University of Copenhagen
2017-2019

Arctic and Antarctic Research Institute
2016-2019

Julien Emile‐Geay Nicholas P. McKay Darrell S. Kaufman Lucien von Gunten Jianghao Wang and 93 more Kevin J. Anchukaitis Nerilie J. Abram J. A. Addison Mark A.J. Curran Michael N. Evans Benjamin J. Henley Zhixin Hao Belén Martrat Helen McGregor Raphael Neukom Gregory T. Pederson Barbara Stenni Kaustubh Thirumalai J. Werner Chenxi Xu Dmitry Divine Bronwyn Dixon Joëlle Gergis Ignacio A. Mundo Takeshi Nakatsuka Steven J. Phipps Cody Routson Eric J. Steig Jessica E. Tierney Jonathan Tyler Kathryn Allen Nancy A. N. Bertler Jesper Björklund Brian Chase Min‐Te Chen E. R. Cook Rixt de Jong Kristine L. DeLong Daniel A. Dixon Alexey Ekaykin Vasile Ersek Helena L. Filipsson Pierre Francus Mandy Freund Massimo Frezzotti Narayan Gaire Konrad Gajewski Quansheng Ge Hugues Goosse A. A. Gornostaeva Martín Grosjean Kazuho Horiuchi Anne Hormes Katrine Husum Elisabeth Isaksson K. Selvaraj Kenji Kawamura K. Halimeda Kilbourne Nalân Koç Guillaume Leduc Hans W. Linderholm Andrew Lorrey Vladimir N Mikhalenko P. Graham Mortyn Hideaki Motoyama Andrew Moy Robert Mulvaney Philipp Munz David J. Nash Hans Oerter Thomas Opel Anaïs Orsi Dmitriy V. Ovchinnikov Trevor J. Porter Heidi Roop Casey Saenger Masaki Sano David J. Sauchyn Krystyna M. Saunders Marit‐Solveig Seidenkrantz Mirko Severi Xuemei Shao Marie‐Alexandrine Sicre Michael Sigl Kate E. Sinclair Scott St. George Jeannine‐Marie St. Jacques Meloth Thamban Udya Thapa Elizabeth R. Thomas Chris Turney Ryu Uemura André Viau Diana Vladimirova Eugene R. Wahl James W. C. White Zicheng Yu Jens Zinke

Abstract Reproducible climate reconstructions of the Common Era (1 CE to present) are key placing industrial-era warming into context natural climatic variability. Here we present a community-sourced database temperature-sensitive proxy records from PAGES2k initiative. The gathers 692 648 locations, including all continental regions and major ocean basins. trees, ice, sediment, corals, speleothems, documentary evidence, other archives. They range in length 50 2000 years, with median 547...

10.1038/sdata.2017.88 article EN cc-by Scientific Data 2017-07-11

Abstract Accurate estimates of the past extent Greenland ice sheet provide critical constraints for models used to determine Greenland’s response climate forcing and contribution global sea level. Here we use a continuous core dust record from Renland cap on east coast constrain timing changes margin relative level over last glacial cycle. During Holocene previous interglacial period (Eemian) was dominated by coarse particles consistent with rock samples central East Greenland. From particle...

10.1038/s41467-019-12546-2 article EN cc-by Nature Communications 2019-10-03

Several recent studies from both Greenland and Antarctica have reported significant changes in the water isotopic composition of near-surface snow between precipitation events. These been linked to exchange with atmospheric vapor sublimation-induced fractionation, but processes are poorly constrained by observations. Understanding quantifying these crucial interpretation ice core climate proxies formulation isotope-enabled general circulation models. Here, we present continuous measurements...

10.1029/2018jd029619 article EN cc-by-nc-nd Journal of Geophysical Research Atmospheres 2019-02-19

The Sentinel Application Platform (SNAP) architecture facilitates Earth Observation data processing. In this work, we present results from a new Snow Processor for SNAP. We also describe physical principles behind the developed snow property retrieval technique based on analysis of Ocean and Land Colour Instrument (OLCI) onboard Sentinel-3A/B measurements over clean polluted fields. Using OLCI spectral reflectance in range 400–1020 nm, derived important properties such as broadband albedo,...

10.3390/rs11192280 article EN cc-by Remote Sensing 2019-09-29

In this study, we present the age scales for three Antarctic Peninsula (AP) ice cores: Palmer, Rendezvous, and Jurassic. The cores are all intermediate-depth cores, in 133–141 m depth range. Non-sea-salt sulfate ([nssSO42−]) hydrogen peroxide (H2O2) display marked seasonal variability suitable annual-layer counting. Palmer core covers 390 years, 1621–2011 C.E., is one of oldest AP cores. Rendezvous Jurassic lower elevation high-snow accumulation sites therefore cover shorter intervals,...

10.3390/geosciences12020087 article EN cc-by Geosciences 2022-02-16

Abstract. Changes in sea ice conditions and atmospheric circulation over the Southern Ocean play an important role modulating Antarctic climate. However, observations of both wind are limited Antarctica Ocean, temporally spatially, prior to satellite era (1970 onwards). Ice core chemistry data can be used reconstruct changes annual, decadal, millennial timescales. To facilitate reconstructions, CLIVASH2k (CLimate Variability Hemisphere past 2000 years) working group has compiled a database...

10.5194/essd-15-2517-2023 article EN cc-by Earth system science data 2023-06-20

Abstract. We use isotopic composition (δD) data from six sites in Princess Elizabeth Land (PEL) order to reconstruct air temperature variability this sector of East Antarctica over the last 350 years. First, we present-day instrumental mean annual surface demonstrate that studied region (between Russia's Progress, Vostok and Mirny research stations) is characterized by uniform variability. thus construct a stacked record anomaly for whole period 1958–2015. A comparison series with Southern...

10.5194/cp-13-61-2017 article EN cc-by Climate of the past 2017-01-16

The Sentinel Application Platform (SNAP) architecture facilitates Earth Observation data processing (http://step.esa.int/main/toolboxes/snap/). In this work we present results from a new Snow Processor for SNAP. We also describe physical principles behind the developed snow property retrieval technique based on analysis of Ocean and Land Colour Instrument (OLCI) onboard Sentinel-3A/B measurements over clean polluted fields. Using OLCI spectral reflectance in range 400-1020nm, derive...

10.20944/preprints201906.0162.v1 preprint EN 2019-06-17

Abstract. A new ice core was drilled in West Antarctica on Skytrain Ice Rise field season 2018/2019. This 651 m is one of the main targets WACSWAIN (WArm Climate Stability Antarctic sheet last INterglacial) project. present-day accumulation rate 13.5 cm w.e. yr−1 derived. Although project mainly aims to investigate interglacial (115–130 ka), a robust chronology period covering recent past needed constrain age models for deepest ice. Additionally, this time important understanding current...

10.5194/cp-18-1831-2022 article EN cc-by Climate of the past 2022-08-10

The remote Antarctic continent, distant from human industrial activity, should be one of the last places on Earth to capture Anthropogenic change. Hence, stratigraphic evidence pollution and nuclear activity in provides proof global nature Anthropocene epoch. We propose an Peninsula ice core candidate for Global boundary Stratotype Section Point (GSSP) onset Anthropocene. Palmer captures first spheroidal carbonaceous fly ash particles (SCPs), resulting high temperature combustion deposited...

10.1177/20530196231155191 article EN cc-by The Anthropocene Review 2023-03-16

Abstract Sea‐ice extent is predicted to decrease in a warming climate. However, despite global over the past century, total Antarctic sea ice remained relatively stable from 1979 until 2015, before strongly melting. Here we explore long‐term variability by reconstructing since 1700 CE, based on paleoclimate records and data assimilation. Our results indicate decline southern hemisphere sea‐ice 20th driven reduction of 0.26 million km 2 Weddell Sea that reached values at end century lower...

10.1029/2023gl104666 article EN cc-by-nc Geophysical Research Letters 2023-10-28

Biomass burning plays an important role in climate-forcing and atmospheric chemistry. The drivers of fire activity over the past two centuries, however, are hotly debated fueled by poor constraints on magnitude trends preindustrial regimes. As a powerful tracer biomass burning, reconstructions paleoatmospheric carbon monoxide (CO) can provide valuable information evolution across to industrial transition. Here too, significant disagreements between existing CO records currently allow for...

10.1073/pnas.2402868121 article EN cc-by-nc-nd Proceedings of the National Academy of Sciences 2024-08-05

We estimated the stable isotopic composition of water from subglacial Lake Vostok using two different sets samples: (1) frozen on drill bit immediately after first lake unsealing and (2) in borehole re-drilled one year later. The most reliable values are: -59.0 ± 0.3 ‰ for oxygen-18, -455 1 deuterium 17 d-excess. This result is also confirmed by modelling transformations which froze borehole, a laboratory experiment simulating this process. A comparison newly obtained with that ice (-56.2...

10.1080/10256016.2015.1129327 article EN Isotopes in Environmental and Health Studies 2016-02-10

Abstract. Changes in sea ice conditions and atmospheric circulation over the Southern Ocean play an important role modulating Antarctic climate. However, observations of both wind are limited Antarctica Ocean, temporally spatially. Ice core chemistry data can be used to reconstruct changes annual, decadal, millennial timescales. To facilitate reconstructions, CLIVASH2k working group has compiled a database two species, sodium [Na+] sulphate [SO42-], commonly measured ionic species. The...

10.5194/essd-2022-368 preprint EN cc-by 2022-12-12

During the field campaign in August 18–30, 2020 meteorological regime and heat balance of glacier surface were investigated crater Mt Elbrus Eastern Summit (5600 m a.s.l.) together with GPR measurements ice thickness seasonal snow cover. Preliminary data analysis allowed following features: predominance synoptic fluctuations over diurnal ones; high values average maximum wind speed associated impact jet streams influence leeward storms; extremely temporal variability relative humidity its...

10.31857/s2076673421010078 article EN cc-by Journal Ice and Snow 2021-01-01

Work on the project focused following five areas: 1) field works in Antarctica at Vostok and Concordia stations; 2) experimental theoretical studies of ice core paleoclimate research; 3) related to exploration subglacial Lake Vostok; 4) development technology drilling equipment for deep coring lakes; 5) upgrading analytical instrumentation Climate Environmental Research Laboratory (CERL) Arctic Antarctic Institute. The main achievements research include further elaboration a new method...

10.15356/2076-6734-2017-1-133-141 article EN cc-by Journal Ice and Snow 2017-01-01

Abstract. We use isotopic composition (δD) data from 6 sites in Princess Elisabeth Land (PEL) order to reconstruct the air temperature variability this sector of East Antarctica for last 350 years. First, we present-day instrumental mean annual surface demonstrate that studied region (between Russian research stations Progress, Vostok and Mirny) is characterized by uniform variability. thus construct stacked record anomaly whole period 1958–2015. A comparison series with Southern Hemisphere...

10.5194/cp-2016-76 preprint EN cc-by 2016-07-08

The results of detailed isotopic studies ice core samples from the Vostok station (East Antarctica) related to MIS-11 era (the 11th sea isotope stage, i.e. 370–440 thousand years ago) are presented. Reconstruction paleoclimatic conditions in this period time was performed using method interpretation ice, developed by authors article, which is based on joint analysis three independent parameters: δD, d-excess, 17 O-excess. composition (δD) and deuterium excess depend following meteorological...

10.15356/2076-6734-2018-2-149-158 article EN cc-by Journal Ice and Snow 2018-05-21

The knowledge of the spatial distribution snow accumulation rate and isotopic composition in different scales, from local to continental, over Antarctic Ice Sheet is critically important for interpretation paleoclimate data obtained deep ice cores, correct assessment sheet mass balance, etc. With this mind, we have synthesized geodetic, glaciological geochemical collected vicinity central Vostok station 1970–2017 order shed light on processes governing scale 100 1000 m. First, discovered...

10.30758/0555-2648-2019-65-1-46-62 article EN Arctic and Antarctic Research 2019-04-08

Jacobsite is a characteristic minor mineral of manganese ores at the Ushkatyn-III deposit in Central Kazakhstan. It mainly associates with hausmannite, tephroite, sonolite, friedelite, pennantite and calcite bulk mass ores. A similar association, but without also jacobsite from veinlets intersecting ore. The chemical composition varies Mn1.5Fe1.5O4 to MnFe2O4. high content (1 atoms per formula unit (apfu)) dominates ores, while veins are dominated by stoichiometric (Mn ~1 apfu). was formed...

10.31857/s0869605524010063 article EN Zapiski RMO (Proceedings of the Russian Mineralogical Society) 2024-08-11

<p>In 2016–2018, during Russian Arctic Expedition on Svalbard (RAE-S) we have collected the samples of atmospheric precipitation, terrestrial waters, snow and ice West Spitsbergen island in vicinity Grønfjorden. The measurements stable water isotope content (δ<sup>18</sup>O δD) precipitation Barentsburg has allowed to draw Local Meteoric Water Line analyze relationship between isotopic air...

10.5194/egusphere-egu2020-13048 article EN 2020-03-09

In this study, we used the stable water isotope record (δ18O) from an ice core drilled in Palmer Land, southern Antarctic Peninsula (AP). Utilizing δ18O identified two climate regimes during satellite era. During 1979–1998 positive interdecadal Pacific oscillation (IPO) phase, a low-pressure system north of Weddell Sea drove southeasterly winds that are associated with increase warm air mass intrusion onto Larsen shelves, which melted and decreased sea concentration Sea/increase...

10.3390/geosciences12090344 article EN cc-by Geosciences 2022-09-16

The present-day global climate changes, very likely caused by anthropogenic activity, may potentially present a serious threat to the whole human civilization in near future. In order develop plan of measures aimed at elimination these threats and adaptation undesirable one should deeply understand mechanism past (and thus, future) climatic changes our planet. this study we compare data instrumental observations air temperature snow accumulation rate performed Central Antarctica (the Vostok...

10.15356/2076-6734-2017-1-5-9 article EN cc-by Journal Ice and Snow 2017-01-01
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