Abstract is: Valerie Masson-Delmotte is a French climate scientist and Research Director at the French Alternative Energies and Atomic Energy Commission, where she works in the Climate and Environment Sciences Laboratory (LSCE). She uses data from past climates to test models of climate change, and has contributed to several IPCC reports.
human | Q5 |
P512 | academic degree | habilitation | Q308678 |
doctorate in France | Q3033550 | ||
P166 | award received | Time 100 | Q604370 |
Descartes Prize | Q205811 | ||
Knight of the Legion of Honour | Q10855271 | ||
CNRS silver medal | Q3332287 | ||
Irène-Joliot-Curie Prize | Q3404822 | ||
Knight of the National Order of Merit | Q13422138 | ||
Jean-Perrin Prize | Q16671125 | ||
Honorary doctor of the University of Liège | Q23700921 | ||
Étienne Roth award | Q125526236 | ||
Milutin Milankovic Medal | Q53705821 | ||
Nature's 10 | Q59918767 | ||
P27 | country of citizenship | France | Q142 |
P184 | doctoral advisor | Sylvie Joussaume | Q21028340 |
P185 | doctoral student | Jean-Louis Bonne | Q58323834 |
P69 | educated at | École Centrale Paris | Q273447 |
Laboratoire des sciences du climat et de l'environnement | Q3214491 | ||
P108 | employer | University of Bordeaux | Q13344 |
Alternative Energies and Atomic Energy Commission | Q868550 | ||
Paris-Saclay University | Q109409389 | ||
P734 | family name | Masson | Q11172443 |
Masson | Q11172443 | ||
Masson | Q11172443 | ||
Delmotte | Q25369670 | ||
Delmotte | Q25369670 | ||
Delmotte | Q25369670 | ||
P101 | field of work | greenhouse effect | Q41560 |
climate change | Q125928 | ||
greenhouse gas | Q167336 | ||
climatology | Q52139 | ||
paleoclimatology | Q191069 | ||
P735 | given name | Valérie | Q18066725 |
Valérie | Q18066725 | ||
P1412 | languages spoken, written or signed | French | Q150 |
English | Q1860 | ||
P6104 | maintained by WikiProject | Women in Science 2022 - Rejuvenation | Q110812727 |
P463 | member of | Intergovernmental Panel on Climate Change | Q171183 |
Academia Europaea | Q337234 | ||
Laboratoire des sciences du climat et de l'environnement | Q3214491 | ||
High Council on Climate | Q60834697 | ||
P1559 | name in native language | Valérie Masson-Delmotte | |
P103 | native language | French | Q150 |
P1971 | number of children | 2 | |
P106 | occupation | scientist | Q901 |
author | Q482980 | ||
climatologist | Q1113838 | ||
researcher | Q1650915 | ||
science communicator | Q15143191 | ||
paleoclimatologist | Q56682806 | ||
P39 | position held | municipal councillor | Q15113603 |
directeur de recherche | Q18121578 | ||
co-president | Q105490190 | ||
P21 | sex or gender | female | Q6581072 |
P8687 | social media followers | 70649 | |
P26 | spouse | Marc Delmotte | Q114081107 |
Q61078680 | 1-D-ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica |
Q109050110 | A 120,000-year long climate record from a NW-Greenland deep ice core at ultra-high resolution |
Q56192287 | A 60-year ice-core record of regional climate from Adélie Land, coastal Antarctica |
Q56100379 | A Review of Antarctic Surface Snow Isotopic Composition: Observations, Atmospheric Circulation, and Isotopic Modeling* |
Q112607582 | A Roadmap for Using the UN Decade of Ocean Science for Sustainable Development in Support of Science, Policy, and Action |
Q56100268 | A comparison of the present and last interglacial periods in six Antarctic ice cores |
Q56100580 | A continuous record of temperature evolution over a sequence of Dansgaard-Oeschger events during Marine Isotopic Stage 4 (76 to 62 kyr BP) |
Q56100302 | A generalized additive model for the spatial distribution of stable isotopic composition in Antarctic surface snow |
Q56100232 | A global picture of the first abrupt climatic event occurring during the last glacial inception |
Q56100582 | A late medieval warm period in the Southern Ocean as a delayed response to external forcing? |
Q56100584 | A late-glacial high-resolution site and source temperature record derived from the EPICA Dome C isotope records (East Antarctica) |
Q30978222 | A model-tested North Atlantic Oscillation reconstruction for the past millennium |
Q61656120 | A new Himalayan ice core CH4 record: possible hints at the preindustrial latitudinal gradient |
Q56100362 | A new spatial distribution map ofδ18O in Antarctic surface snow |
Q61046413 | A review of climatic controls on δ18O in precipitation over the Tibetan Plateau: Observations and simulations |
Q61046446 | A review of the bipolar see–saw from synchronized and high resolution ice core water stable isotope records from Greenland and East Antarctica |
Q33611781 | Abrupt change of Antarctic moisture origin at the end of Termination II. |
Q59308927 | Acquiring High to Ultra-High Resolution Geological Records of Past Climate Change by Scientific Drilling |
Q120768963 | Acquiring High to Ultra-High Resolution Geological Records of Past Climate Change by Scientific Drilling |
Q56100586 | Age of Himalayan bottom ice cores |
Q55035237 | An oceanic cold reversal during the last deglaciation. |
Q21093487 | An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka |
Q21128943 | An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka |
Q56100303 | An unstable tree-growth response to climate in two 500 year chronologies, North Eastern Qinghai-Tibetan Plateau |
Q56100598 | Analyse isotopique de l'air piégé dans la glace pour quantifier les variations de température |
Q58237612 | Antarctic climate change and the environment: an update |
Q58382084 | Antarctic climate variability at regional and continental scales over the last 2,000 years |
Q58382081 | Antarctic climate variability on regional and continental scales over the last 2000 years |
Q56100234 | Antarctic temperature changes during the last millennium: evaluation of simulations and reconstructions |
Q57261599 | Application of eco-physiological models to the climatic interpretation of δ13C and δ18O measured in Siberian larch tree-rings |
Q59836460 | Archival of the water stable isotope signal in East Antarctic ice cores |
Q59836454 | Archival processes of the water stable isotope signal in East Antarctic ice cores |
Q59836456 | Archival processes of the water stable isotope signal in East Antarctic ice cores |
Q46889970 | Are We Reaching the Limits of Homo sapiens? |
Q21132406 | Assessing "dangerous climate change": required reduction of carbon emissions to protect young people, future generations and nature |
Q58100294 | Assessing recent trends in high-latitude Southern Hemisphere surface climate |
Q109539594 | Assessing the robustness of Antarctic temperature reconstructions over the past 2 millennia using pseudoproxy and data assimilation experiments |
Q58243396 | Assessing the robustness of Antarctic temperature reconstructions over the past two millennia using pseudoproxy and data assimilation experiments |
Q51411717 | Asynchrony between Antarctic temperature and CO2 associated with obliquity over the past 720,000 years. |
Q56100239 | Atmospheric circulation change in the central Himalayas indicated by a high-resolution ice core deuterium excess record |
Q56100393 | Atmospheric influence on the deuterium excess signal in polar firn: implications for ice-core interpretation |
Q28283878 | Atmospheric methane and nitrous oxide of the Late Pleistocene from Antarctic ice cores |
Q56335990 | Author Correction: Choosing the future of Antarctica |
Q58815157 | Author Correction: Palaeoclimate constraints on the impact of 2 °C anthropogenic warming and beyond |
Q56100223 | Bi-hemispheric forcing for Indo-Asian monsoon during glacial terminations |
Q30918254 | Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions |
Q56100272 | Can climate variations be inferred from tree-ring parameters and stable isotopes from Larix decidua? Juvenile effects, budmoth outbreaks, and divergence issue |
Q61046496 | Challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from Adélie Land, coastal Antarctica |
Q109933940 | Challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from Adélie Land, coastal Antarctica |
Q56100560 | Changes in European precipitation seasonality and in drought frequencies revealed by a four-century-long tree-ring isotopic record from Brittany, western France |
Q56100304 | Changes in atmospheric CO2 and its carbon isotopic ratio during the penultimate deglaciation |
Q58303925 | Characterizing atmospheric circulation signals in Greenland ice cores: insights from a weather regime approach |
Q56340101 | Choosing the future of Antarctica |
Q63964851 | Climate dependent contrast in surface mass balance in East Antarctica over the past 216 ka |
Q56100197 | Climate dependent contrast in surface mass balance in East Antarctica over the past 216 kyr |
Q56100306 | Climate of the last million years: new insights from EPICA and other records |
Q56001205 | Climate response to the Samalas volcanic eruption in 1257 revealed by proxy records |
Q56100220 | Climatic controls on water vapor deuterium excess in the marine boundary layer of the North Atlantic based on 500 days of in situ, continuous measurements |
Q56100205 | Climatic controls on water vapor deuterium excess in the marine boundary layer of the North Atlantic based on 500 days of in situ, continuous measurements |
Q59836458 | Climatic variability in Princess Elizabeth Land (East Antarctica) over the last 350 years |
Q59836461 | Climatic variability in Princess Elizabeth Land (East Antarctica) over the last 350 years |
Q64298021 | Coastal water vapor isotopic composition driven by katabatic wind variability in summer at Dumont d'Urville, coastal East Antarctica |
Q90854287 | Collapsing glaciers threaten Asia's water supplies |
Q56100225 | Combining ice core records and ice sheet models to explore the evolution of the East Antarctic Ice sheet during the Last Interglacial period |
Q56100588 | Common millennial-scale variability of Antarctic and Southern Ocean temperatures during the past 5000 years reconstructed from the EPICA Dome C ice core |
Q56100436 | Connection between South Mediterranean climate and North African atmospheric circulation during the last 50,000yrBP North Atlantic cold events |
Q56100367 | Constraining future climate change using ice core data |
Q30049024 | Continental-scale temperature variability during the past two millennia |
Q56100221 | Continuous measurements of atmospheric water vapour isotopes in Western Siberia (Kourovka) |
Q56100208 | Continuous measurements of atmospheric water vapour isotopes in western Siberia (Kourovka) |
Q57879695 | Continuous measurements of isotopic composition of water vapour on the East Antarctic Plateau |
Q61044043 | Continuous measurements of isotopic composition of water vapour on the East Antarctic Plateau |
Q58265478 | Continuous monitoring of summer surface water vapor isotopic composition above the Greenland Ice Sheet |
Q109050223 | Continuous monitoring of summer surface water vapour isotopic composition above the Greenland Ice Sheet |
Q56100307 | Deep ice cores: the need for going back in time |
Q56100240 | Deglaciation records of 17O-excess in East Antarctica: reliable reconstruction of oceanic normalized relative humidity from coastal sites |
Q56100210 | Developing a western Siberia reference site for tropospheric water vapour isotopologue observations obtained by different techniques (in situ and remote sensing) |
Q24289401 | EPICA Dome C record of glacial and interglacial intensities |
Q28266437 | Eight glacial cycles from an Antarctic ice core |
Q56864265 | Estimates of volcanic-induced cooling in the Northern Hemisphere over the past 1,500 years |
Q58092632 | Estimating Changes in Global Temperature since the Preindustrial Period |
Q58303866 | Evaluating the skills of isotope-enabled general circulation models against in situ atmospheric water vapor isotope observations |
Q56100241 | Evaluation of climate models using palaeoclimatic data |
Q56100202 | Evidence for a three-phase sequence during Heinrich Stadial 4 using a multiproxy approach based on Greenland ice core records |
Q56100592 | Evidence for stratigraphic distortion in the Greenland Ice Core Project (GRIP) ice core during Event 5e1 (120 kyr BP) from gas isotopes |
Q56100397 | Evolution du climat dans les régions polaires |
Q56100274 | Expression of the bipolar see-saw in Antarctic climate records during the last deglaciation |
Q56100308 | Firn processes and δ15N: potential for a gas-phase climate proxy |
Q56100515 | Firn-air δ15N in modern polar sites and glacial–interglacial ice: a model-data mismatch during glacial periods in Antarctica? |
Q56100190 | French summer droughts since 1326 AD: a reconstruction based on tree ring cellulose δ 18 O |
Q57891079 | French summer droughts since 1326 CE: a reconstruction based on tree ring cellulose δ18O |
Q30993404 | GRIP deuterium excess reveals rapid and orbital-scale changes in Greenland moisture origin. |
Q57734659 | Glacial–interglacial dynamics of Antarctic firn columns: comparison between simulations and ice core air-δ15N measurements |
Q123675901 | Global Warming of 1.5°C: IPCC Special Report on impacts of global warming of 1.5°C above pre-industrial levels in context of strengthening response to climate change, sustainable development, and efforts to eradicate poverty |
Q56100243 | Greenland climate change: from the past to the future |
Q30847691 | Greenland temperature response to climate forcing during the last deglaciation |
Q31159882 | High-resolution Greenland ice core data show abrupt climate change happens in few years |
Q34346930 | High-resolution record of Northern Hemisphere climate extending into the last interglacial period |
Q56100563 | Holocene climate evolution in the high-latitude Southern Hemisphere simulated by a coupled atmosphere-sea ice-ocean-vegetation model |
Q56100565 | Holocene climatic changes in Greenland: Different deuterium excess signals at Greenland Ice Core Project (GRIP) and NorthGRIP |
Q47134475 | Holocene sea ice variability driven by wind and polynya efficiency in the Ross Sea. |
Q57264354 | How has climate responded to natural perturbations? |
Q57891417 | How warm was Greenland during the last interglacial period? |
Q123675716 | IPCC 2018: SR15 summary for policymakers |
Q112834786 | Ice core evidence for decoupling between mid-latitude atmospheric water cycle and Greenland temperature during the last deglaciation |
Q61077925 | Ice core evidence for decoupling between midlatitude atmospheric water cycle and Greenland temperature during the last deglaciation |
Q56443797 | Ice melt, sea level rise and superstorms: evidence from paleoclimate data, climate modeling, and modern observations that 2 °C global warming could be dangerous |
Q21129011 | Ice melt, sea level rise and superstorms: evidence from paleoclimate data, climate modeling, and modern observations that 2 °C global warming is highly dangerous |
Q80165303 | Ice sheets and sea level |
Q61046455 | Identification of Air Masses Responsible for Warm Events on the East Antarctic Coast |
Q58118825 | Impact of precipitation intermittency on NAO-temperature signals in proxy records |
Q119315850 | Indicators of Global Climate Change 2022: Annual update of large-scale indicators of the state of the climate system and the human influence |
Q119375151 | Indicators of Global Climate Change 2022: annual update of large-scale indicators of the state of the climate system and human influence |
Q126728459 | Indicators of Global Climate Change 2023: annual update of key indicators of the state of the climate system and human influence |
Q56192284 | Influence of large-scale atmospheric circulation on marine air intrusion toward the East Antarctic coast |
Q56100310 | Insights into hydrological regime of Lake Vostok from differential behavior of deuterium and oxygen-18 in accreted ice |
Q56100406 | Insolation and sea level variations during Quaternary interglacial periods: A review of recent results with special emphasis on the last interglaciation |
Q56100413 | Interannual variability of Greenland winter precipitation sources: 2. Effects of North Atlantic Oscillation variability on stable isotopes in precipitation |
Q114109426 | Interglacial Antarctic–Southern Ocean climate decoupling due to moisture source area shifts |
Q58320759 | Is there 1.5 million-year old ice near Dome C, Antarctica? |
Q58320757 | Is there 1.5-million-year-old ice near Dome C, Antarctica? |
Q57878206 | Isotopic exchange on the diurnal scale between near-surface snow and lower atmospheric water vapor at Kohnen station, East Antarctica |
Q56100568 | Large temperature variations over rapid climatic events in Greenland: a method based on air isotopic measurements |
Q57892355 | Large-scale drivers of Caucasus climate variability in meteorological records and Mt El'brus ice cores |
Q59836462 | Large-scale drivers of Caucasus climate variability in meteorological records and Mt Elbrus ice cores |
Q56100278 | Links between MIS 11 millennial to sub-millennial climate variability and long term trends as revealed by new high resolution EPICA Dome C deuterium data – A comparison with the Holocene |
Q56100446 | Millenial scale variations of the isotopic composition of atmospheric oxygen over Marine Isotopic Stage 4 |
Q56100312 | Millennial and sub-millennial scale climatic variations recorded in polar ice cores over the last glacial period |
Q56100531 | Modeling the isotopic composition of Antarctic snow using backward trajectories: Simulation of snow pit records |
Q56100280 | Modeling the water isotopes in Greenland precipitation 1959–2001 with the meso-scale model REMO-iso |
Q56100600 | Modelling the isotopic composition of snow using backward trajectories: a particular precipitation event in Dronning Maud Land, Antarctica |
Q56100611 | Modern precipitation stable isotope vs. elevation gradients in the High Himalaya. Comment on “A new approach to stable isotope-based paleoaltimetry: implications for paleoaltimetry and paleohypsometry of the High Himalaya since the Late Miocene” |
Q58265451 | Moisture sources and synoptic to seasonal variability of North Atlantic water vapor isotopic composition |
Q56100215 | Multi-proxy fingerprint of Heinrich event 4 in Greenland ice core records |
Q56100314 | New MIS 19 EPICA Dome C high resolution deuterium data: Hints for a problematic preservation of climate variability at sub-millennial scale in the “oldest ice” |
Q114667830 | Ocean as the main driver of Antarctic ice sheet retreat during the Holocene |
Q56100245 | On the gas-ice depth difference (Δdepth) along the EPICA Dome C ice core |
Q56100542 | On the limits of Antarctic and marine climate records synchronization: Lag estimates during marine isotopic stages 5d and 5c |
Q34646794 | Orbital and millennial Antarctic climate variability over the past 800,000 years. |
Q31155450 | Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years |
Q56100621 | Oxygen isotope and palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and NorthGRIP |
Q56658823 | Palaeoclimate constraints on the impact of 2 °C anthropogenic warming and beyond |
Q56100317 | Paleoclimates: what do we learn from deep ice cores? |
Q28596056 | Paradoxical cold conditions during the medieval climate anomaly in the Western Arctic |
Q29999539 | Past and future polar amplification of climate change: climate model intercomparisons and ice-core constraints |
Q118117969 | Past temperature reconstructions from deep ice cores: relevance for future climate change |
Q57891146 | Phase relationships between orbital forcing and the composition of air trapped in Antarctic ice cores |
Q56100195 | Phase relationships between orbital forcing and the composition of air trapped in Antarctic ice cores |
Q56100283 | Precipitation Water Stable Isotopes in the South Tibetan Plateau: Observations and Modeling* |
Q57879078 | Precipitation regime and stable isotopes at Dome Fuji, East Antarctica |
Q56100551 | Publisher’s Erratum: Past and future polar amplification of climate change: climate model intercomparisons and ice-core constraints |
Q56100602 | Quantification of rapid temperature change during DO event 12 and phasing with methane inferred from air isotopic measurements |
Q56100248 | Ranges of moisture-source temperature estimated from Antarctic ice cores stable isotope records over glacial–interglacial cycles |
Q56100573 | Rapid climate variability during warm and cold periods in polar regions and Europe |
Q56100575 | Rapid deuterium-excess changes in Greenland ice cores: a link between the ocean and the atmosphere |
Q114141186 | Recent Progress and Emerging Topics on Weather and Climate Extremes Since the Fifth Assessment Report of the Intergovernmental Panel on Climate Change |
Q56100200 | Recent changes in north-west Greenland climate documented by NEEM shallow ice core data and simulations, and implications for past temperature reconstructions |
Q56100192 | Recent changes in north-west Greenland climate documented by NEEM shallow ice core data and simulations, and implications for past-temperature reconstructions |
Q56100612 | Recent southern Indian Ocean climate variability inferred from a Law Dome ice core: new insights for the interpretation of coastal Antarctic isotopic records |
Q61046402 | Reconciling glacial Antarctic water stable isotopes with ice sheet topography and the isotopic paleothermometer |
Q56100577 | Reconstructing the variability of the climate system: Facts and theories |
Q56100554 | Reconstruction of past precipitation δ18O using tree-ring cellulose δ18O and δ13C: A calibration study near Lac d'Annecy, France |
Q56100251 | Reconstruction of southeast Tibetan Plateau summer climate using tree ring δ18O: moisture variability over the past two centuries |
Q56100603 | Reconstruction of summer droughts using tree-ring cellulose isotopes: a calibration study with living oaks from Brittany (western France) |
Q115485122 | Reconstruction of summer droughts using tree-ring cellulose isotopes: a calibration study with living oaks from Brittany (western France) |
Q56100252 | Regional imprints of millennial variability during the MIS 3 period around Antarctica |
Q63645558 | Regional seesaw between North Atlantic and Nordic Seas during the last glacial abrupt climate events |
Q57892257 | Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events |
Q56100616 | Relative Timing of Deglacial Climate Events in Antarctica and Greenland |
Q57973829 | Retrieving the paleoclimatic signal from the deeper part of the EPICA Dome C ice core |
Q56100284 | Sampling strategy and climatic implications of tree-ring stable isotopes on the southeast Tibetan Plateau |
Q56100288 | Sensitivity of interglacial Greenland temperature and δ18O: ice core data, orbital and increased CO2 climate simulations |
Q58265443 | Sequence of events from the onset to the demise of the Last Interglacial: Evaluating strengths and limitations of chronologies used in climatic archives |
Q56100472 | Signal strength and climate calibration of a European tree-ring isotope network |
Q57053074 | Six research priorities for cities and climate change |
Q56100230 | Snow accumulation and its moisture origin over Dome Argus, Antarctica |
Q59468516 | Southern Tibetan Plateau ice core δ18O reflects abrupt shifts in atmospheric circulation in the late 1970s |
Q56100617 | Spatial and temporal variability in isotope composition of recent snow in the vicinity of Vostok station, Antarctica: implications for ice-core record interpretation |
Q61046459 | Spatial distribution of 17O-excess in surface snow along a traverse from Zhongshan station to Dome A, East Antarctica |
Q58265500 | Spatial gradients of temperature, accumulation and δ 18 O-ice in Greenland over a series of Dansgaard-Oeschger events |
Q58265481 | Spatial gradients of temperature, accumulation and δ¹⁸O-ice in Greenland over a series of Dansgaard–Oeschger events |
Q28283869 | Stable carbon cycle-climate relationship during the Late Pleistocene |
Q61046416 | Stable isotopes in surface snow along a traverse route from Zhongshan station to Dome A, East Antarctica |
Q115957443 | Summer Temperature over the Tibetan Plateau Modulated by Atlantic Multidecadal Variability |
Q56100372 | Summer maximum temperature in northern France over the past century: instrumental data versus multiple proxies (tree-ring isotopes, grape harvest dates and forest fires) |
Q57240311 | Summer temperature trend over the past two millennia using air content in Himalayan ice |
Q109539654 | Supplementary material to "Antarctic climate variability at regional and continental scales over the last 2,000 years" |
Q114958140 | Supplementary material to "Archival of the water stable isotope signal in East Antarctic ice cores" |
Q114958137 | Supplementary material to "Archival processes of the water stable isotope signal in East Antarctic ice cores" |
Q114958146 | Supplementary material to "Climatic variability in Princess Elizabeth Land (East Antarctica) over the last 350 years" |
Q112834787 | Supplementary material to "Ice core evidence for decoupling between mid-latitude atmospheric water cycle and Greenland temperature during the last deglaciation" |
Q111726657 | Supplementary material to "Large-scale drivers of Caucasus climate variability in meteorological records and Mt Elbrus ice cores" |
Q56100319 | Synchronising EDML and NorthGRIP ice cores using δ18O of atmospheric oxygen (δ18Oatm) and CH4 measurements over MIS5 (80–123 kyr) |
Q34035857 | Synchronous change of atmospheric CO2 and Antarctic temperature during the last deglacial warming |
Q56100290 | TALDICE-1 age scale of the Talos Dome deep ice core, East Antarctica |
Q24273405 | Target Atmospheric CO2: Where Should Humanity Aim? |
Q57991195 | Temperature trends during the Present and Last Interglacial periods – a multi-model-data comparison |
Q58650446 | Temporal and spatial structure of multi-millennial temperature changes at high latitudes during the Last Interglacial |
Q56100500 | The GRIP deuterium-excess record |
Q122389773 | The Southern Hemisphere at glacial terminations: insights from the Dome C ice core |
Q56100323 | The deuterium excess records of EPICA Dome C and Dronning Maud Land ice cores (East Antarctica) |
Q56100556 | The glacial inception as recorded in the NorthGRIP Greenland ice core: timing, structure and associated abrupt temperature changes |
Q109934472 | The influence of the synoptic regime on stable water isotopes in precipitation at Dome C, East Antarctica |
Q56192286 | The influence of volcanic eruptions on weather regimes over the North Atlantic simulated by ECHAM5/MPI-OM ensemble runs from 800 to 2000 CE |
Q56100214 | The isotopic composition of water vapour and precipitation in Ivittuut, southern Greenland |
Q56100294 | The last deglaciation: timing the bipolar seesaw |
Q58083486 | The recent warming trend in North Greenland |
Q115607770 | The response of relative humidity to centennial-scale warming over the southeastern Tibetan Plateau inferred from tree-ring width chronologies |
Q58315207 | The summer 2012 Greenland heat wave: In situ and remote sensing observations of water vapor isotopic composition during an atmospheric river event |
Q57879215 | Three-year monitoring of stable isotopes of precipitation at Concordia Station, East Antarctica |
Q56100622 | Tibetan Plateau summer monsoon northward extent revealed by measurements of water stable isotopes |
Q56100256 | Towards orbital dating of the EPICA Dome C ice core using δO2/N2 |
Q56100425 | Transferring radiometric dating of the last interglacial sea level high stand to marine and ice core records |
Q63970968 | Tree age, site and climate controls on tree ring cellulose δ18O: A case study on oak trees from south-western France |
Q56100504 | Tree-rings and the climate of New Caledonia (SW Pacific) |
Q56100579 | Trends in sub-annual climate variability since the Little Ice Age in western Europe |
Q56100259 | Triple isotopic composition of oxygen in surface snow and water vapor at NEEM (Greenland) |
Q110603737 | Two-phase change in CO2, Antarctic temperature and global climate during Termination II |
Q56100261 | Uncertainties in elevation changes and their impact on Antarctic temperature records since the end of the last glacial period |
Q56100296 | Understanding the climatic signal in the water stable isotope records from the NEEM shallow firn/ice cores in northwest Greenland |
Q56100334 | Understanding the17O excess glacial-interglacial variations in Vostok precipitation |
Q110676558 | Unprecedented recent warming rate and temperature variability over the east Tibetan Plateau inferred from Alpine treeline dendrochronology |
Q58083702 | Unstable ice stream in Greenland during the Younger Dryas cold event |
Q110920881 | Using data assimilation to investigate the causes of Southern Hemisphere high latitude cooling from 10 to 8 ka BP |
Q56527536 | Using palaeo-climate comparisons to constrain future projections in CMIP5 |
Q119633263 | Using paleo-climate model/data comparisons to constrain future projections |
Q56100212 | Variations of oxygen-18 in West Siberian precipitation during the last 50 years |
Q56100262 | Volcanic synchronisation between the EPICA Dome C and Vostok ice cores (Antarctica) 0–145 kyr BP |
Q56100606 | Vulnerability of two European lakes in response to future climatic changes |
Q58650462 | Warm climate isotopic simulations: what do we learn about interglacial signals in Greenland ice cores? |
Q57891137 | Water and carbon stable isotope records from natural archives: a new database and interactive online platform for data browsing, visualizing and downloading |
Q61046403 | Water stable isotope spatio-temporal variability in Antarctica in 1960–2013: observations and simulations from the ECHAM5-wiso atmospheric general circulation model |
Q57268600 | Water-use efficiency and transpiration across European forests during the Anthropocene |
Q24289402 | What caused Earth's temperature variations during the last 800,000 years? Data-based evidence on radiative forcing and constraints on climate sensitivity |
Q56100217 | What controls the isotopic composition of Greenland surface snow? |
Q29304236 | What drives the millennial and orbital variations of δ18Oatm? |
Q56100267 | Where might we find evidence of a Last Interglacial West Antarctic Ice Sheet collapse in Antarctic ice core records? |
Q56100357 | Winter 2010 in Europe: A cold extreme in a warming climate |
Q56100506 | Wood Cellulose Preparation Methods and Mass Spectrometric Analyses of δ13C, δ18O, and Nonexchangeable δ2H Values in Cellulose, Sugar, and Starch: An Interlaboratory Comparison |
Q57027911 | Young people's burden: requirement of negative CO2 emissions |
Q58115300 | Young people's burden: requirement of negative CO2 emissions |
Q21028340 | Sylvie Joussaume | doctoral student | P185 |
Q114081107 | Marc Delmotte | spouse | P26 |
Q108133155 | Climate Change 2021: The Physical Science Basis | editor | P98 |
Category:Valérie Masson-Delmotte | wikimedia | |
Arabic (ar / Q13955) | فاليري ماسون-ديلموت | wikipedia |
bcl | Valerie Masson-Delmotte | wikipedia |
cy | Valérie Masson-Delmotte | wikipedia |
Valérie Masson-Delmotte | wikipedia | |
Valerie Masson-Delmotte | wikipedia | |
Valérie Masson-Delmotte | wikipedia | |
Valerie Masson-Delmotte | wikipedia | |
Valérie Masson-Delmotte | wikipedia | |
Valérie Masson-Delmotte | wikipedia | |
mg | Valérie Masson-Delmotte | wikipedia |
mk | Валери Масон-Делмот | wikipedia |
Valérie Masson-Delmotte | wikipedia | |
Массон-Дельмот, Валери | wikipedia | |
tl | Valerie Masson-Delmotte | wikipedia |
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