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V. Masson Delmotte
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V. Masson Delmotte
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Sensitivity of interglacial Greenland temperature and δ 18 O: ice core data, orb...
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Archival processes of the water stable isotope signal in East Antarctic ice core...
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Archival processes of the water stable isotope signal in East Antarctic ice core...
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Sensitivity of interglacial Greenland temperature and δ18O: ice core data, orbit...
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Impact of precipitation intermittency on NAO-temperature signals in proxy record...
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Impact of precipitation intermittency on NAO-temperature signals in proxy record...
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Evidence for a three-phase sequence during Heinrich Stadial 4 using a multiproxy...
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Evidence for a three-phase sequence during Heinrich Stadial 4 using a multiproxy...
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Climate of the Past Towards orbital dating of the EPICA Dome C ice core using δO...
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TALDICE-1 age scale of the Talos Dome deep ice core, East Antarctica
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TALDICE-1 age scale of the Talos Dome deep ice core, East Antarctica
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Stable isotope records from the new TALDICE ice core(East Antarctica)
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Past temperature reconstructions from deep ice cores: relevance for future clima...
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Three-year monitoring of stable isotopes of precipitation at Concordia Station,...
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Past temperature reconstructions from deep ice cores: relevance for future clima...
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Glacial–interglacial dynamics of Antarctic firn columns: comparison between simu...
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Glacial–interglacial dynamics of Antarctic firn columns: comparison between simu...
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Three-year monitoring of stable isotopes of precipitation at Concordia Station,...
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Antarctic temperature changes during the last millennium: evaluation of simulati...
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Spatial gradients of temperature, accumulation and δ 18 O-ice in Greenland over...
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Related Subjects
Environmental sciences
GE1-350
envir
geo
Environmental pollution
Environmental protection
TD169-171.8
TD172-193.5
Antarctica
ice core
Geology
QE1-996.5
Greenland
paleoclimate
water vapor
Chemistry
Physics
QC1-999
QD1-999
Ice core
Paleoclimate
interglacial
water stable isotope
Climate model
Data assimilation
Southern Hemisphere
Temperature
stable isotope
Dome C
GCM
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