about
Northern Hemisphere forcing of climatic cycles in Antarctica over the past 360,000 yearsIce record of delta13C for atmospheric CH4 across the Younger Dryas-Preboreal transitionNitrogen trifluoride global emissions estimated from updated atmospheric measurementsLittle Ice Age cold interval in West Antarctica: Evidence from borehole temperature at the West Antarctic Ice Sheet (WAIS) Divide4±1.5 °C abrupt warming 11,270 yr ago identified from trapped air in Greenland iceRadiometric 81Kr dating identifies 120,000-year-old ice at Taylor Glacier, AntarcticaGreenland temperature response to climate forcing during the last deglaciation.Isotopic constraints on marine and terrestrial N2O emissions during the last deglaciation.Oxygen-18 of O2 records the impact of abrupt climate change on the terrestrial biosphere.Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation.Deglacial temperature history of West Antarctica.Paleoclimate. Enhanced tropical methane production in response to iceberg discharge in the North Atlantic.Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletionAtmospheric science. Monsoons and meltdowns.14CH4 measurements in Greenland ice: investigating last glacial termination CH4 sources.New methods for measuring atmospheric heavy noble gas isotope and elemental ratios in ice core samples.Climate change: Southern see-saw seen.Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar icePrecise timing and characterization of abrupt climate change 8200 years ago from air trapped in polar iceThe Ross Sea Dipole – temperature, snow accumulation and sea ice variability in the Ross Sea region, Antarctica, over the past 2700 yearsTiming of atmospheric CO2 and Antarctic temperature changes across termination IIIObserving and modeling the influence of layering on bubble trapping in polar firnDeep air convection in the firn at a zero-accumulation site, central AntarcticaOxygen loss in biosphere 2Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprintDispersion in deep polar firn driven by synoptic-scale surface pressure variabilityAtmospheric gas records from Taylor Glacier, Antarctica, reveal ancient ice with ages spanning the entire last glacial cycleWave inhibition by sea ice enables trans-Atlantic ice rafting of debris during Heinrich eventsThe influence of layering and barometric pumping on firn air transport in a 2D modelWhere to find 1.5 million yr old ice for the IPICS "Oldest-Ice" ice coreThe recent warming trend in North GreenlandDifferentiating bubble-free layers from melt layers in ice cores using noble gasesHigh variability of Greenland surface temperature over the past 4000 years estimated from trapped air in an ice corePersistent multi-decadal Greenland temperature fluctuation through the last millenniumArgon and nitrogen isotopes of trapped air in the GISP2 ice core during the Holocene epoch (0–11,500 B.P.): Methodology and implications for gas loss processesA redetermination of the isotopic abundances of atmospheric ArConvective mixing of air in firn at four polar sitesA record of atmospheric halocarbons during the twentieth century from polar firn airAn 83 000 year old ice core from Roosevelt Island, Ross Sea, AntarcticaThe Ross Sea Dipole – Temperature, Snow Accumulation and Sea Ice Variability in the Ross Sea Region, Antarctica, over the Past 2,700 Years
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P50
description
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Jeffrey P Severinghaus
@ast
Jeffrey P Severinghaus
@en
Jeffrey P Severinghaus
@es
Jeffrey P Severinghaus
@nl
type
label
Jeffrey P Severinghaus
@ast
Jeffrey P Severinghaus
@en
Jeffrey P Severinghaus
@es
Jeffrey P Severinghaus
@nl
prefLabel
Jeffrey P Severinghaus
@ast
Jeffrey P Severinghaus
@en
Jeffrey P Severinghaus
@es
Jeffrey P Severinghaus
@nl
P106
P31
P496
0000-0001-8883-3119