about
High-resolution interpolar difference of atmospheric methane around the Last Glacial MaximumIsotopic constraints on marine and terrestrial N2O emissions during the last deglaciation.A gas chromatography/combustion/isotope ratio mass spectrometry system for high-precision delta13C measurements of atmospheric methane extracted from ice core samples.A gas chromatography/pyrolysis/isotope ratio mass spectrometry system for high-precision deltaD measurements of atmospheric methane extracted from ice cores.Hydrogen isotopes preclude marine hydrate CH4 emissions at the onset of Dansgaard-Oeschger events.Carbon isotope constraints on the deglacial CO₂ rise from ice cores.Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records.Stable isotope constraints on Holocene carbon cycle changes from an Antarctic ice core.Changing boreal methane sources and constant biomass burning during the last termination.Amount-dependent isotopic fractionation during compound-specific isotope analysis.The EPICA Dronning Maud Land deep drilling operationComparative carbon cycle dynamics of the present and last interglacialInterlaboratory comparison of <i>δ</i><sup>13</sup>C and <i>δ</i>D measurements of atmospheric CH<sub>4</sub> for combined use of data sets from different laboratoriesIntercomparisons of δ<sup>13</sup>C and δD measurements of atmospheric CH<sub>4</sub> for combined use of datasets from different laboratoriesOn the interference of Kr during carbon isotope analysis of methane using continuous-flow combustion–isotope ratio mass spectrometrySimultaneous stable isotope analysis of methane and nitrous oxide on ice core samplesClimatic and insolation control on the high-resolution total air content in the NGRIP ice coreA 156 kyr smoothed history of the atmospheric greenhouse gases CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O and their radiative forcingBipolar carbon and hydrogen isotope constraints of the Holocene methane budgetComment on "Changes in atmospheric CO 2 levels recorded by the isotopic signature of n -alkanes from plants" from K.S. Machado and S. FroehnerContinuous records of the atmospheric greenhouse gases CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>O and their radiative forcing since the penultimate glacial maximumEvolution of the stable carbon isotope composition of atmospheric CO2over the last glacial cycleStratospheric age of air variations between 1600 and 2100Climatic and insolation control on the high-resolution total air content in the NGRIP ice coreComment on “Synchronous records of pCO2 and Δ14C suggest rapid, ocean-derived pCO2 fluctuations at the onset of Younger Dryas” by Steinthorsdottir et alRevision of the EPICA Dome C CO2 record from 800 to 600 kyr before presentOnline technique for isotope and mixing ratios of CH<sub>4</sub>, N<sub>2</sub>O, Xe and mixing ratios of organic trace gases on a single ice core sampleImproving accuracy and precision of ice core δD(CH<sub>4</sub>) analyses using methane pre-pyrolysis and hydrogen post-pyrolysis trapping and subsequent chromatographic separationOnline technique for isotope and mixing ratios of CH 4 , N 2 O, Xe and mixing ratios of organic trace gases on a single ice core sampleImproving accuracy and precision of ice core δD (CH 4 ) analyses using methane pre- and hydrogen post-pyrolysis trapping and subsequent chromatographic separationA reconstruction of atmospheric carbon dioxide and its stable carbon isotopic composition from the penultimate glacial maximum to the last glacial inceptionA high resolution record of atmospheric carbon dioxide and its stable carbon isotopic composition from the penultimate glacial maximum to the glacial inceptionOn the interference of 86 Kr 2+ during carbon isotope analysis of atmospheric methane using continuous flow combustion – isotope ratio mass spectrometryIndependent variations of CH4 emissions and isotopic composition over the past 160,000 yearsA sublimation technique for high-precision measurements of δ<sup>13</sup>CO<sub>2</sub> and mixing ratios of CO<sub>2</sub> and N<sub>2</sub>O from air trapped in ice coresAtmosphericδ13CO2and its relation topCO2and deep oceanδ13C during the late PleistoceneThe role of Southern Ocean processes in orbital and millennial CO2 variations – A synthesisAn Improved Continuous Flow Analysis System for High-Resolution Field Measurements on Ice CoresN<sub>2</sub>O changes from the Last Glacial Maximum to the preindustrial – Part I: Quantitative reconstruction of terrestrial and marine emissions using N<sub>2</sub>O stable isotopes in ice coresN<sub>2</sub>O changes from the Last Glacial Maximum to the preindustrial – Part II: Terrestrial N<sub>2</sub>O emissions constrain carbon-nitrogen interactions
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description
hulumtues
@sq
researcher
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ricercatore
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wetenschapper
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հետազոտող
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name
Jochen Schmitt
@ast
Jochen Schmitt
@en
Jochen Schmitt
@es
Jochen Schmitt
@nl
Jochen Schmitt
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type
label
Jochen Schmitt
@ast
Jochen Schmitt
@en
Jochen Schmitt
@es
Jochen Schmitt
@nl
Jochen Schmitt
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altLabel
Switzerland Jochen Schmitt @ Uni Bern
@en
prefLabel
Jochen Schmitt
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Jochen Schmitt
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Jochen Schmitt
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Jochen Schmitt
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Jochen Schmitt
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P214
P1053
B-7893-2009
P106
P1153
15059421100
P21
P214
P31
P3829
P496
0000-0003-4695-3029
P734
P735
P7859
viaf-13475871