about
Natural and anthropogenic variations in methane sources during the past two millennia.Methane emissions from terrestrial plants under aerobic conditions.Methoxyl groups of plant pectin as a precursor of atmospheric methane: evidence from deuterium labelling studies.Dynamic processes governing lower-tropospheric HDO/H2O ratios as observed from space and ground.Rapid Sediment Accumulation Results in High Methane Effluxes from Coastal SedimentsIron-mediated anaerobic oxidation of methane in brackish coastal sediments.Statistical clumped isotope signatures.Influence of flooding on delta15N, delta18O, 1delta15N and 2delta15N signatures of N2O released from estuarine soils--a laboratory experiment using tidal flooding chambers.Characterisation of the semi-volatile component of Dissolved Organic Matter by Thermal Desorption - Proton Transfer Reaction - Mass Spectrometry.Correction of mass spectrometric isotope ratio measurements for isobaric isotopologues of O2, CO, CO2, N2O and SO2.Gas chromatography/isotope-ratio mass spectrometry method for high-precision position-dependent 15N and 18O measurements of atmospheric nitrous oxide.A new continuous flow isotope ratio mass spectrometry system for the analysis of delta2H, delta17O and delta18O of small (120 microg) water samples in atmospheric applications.Iconic CO2 time series at risk.Newly detected ozone-depleting substances in the atmosphereAnaerobic oxidation of methane alters sediment records of sulfur, iron and phosphorus in the Black SeaMethane emissions from floodplains in the Amazon Basin: challenges in developing a process-based model for global applicationsCorrection to “Interannual variability of carbon monoxide emission estimates over South America from 2006 to 2010”Interannual variability of carbon monoxide emission estimates over South America from 2006 to 2010Optimizing global CO emission estimates using a four-dimensional variational data assimilation system and surface network observationsEarly anthropogenic CH4emissions and the variation of CH4and13CH4over the last millenniumSources and atmospheric processing of size segregated aerosol particles revealed by stable carbon isotope ratios and chemical speciationBrief communication: Analysis of organic matter in surface snow by PTR-MS – implications for dry deposition dynamics in the AlpsThe impact of precipitation evaporation on the atmospheric aerosol distribution in EC-Earth v3.2.0Interlaboratory 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 laboratoriesQuantification of CO emissions from the city of Madrid using MOPITT satellite retrievals and WRF simulationsIntercomparisons of δ<sup>13</sup>C and δD measurements of atmospheric CH<sub>4</sub> for combined use of datasets from different laboratoriesChemical and isotopic composition of secondary organic aerosol generated by <i>α</i>-pinene ozonolysisRetrievals of heavy ozone with MIPASIn situ observations of the isotopic composition of methane at the Cabauw tall tower siteDevelopment and evaluation of a suite of isotope reference gases for methane in airReal-time analysis of <i>δ</i><sup>13</sup>C- and <i>δ</i>D-CH<sub>4</sub> in ambient air with laser spectroscopy: method development and first intercomparison resultsIsotopic signatures of production and uptake of H<sub>2</sub> by soilOn the use of satellite-derived CH<sub>4</sub> : CO<sub>2</sub> columns in a joint inversion of CH<sub>4</sub> and CO<sub>2</sub> fluxesDevelopment of an atmospheric N<sub>2</sub>O isotopocule model and optimization procedure, and application to source estimationChlorine isotope composition in chlorofluorocarbons CFC-11, CFC-12 and CFC-113 in firn, stratospheric and tropospheric airGlobal-scale remote sensing of water isotopologues in the troposphere: representation of first-order isotope effectsContinuous-flow IRMS technique for determining the <sup>17</sup>O excess of CO<sub>2</sub> using complete oxygen isotope exchange with cerium oxideSoil carbon content and relative abundance of high affinity H2-oxidizing bacteria predict atmospheric H2 soil uptake activity better than soil microbial community compositionThe effect of stratospheric sulfur from Mount Pinatubo on tropospheric oxidizing capacity and methaneHESS Opinions "A perspective on isotope versus non-isotope approaches to determine the contribution of transpiration to total evaporation"
P50
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P50
description
hulumtues
@sq
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Thomas Röckmann
@ast
Thomas Röckmann
@en
Thomas Röckmann
@es
Thomas Röckmann
@nl
Thomas Röckmann
@sl
type
label
Thomas Röckmann
@ast
Thomas Röckmann
@en
Thomas Röckmann
@es
Thomas Röckmann
@nl
Thomas Röckmann
@sl
prefLabel
Thomas Röckmann
@ast
Thomas Röckmann
@en
Thomas Röckmann
@es
Thomas Röckmann
@nl
Thomas Röckmann
@sl
P1053
F-4479-2015
P106
P1153
7003501766
P21
P31
P3829
P3835
thomas-rckmann
P496
0000-0002-6688-8968