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Martin Heimann

Biographic Data

ID5597357
NAMEMartin Heimann
GIVEN NAMESMartin
FAMILY NAMEHeimann
SIGNATUREHEIMANN M
AFFILIATIONSMax Planck Institute for Biogeochemistry
ORCID0000-0001-6296-5113
VERIFIEDYes
TOTAL WORKS6
TOTAL CITATIONS24
WORKS AS AUTHOR6
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1980
LATEST PUBLICATION YEAR2017
H-INDEX2
  • Contrasting and interacting changes in simulated spring and summer carbon cycle extremes in European ecosystems

    Open Access•Sebastian Sippel, Matthias Forkel et al.•ARTICLE•Environmental Research Letters•2017

    Climate extremes have the potential to cause extreme responses of terrestrial ecosystem functioning. However, it is neither straightforward to quantify and predict extreme ecosystem responses, nor to attribute these responses to specific climate drivers. Here, we construct a factorial experiment based on a large ensemble of process-oriented ecosystem model simulations driven by a regional climate model (12 500 model years in 1985–2010) in six Eur…

  • The carbon budget of the northern cryosphere region

    Open Access•A D McGuire, Robie W Macdonald et al.•ARTICLE•Current Opinion in Environmental…•2010•Cited by: 1

  • Modelling terrestrial vegetation dynamics and carbon cycling for an abrupt climatic change event

    Open Access•Marko Scholze, Wolfgang Knorr et al.•ARTICLE•The Holocene•2003•References: 4

    Abrupt climatic changes have occurred several times in the past, leading to large-scale modifications of vegetation patterns with important consequences for the global carbon cycle. Dynamic global vegetation models (DGVM) constitute an advanced tool for reconstructing past or predicting future shifts in vegetation distributions in response to climatic change on a global scale. The Lund-Potsdam-Jena (LPJ) model is a DGVM that also includes a compl…

  • Water isotope modeling in the Asian monsoon region

    Open Access•Georg Hoffmann, Martin Heimann•ARTICLE•Quaternary International•1997

  • Low-Level Gas Proportional Counting in An Underground Laboratory

    Open Access•H H Loosli, Martin Heimann et al.•ARTICLE•Radiocarbon•1980•Cited by: 7•References: 3

    Results of measurements in an underground laboratory, 70m of water equivalent below surface, are given. Background values of proportional gas counters with volumes between 16cc and 1.5L are lower by a factor of 2—4.5 compared to the values in the previously used laboratory (7m w.e.). High counting gas pressures, up to 5 at CH 4 and up to 36 at P-10, enable the use of relatively small counters with correspondingly small background contributions fr…

  • C Variations Caused by Changes in the Global Carbon Cycle

    Open Access•Ulrich Siegenthaler, Martin Heimann et al.•ARTICLE•Radiocarbon•1980•Cited by: 16•References: 24

    A box-diffusion model for the carbon cycle is used to estimate the magnitude of 14 C variations caused by changes of reservoir sizes and exchange fluxes in the global carbon system. The influence of changes in atmospheric CO 2 concentration, biomass, CO 2 exchange rate between atmosphere and ocean, and ocean mixing is considered. Steady-state 14 C concentrations as well as the transients are calculated. For changing biomass, atmospheric CO 2 leve…

  • C Variations Caused by Changes in the Global Carbon Cycle

    Open Access•Ulrich Siegenthaler, Martin Heimann et al.•ARTICLE•Radiocarbon•1980•Cited by: 16•References: 24

    A box-diffusion model for the carbon cycle is used to estimate the magnitude of 14 C variations caused by changes of reservoir sizes and exchange fluxes in the global carbon system. The influence of changes in atmospheric CO 2 concentration, biomass, CO 2 exchange rate between atmosphere and ocean, and ocean mixing is considered. Steady-state 14 C concentrations as well as the transients are calculated. For changing biomass, atmospheric CO 2 leve…

  • Low-Level Gas Proportional Counting in An Underground Laboratory

    Open Access•H H Loosli, Martin Heimann et al.•ARTICLE•Radiocarbon•1980•Cited by: 7•References: 3

    Results of measurements in an underground laboratory, 70m of water equivalent below surface, are given. Background values of proportional gas counters with volumes between 16cc and 1.5L are lower by a factor of 2—4.5 compared to the values in the previously used laboratory (7m w.e.). High counting gas pressures, up to 5 at CH 4 and up to 36 at P-10, enable the use of relatively small counters with correspondingly small background contributions fr…

  • The carbon budget of the northern cryosphere region

    Open Access•A D McGuire, Robie W Macdonald et al.•ARTICLE•Current Opinion in Environmental…•2010•Cited by: 1

  • Low-Level Gas Proportional Counting in An Underground Laboratory

    Open Access•H H Loosli, Martin Heimann et al.•ARTICLE•Radiocarbon•1980•Cited by: 7•References: 3

    Results of measurements in an underground laboratory, 70m of water equivalent below surface, are given. Background values of proportional gas counters with volumes between 16cc and 1.5L are lower by a factor of 2—4.5 compared to the values in the previously used laboratory (7m w.e.). High counting gas pressures, up to 5 at CH 4 and up to 36 at P-10, enable the use of relatively small counters with correspondingly small background contributions fr…

  • C Variations Caused by Changes in the Global Carbon Cycle

    Open Access•Ulrich Siegenthaler, Martin Heimann et al.•ARTICLE•Radiocarbon•1980•Cited by: 16•References: 24

    A box-diffusion model for the carbon cycle is used to estimate the magnitude of 14 C variations caused by changes of reservoir sizes and exchange fluxes in the global carbon system. The influence of changes in atmospheric CO 2 concentration, biomass, CO 2 exchange rate between atmosphere and ocean, and ocean mixing is considered. Steady-state 14 C concentrations as well as the transients are calculated. For changing biomass, atmospheric CO 2 leve…

  • Water isotope modeling in the Asian monsoon region

    Open Access•Georg Hoffmann, Martin Heimann•ARTICLE•Quaternary International•1997

  • Modelling terrestrial vegetation dynamics and carbon cycling for an abrupt climatic change event

    Open Access•Marko Scholze, Wolfgang Knorr et al.•ARTICLE•The Holocene•2003•References: 4

    Abrupt climatic changes have occurred several times in the past, leading to large-scale modifications of vegetation patterns with important consequences for the global carbon cycle. Dynamic global vegetation models (DGVM) constitute an advanced tool for reconstructing past or predicting future shifts in vegetation distributions in response to climatic change on a global scale. The Lund-Potsdam-Jena (LPJ) model is a DGVM that also includes a compl…

  • The carbon budget of the northern cryosphere region

    Open Access•A D McGuire, Robie W Macdonald et al.•ARTICLE•Current Opinion in Environmental…•2010•Cited by: 1

  • Contrasting and interacting changes in simulated spring and summer carbon cycle extremes in European ecosystems

    Open Access•Sebastian Sippel, Matthias Forkel et al.•ARTICLE•Environmental Research Letters•2017

    Climate extremes have the potential to cause extreme responses of terrestrial ecosystem functioning. However, it is neither straightforward to quantify and predict extreme ecosystem responses, nor to attribute these responses to specific climate drivers. Here, we construct a factorial experiment based on a large ensemble of process-oriented ecosystem model simulations driven by a regional climate model (12 500 model years in 1985–2010) in six Eur…

Environmental Science (6 works) · Geology (6 works) · Atmospheric sciences (5 works) · Climatology (5 works) · Carbon cycle (4 works) · Ecology (4 works) · Ecosystem (4 works) · Oceanography (4 works) · Atmospheric and Environmental Gas Dynamics (3 works) · Climate change (3 works)

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