Hasil Pencarian - M.C. Krol

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  1. 1
    McSCIA: application of the Equivalence Theorem in a Monte Carlo radiative transfer model for spherical shell atmospheres

    McSCIA: application of the Equivalence Theorem in a Monte Carlo radiative transfer model for spherical shell atmospheres oleh F. Spada, M. C. Krol, M. C. Krol, M. C. Krol, P. Stammes

    Diterbitkan 2006-01-01
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  2. 2
    ICLASS 1.1, a variational Inverse modelling framework for the Chemistry Land-surface Atmosphere Soil Slab model: description, validation, and application

    ICLASS 1.1, a variational Inverse modelling framework for the Chemistry Land-surface Atmosphere Soil Slab model: description, validation, and application oleh P. J. M. Bosman, M. C. Krol, M. C. Krol

    Diterbitkan 2023-01-01
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  3. 3
    A three-dimensional-model inversion of methyl chloroform to constrain the atmospheric oxidative capacity

    A three-dimensional-model inversion of methyl chloroform to constrain the atmospheric oxidative capacity oleh S. Naus, S. A. Montzka, P. K. Patra, P. K. Patra, M. C. Krol, M. C. Krol

    Diterbitkan 2021-03-01
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  4. 4
    A consistent molecular hydrogen isotope chemistry scheme based on an independent bond approximation

    A consistent molecular hydrogen isotope chemistry scheme based on an independent bond approximation oleh M. C. Krol, T. Röckmann, G. Pieterse

    Diterbitkan 2009-11-01
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  5. 5
    Role of oceanic ozone deposition in explaining temporal variability in surface ozone at High Arctic sites

    Role of oceanic ozone deposition in explaining temporal variability in surface ozone at High Arctic sites oleh J. G. M. Barten, L. N. Ganzeveld, G.-J. Steeneveld, M. C. Krol, M. C. Krol

    Diterbitkan 2021-07-01
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  6. 6
    Optimizing the carbonic anhydrase temperature response and stomatal conductance of carbonyl sulfide leaf uptake in the Simple Biosphere model (SiB4)

    Optimizing the carbonic anhydrase temperature response and stomatal conductance of carbonyl sulfide leaf uptake in the Simple Biosphere model (SiB4) oleh A. Cho, L. M. J. Kooijmans, K.-M. Kohonen, R. Wehr, M. C. Krol, M. C. Krol

    Diterbitkan 2023-07-01
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  7. 7
    European NO<sub><i>x</i></sub> emissions in WRF-Chem derived from OMI: impacts on summertime surface ozone

    European NO<sub><i>x</i></sub> emissions in WRF-Chem derived from OMI: impacts on summertime surface ozone oleh A. J. Visser, K. F. Boersma, K. F. Boersma, L. N. Ganzeveld, M. C. Krol, M. C. Krol

    Diterbitkan 2019-09-01
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  8. 8
    Evaluation of nitrogen oxides (NO<sub><i>x</i></sub>) sources and sinks and ozone production in Colombia and surrounding areas

    Evaluation of nitrogen oxides (NO<sub><i>x</i></sub>) sources and sinks and ozone production in Colombia and surrounding areas oleh J. G. M. Barten, L. N. Ganzeveld, A. J. Visser, R. Jiménez, M. C. Krol, M. C. Krol

    Diterbitkan 2020-08-01
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  9. 9
    Four-dimensional variational data assimilation for inverse modelling of atmospheric methane emissions: method and comparison with synthesis inversion

    Four-dimensional variational data assimilation for inverse modelling of atmospheric methane emissions: method and comparison with synthesis inversion oleh J. F. Meirink, P. Bergamaschi, M. C. Krol

    Diterbitkan 2008-11-01
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  10. 10
    Combined assimilation of NOAA surface and MIPAS satellite observations to constrain the global budget of carbonyl sulfide

    Combined assimilation of NOAA surface and MIPAS satellite observations to constrain the global budget of carbonyl sulfide oleh J. Ma, L. M. J. Kooijmans, N. Glatthor, S. A. Montzka, M. von Hobe, T. Röckmann, M. C. Krol, M. C. Krol

    Diterbitkan 2024-05-01
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  11. 11
    What chemical species are responsible for new particle formation and growth in the Netherlands? A hybrid positive matrix factorization (PMF) analysis using aerosol composition (ACSM) and size (SMPS)

    What chemical species are responsible for new particle formation and growth in the Netherlands? A hybrid positive matrix factorization (PMF) analysis using aerosol composition (ACS... oleh F. R. Nursanto, R. Meinen, R. Holzinger, M. C. Krol, M. C. Krol, X. Liu, U. Dusek, B. Henzing, J. L. Fry

    Diterbitkan 2023-09-01
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  12. 12
    On the role of hydroxyl radicals in the self-cleansing capacity of the troposphere

    On the role of hydroxyl radicals in the self-cleansing capacity of the troposphere oleh J. Lelieveld, F. J. Dentener, W. Peters, M. C. Krol

    Diterbitkan 2004-01-01
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  13. 13
    Ozone deposition impact assessments for forest canopies require accurate ozone flux partitioning on diurnal timescales

    Ozone deposition impact assessments for forest canopies require accurate ozone flux partitioning on diurnal timescales oleh A. J. Visser, L. N. Ganzeveld, I. Goded, M. C. Krol, M. C. Krol, I. Mammarella, G. Manca, K. F. Boersma, K. F. Boersma

    Diterbitkan 2021-12-01
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  14. 14
    Estimation of OH in urban plumes using TROPOMI-inferred NO<sub>2</sub>&thinsp;∕&thinsp;CO

    Estimation of OH in urban plumes using TROPOMI-inferred NO<sub>2</sub>&thinsp;∕&thinsp;CO oleh S. Lama, S. Houweling, S. Houweling, K. F. Boersma, K. F. Boersma, I. Aben, I. Aben, H. A. C. Denier van der Gon, M. C. Krol, M. C. Krol

    Diterbitkan 2022-12-01
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  15. 15
    Inverse modelling of carbonyl sulfide: implementation, evaluation and implications for the global budget

    Inverse modelling of carbonyl sulfide: implementation, evaluation and implications for the global budget oleh J. Ma, L. M. J. Kooijmans, A. Cho, S. A. Montzka, N. Glatthor, J. R. Worden, L. Kuai, E. L. Atlas, M. C. Krol, M. C. Krol

    Diterbitkan 2021-03-01
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  16. 16
    Emission ratio and isotopic signatures of molecular hydrogen emissions from tropical biomass burning

    Emission ratio and isotopic signatures of molecular hydrogen emissions from tropical biomass burning oleh F. A. Haumann, A. M. Batenburg, G. Pieterse, C. Gerbig, M. C. Krol, T. Röckmann

    Diterbitkan 2013-09-01
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  17. 17
    Quantifying burning efficiency in megacities using the NO<sub>2</sub>∕CO ratio from the Tropospheric Monitoring Instrument (TROPOMI)

    Quantifying burning efficiency in megacities using the NO<sub>2</sub>∕CO ratio from the Tropospheric Monitoring Instrument (TROPOMI) oleh S. Lama, S. Houweling, S. Houweling, K. F. Boersma, K. F. Boersma, H. Eskes, I. Aben, I. Aben, H. A. C. Denier van der Gon, M. C. Krol, M. C. Krol, H. Dolman, T. Borsdorff, A. Lorente

    Diterbitkan 2020-09-01
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  18. 18
    What can <sup>14</sup>CO measurements tell us about OH?

    What can <sup>14</sup>CO measurements tell us about OH? oleh P. Jöckel, S. Houweling, D. Lowe, J. E. Mak, P. Bergamaschi, J. F. Meirink, M. C. Krol, T. Röckmann

    Diterbitkan 2008-08-01
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  19. 19
    A conceptual framework to quantify the influence of convective boundary layer development on carbon dioxide mixing ratios

    A conceptual framework to quantify the influence of convective boundary layer development on carbon dioxide mixing ratios oleh D. Pino, J. Vilà-Guerau de Arellano, W. Peters, J. Schröter, C. C. van Heerwaarden, M. C. Krol

    Diterbitkan 2012-03-01
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  20. 20
    Global modelling of H<sub>2</sub> mixing ratios and isotopic compositions with the TM5 model

    Global modelling of H<sub>2</sub> mixing ratios and isotopic compositions with the TM5 model oleh R. L. Langenfelds, P. B. Krummel, L. P. Steele, A. M. Batenburg, M. C. Krol, G. Pieterse, T. Röckmann

    Diterbitkan 2011-07-01
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