Hasil Pencarian - D. G. Partridge

Perbaiki Hasil
  1. 1
    Inverse modelling of Köhler theory – Part 1: A response surface analysis of CCN spectra with respect to surface-active organic species

    Inverse modelling of Köhler theory – Part 1: A response surface analysis of CCN spectra with respect to surface-active organic species oleh S. Lowe, S. Lowe, S. Lowe, D. G. Partridge, D. G. Partridge, D. G. Partridge, D. Topping, D. Topping, P. Stier

    Diterbitkan 2016-09-01
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  2. 2
    The importance of temporal collocation for the evaluation of aerosol models with observations

    The importance of temporal collocation for the evaluation of aerosol models with observations oleh N. A. J. Schutgens, D. G. Partridge, D. G. Partridge, P. Stier

    Diterbitkan 2016-01-01
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  3. 3
    New trajectory-driven aerosol and chemical process model Chemical and Aerosol Lagrangian Model (CALM)

    New trajectory-driven aerosol and chemical process model Chemical and Aerosol Lagrangian Model (CALM) oleh P. Tunved, D. G. Partridge, H. Korhonen

    Diterbitkan 2010-11-01
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  4. 4
    Links between satellite-retrieved aerosol and precipitation

    Links between satellite-retrieved aerosol and precipitation oleh E. Gryspeerdt, P. Stier, D. G. Partridge

    Diterbitkan 2014-09-01
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  5. 5
    Satellite observations of cloud regime development: the role of aerosol processes

    Satellite observations of cloud regime development: the role of aerosol processes oleh E. Gryspeerdt, P. Stier, D. G. Partridge

    Diterbitkan 2014-02-01
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  6. 6
    Cloud condensation nuclei concentrations derived from the CAMS reanalysis

    Cloud condensation nuclei concentrations derived from the CAMS reanalysis oleh K. Block, M. Haghighatnasab, M. Haghighatnasab, D. G. Partridge, P. Stier, J. Quaas

    Diterbitkan 2024-01-01
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  7. 7
    On the characteristics of aerosol indirect effect based on dynamic regimes in global climate models

    On the characteristics of aerosol indirect effect based on dynamic regimes in global climate models oleh S. Zhang, S. Zhang, S. Zhang, M. Wang, M. Wang, M. Wang, S. J. Ghan, A. Ding, A. Ding, H. Wang, K. Zhang, D. Neubauer, U. Lohmann, S. Ferrachat, T. Takeamura, A. Gettelman, H. Morrison, Y. Lee, D. T. Shindell, D. G. Partridge, D. G. Partridge, D. G. Partridge, P. Stier, Z. Kipling, C. Fu, C. Fu

    Diterbitkan 2016-03-01
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  8. 8
    Key drivers of cloud response to surface-active organics

    Key drivers of cloud response to surface-active organics oleh S. J. Lowe, D. G. Partridge, J. F. Davies, K. R. Wilson, D. Topping, I. Riipinen

    Diterbitkan 2019-11-01
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  9. 9
    Inverse modelling of cloud-aerosol interactions – Part 2: Sensitivity tests on liquid phase clouds using a Markov chain Monte Carlo based simulation approach

    Inverse modelling of cloud-aerosol interactions – Part 2: Sensitivity tests on liquid phase clouds using a Markov chain Monte Carlo based simulation approach oleh D. G. Partridge, J. A. Vrugt, P. Tunved, A. M. L. Ekman, H. Struthers, A. Sorooshian

    Diterbitkan 2012-03-01
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  10. 10
    Inverse modeling of cloud-aerosol interactions – Part 1: Detailed response surface analysis

    Inverse modeling of cloud-aerosol interactions – Part 1: Detailed response surface analysis oleh D. G. Partridge, J. A. Vrugt, P. Tunved, A. M. L. Ekman, D. Gorea, A. Sorooshian

    Diterbitkan 2011-07-01
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  11. 11
    Including ash in UKESM1 model simulations of the Raikoke volcanic eruption reveals improved agreement with observations

    Including ash in UKESM1 model simulations of the Raikoke volcanic eruption reveals improved agreement with observations oleh A. F. Wells, A. Jones, M. Osborne, L. Damany-Pearce, D. G. Partridge, J. M. Haywood, J. M. Haywood

    Diterbitkan 2023-04-01
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  12. 12
    The importance of vertical velocity variability for estimates of the indirect aerosol effects

    The importance of vertical velocity variability for estimates of the indirect aerosol effects oleh R. E. L. West, P. Stier, A. Jones, C. E. Johnson, G. W. Mann, N. Bellouin, D. G. Partridge, Z. Kipling

    Diterbitkan 2014-06-01
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  13. 13
    In-plume and out-of-plume analysis of aerosol–cloud interactions derived from the 2014–2015 Holuhraun volcanic eruption

    In-plume and out-of-plume analysis of aerosol–cloud interactions derived from the 2014–2015 Holuhraun volcanic eruption oleh A. H. Peace, A. H. Peace, Y. Chen, G. Jordan, D. G. Partridge, F. Malavelle, E. Duncan, J. M. Haywood, J. M. Haywood

    Diterbitkan 2024-08-01
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  14. 14
    The global aerosol–climate model ECHAM6.3–HAM2.3 – Part 2: Cloud evaluation, aerosol radiative forcing, and climate sensitivity

    The global aerosol–climate model ECHAM6.3–HAM2.3 – Part 2: Cloud evaluation, aerosol radiative forcing, and climate sensitivity oleh D. Neubauer, S. Ferrachat, C. Siegenthaler-Le Drian, P. Stier, D. G. Partridge, I. Tegen, I. Bey, I. Bey, T. Stanelle, H. Kokkola, U. Lohmann

    Diterbitkan 2019-08-01
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  15. 15
    Cloud response to co-condensation of water and organic vapors over the boreal forest

    Cloud response to co-condensation of water and organic vapors over the boreal forest oleh L. Heikkinen, L. Heikkinen, D. G. Partridge, S. Blichner, S. Blichner, W. Huang, R. Ranjan, R. Ranjan, P. Bowen, E. Tovazzi, T. Petäjä, C. Mohr, C. Mohr, I. Riipinen, I. Riipinen

    Diterbitkan 2024-04-01
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  16. 16
    How well are aerosol–cloud interactions represented in climate models? – Part 1: Understanding the sulfate aerosol production from the 2014–15 Holuhraun eruption

    How well are aerosol–cloud interactions represented in climate models? – Part 1: Understanding the sulfate aerosol production from the 2014–15 Holuhraun eruption oleh G. Jordan, F. Malavelle, Y. Chen, A. Peace, E. Duncan, D. G. Partridge, P. Kim, D. Watson-Parris, T. Takemura, D. Neubauer, G. Myhre, R. Skeie, A. Laakso, J. Haywood, J. Haywood

    Diterbitkan 2024-02-01
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  17. 17
    Revising the hygroscopicity of inorganic sea salt particles

    Revising the hygroscopicity of inorganic sea salt particles oleh P. Zieger, O. Väisänen, J. C. Corbin, D. G. Partridge, S. Bastelberger, M. Mousavi-Fard, B. Rosati, M. Gysel, U. K. Krieger, C. Leck, A. Nenes, I. Riipinen, A. Virtanen, M. E. Salter

    Diterbitkan 2017-07-01
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  18. 18
    Surprising similarities in model and observational aerosol radiative forcing estimates

    Surprising similarities in model and observational aerosol radiative forcing estimates oleh E. Gryspeerdt, J. Mülmenstädt, J. Mülmenstädt, A. Gettelman, F. F. Malavelle, F. F. Malavelle, H. Morrison, D. Neubauer, D. G. Partridge, P. Stier, T. Takemura, H. Wang, M. Wang, M. Wang, M. Wang, K. Zhang

    Diterbitkan 2020-01-01
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  19. 19
    Ensembles of Global Climate Model Variants Designed for the Quantification and Constraint of Uncertainty in Aerosols and Their Radiative Forcing

    Ensembles of Global Climate Model Variants Designed for the Quantification and Constraint of Uncertainty in Aerosols and Their Radiative Forcing oleh M. Yoshioka, L. A. Regayre, K. J. Pringle, J. S. Johnson, G. W. Mann, D. G. Partridge, D. M. H. Sexton, G. M. S. Lister, N. Schutgens, P. Stier, Z. Kipling, N. Bellouin, J. Browse, B. B. B. Booth, C. E. Johnson, B. Johnson, J. D. P. Mollard, L. Lee, K. S. Carslaw

    Diterbitkan 2019-11-01
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  20. 20
    General circulation models simulate negative liquid water path–droplet number correlations, but anthropogenic aerosols still increase simulated liquid water path

    General circulation models simulate negative liquid water path–droplet number correlations, but anthropogenic aerosols still increase simulated liquid water path oleh J. Mülmenstädt, E. Gryspeerdt, S. Dipu, J. Quaas, A. S. Ackerman, A. M. Fridlind, F. Tornow, F. Tornow, S. E. Bauer, A. Gettelman, Y. Ming, Y. Zheng, Y. Zheng, P.-L. Ma, H. Wang, K. Zhang, M. W. Christensen, A. C. Varble, L. R. Leung, X. Liu, D. Neubauer, D. G. Partridge, P. Stier, T. Takemura

    Diterbitkan 2024-06-01
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