Radiative sensitivities for cloud structural properties that are unresolved by conventional GCMs
暂无分享,去创建一个
[1] E. Clothiaux,et al. Assessing 1D atmospheric solar radiative transfer models: Interpretation and handling of unresolved clouds , 2003 .
[2] Akio Arakawa,et al. CLOUDS AND CLIMATE: A PROBLEM THAT REFUSES TO DIE. Clouds of many , 2022 .
[3] Jiangnan Li,et al. Accounting for Unresolved Clouds in a 1D Infrared Radiative Transfer Model. Part II: Horizontal Variability of Cloud Water Path , 2002 .
[4] T. Charlock. Cloud optical feedback and climate stability in a radiative-convective model , 1982 .
[5] Q. Fu. An Accurate Parameterization of the Infrared Radiative Properties of Cirrus Clouds for Climate Models , 1996 .
[6] D. W. Johnson,et al. The Measurement and Parameterization of Effective Radius of Droplets in Warm Stratocumulus Clouds , 1994 .
[7] Robin J. Hogan,et al. Deriving cloud overlap statistics from radar , 2000 .
[8] K. Bower,et al. A parameterisation of the effective radius of ice free clouds for use in global climate models , 1992 .
[9] Anthony B. Davis,et al. Scale Invariance in Liquid Water Distributions in Marine Stratocumulus. Part II: Multifractal Properties and Intermittency Issues , 1997 .
[10] Stephen H. Schneider,et al. Cloudiness as a Global Climatic Feedback Mechanism: The Effects on the Radiation Balance and Surface Temperature of Variations in Cloudiness , 1972 .
[11] J. Morcrette,et al. A fast, flexible, approximate technique for computing radiative transfer in inhomogeneous cloud fields , 2003 .
[12] H. Barker,et al. A Parameterization for Computing Grid-Averaged Solar Fluxes for Inhomogeneous Marine Boundary Layer Clouds. Part II: Validation Using Satellite Data , 1996 .
[13] Robert F. Cahalan,et al. The albedo of fractal stratocumulus clouds , 1994 .
[14] S. Klein,et al. Unresolved spatial variability and microphysical process rates in large‐scale models , 2000 .
[15] R. Hogan,et al. Parameterizing Ice Cloud Inhomogeneity and the Overlap of Inhomogeneities Using Cloud Radar Data , 2003 .
[16] A. Lacis,et al. A description of the correlated k distribution method for modeling nongray gaseous absorption, thermal emission, and multiple scattering in vertically inhomogeneous atmospheres , 1991 .
[17] A. Tompkins,et al. Effect of Spatial Organization on Solar Radiative Transfer in Three-Dimensional Idealized Stratocumulus Cloud Fields , 2003 .
[18] E. O'connor,et al. The CloudSat mission and the A-train: a new dimension of space-based observations of clouds and precipitation , 2002 .
[19] Qiang Fu,et al. The sensitivity of domain‐averaged solar fluxes to assumptions about cloud geometry , 1999 .
[20] R. M. Welch,et al. Stratocumulus Cloud Field Reflected Fluxes: The Effect of Cloud Shape , 1984 .
[21] Gerald G. Mace,et al. Cloud-Layer Overlap Characteristics Derived from Long-Term Cloud Radar Data , 2002 .
[22] G. Stephens. Radiative Transfer through Arbitrarily Shaped Optical Media. Part II. Group Theory and Simple Closures , 1988 .
[23] E. Clothiaux,et al. Global consequences of interactions between clouds and radiation at scales unresolved by global climate models , 2005 .
[24] H. Barker,et al. Neglect by GCMs of subgrid‐scale horizontal variations in cloud‐droplet effective radius: A diagnostic radiative analysis , 2004 .
[25] Sally A. McFarlane,et al. Albedo bias and the horizontal variability of clouds in subtropical marine boundary layers: Observations from ships and satellites , 1999 .
[26] Philip J. Rasch,et al. Parameterizing Vertically Coherent Cloud Distributions , 2002 .
[27] H. Barker. Estimating Cloud Field Albedo Using One-Dimensional Series Of Optical Depth , 1996 .
[28] D. Randall,et al. Stochastic generation of subgrid‐scale cloudy columns for large‐scale models , 2004 .
[29] Leon D. Rotstayn,et al. Indirect forcing by anthropogenic aerosols: A global climate model calculation of the effective‐radius and cloud‐lifetime effects , 1999 .
[30] Lazaros Oreopoulos,et al. Overlap properties of clouds generated by a cloud‐resolving model , 2003 .
[31] Eugene E. Clothiaux,et al. Atmospheric radiative transfer through global arrays of 2D clouds , 2005 .
[32] H. Barker,et al. Accounting for subgrid‐scale cloud variability in a multi‐layer 1d solar radiative transfer algorithm , 1999 .
[33] Roger Davies,et al. Plane Parallel Albedo Biases from Satellite Observations. Part I: Dependence on Resolution and Other Factors , 1998 .
[34] S. Bony,et al. On dynamic and thermodynamic components of cloud changes , 2004 .
[35] Graham Feingold,et al. The Retrieval of Stratus Cloud Droplet Effective Radius with Cloud Radars , 2002 .
[36] Solar radiative transfer for stratiform clouds with horizontal variations in liquid‐water path and droplet effective radius , 2003 .
[37] S. Matrosov,et al. Profiling cloud ice mass and particle characteristic size from Doppler radar measurements , 2002 .
[38] Jiangnan Li,et al. Accounting for Unresolved Clouds in a 1D Infrared Radiative Transfer Model. Part I: Solution for Radiative Transfer, Including Cloud Scattering and Overlap , 2002 .
[39] Filipe Aires,et al. Inferring instantaneous, multivariate and nonlinear sensitivities for the analysis of feedback processes in a dynamical system: Lorenz model case‐study , 2003 .
[40] D. Randall,et al. A cloud resolving model as a cloud parameterization in the NCAR Community Climate System Model: Preliminary results , 2001 .
[41] Howard W. Barker,et al. Solar Radiative Transfer Through Clouds Possessing Isotropic Variable Extinction Coefficient , 1992 .
[42] G. Paltridge. Cloud‐radiation feedback to climate , 1980 .