Effect of hygroscopic growth on the aerosol light-scattering coefficient: A review of measurements, techniques and error sources
Abstract Knowledge of the scattering enhancement factor, f (RH), is important for an accurate
description of direct aerosol radiative forcing. This factor is defined as the ratio between the …
description of direct aerosol radiative forcing. This factor is defined as the ratio between the …
Stratospheric aerosols: Observation and theory
RP Turco, RC Whitten, OB Toon - Reviews of Geophysics, 1982 - Wiley Online Library
We review current observational and theoretical knowledge of the stratospheric aerosols.
These particles, which are composed primarily of sulfuric acid and other sulfates, are …
These particles, which are composed primarily of sulfuric acid and other sulfates, are …
The Meteorological Research Institute Earth System Model version 2.0, MRI-ESM2. 0: Description and basic evaluation of the physical component
Abstract The new Meteorological Research Institute Earth System Model version 2.0 (MRI-
ESM2. 0) has been developed based on previous models, MRI-CGCM3 and MRI-ESM1 …
ESM2. 0) has been developed based on previous models, MRI-CGCM3 and MRI-ESM1 …
Description and evaluation of the Model for Ozone and Related chemical Tracers, version 4 (MOZART-4)
The Model for Ozone and Related chemical Tracers, version 4 (MOZART-4) is an offline
global chemical transport model particularly suited for studies of the troposphere. The …
global chemical transport model particularly suited for studies of the troposphere. The …
Complex refractive indices and single-scattering albedo of global dust aerosols in the shortwave spectrum and relationship to size and iron content
C Di Biagio, P Formenti, Y Balkanski… - Atmospheric …, 2019 - acp.copernicus.org
The optical properties of airborne mineral dust depend on its mineralogy, size distribution,
and shape, and they might vary between different source regions. To date, large differences …
and shape, and they might vary between different source regions. To date, large differences …
[HTML][HTML] A model for the spectral albedo of snow. II: Snow containing atmospheric aerosols
SG Warren, WJ Wiscombe - Journal of the Atmospheric …, 1980 - journals.ametsoc.org
Small highly absorbing particles, present in concentrations of only 1 part per million by
weight (ppmw) or less, can lower snow albedo in the visible by 5–15% from the high values …
weight (ppmw) or less, can lower snow albedo in the visible by 5–15% from the high values …
Aerosol forcing in the Climate Model Intercomparison Project (CMIP5) simulations by HadGEM2‐ES and the role of ammonium nitrate
N Bellouin, J Rae, A Jones, C Johnson… - Journal of …, 2011 - Wiley Online Library
The latest Hadley Centre climate model, HadGEM2‐ES, includes Earth system components
such as interactive chemistry and eight species of tropospheric aerosols. It has been run for …
such as interactive chemistry and eight species of tropospheric aerosols. It has been run for …
The relative roles of sulfate aerosols and greenhouse gases in climate forcing
JT Kiehl, BP Briegleb - Science, 1993 - science.org
Calculations of the effects of both natural and anthropogenic tropospheric sulfate aerosols
indicate that the aerosol climate forcing is sufficiently large in a number of regions of the …
indicate that the aerosol climate forcing is sufficiently large in a number of regions of the …
Global distribution and climate forcing of carbonaceous aerosols
SH Chung, JH Seinfeld - Journal of Geophysical Research …, 2002 - Wiley Online Library
The global distribution of carbonaceous aerosols is simulated online in the Goddard Institute
for Space Studies General Circulation Model II‐prime (GISS GCM II‐prime). Prognostic …
for Space Studies General Circulation Model II‐prime (GISS GCM II‐prime). Prognostic …
Effects of mixing on extinction by carbonaceous particles
Reported values for the absorption cross section of particulate carbon per unit mass range
from under 4 to over 20 m2/g, and the intermediate value of 10 m2/g is used by many as a …
from under 4 to over 20 m2/g, and the intermediate value of 10 m2/g is used by many as a …