There have been some regional
aerosol clouds due to mankind's activity.
Not exact matches
Although records are sparse, pan evaporation is estimated to have decreased in many places
due to decreases in surface radiation associated with increases in
clouds, changes in
cloud properties and / or increases in air pollution (
aerosols), especially from 1970 to 1990.
Much of this uncertainty is
due to the complexity of
aerosols and their interactions with and impacts on
cloud processes and properties, as well as the wide range of scales on which these interactions occur.
Roughly two - thirds of this reflectivity is
due to
clouds and small particles in the atmosphere called
aerosols.
Much of the uncertainty in projections of global climate change is
due to the complexity of
clouds,
aerosols, and
cloud -
aerosol interactions, and the difficulty of incorporating this information into climate models.
Possible reasons include increased oceanic circulation leading to increased subduction of heat into the ocean, higher than normal levels of stratospheric
aerosols due to volcanoes during the past decade, incorrect ozone levels used as input to the models, lower than expected solar output during the last few years, or poorly modeled
cloud feedback effects.
What it shows is the effect of the structural uncertainty in individual GCMs (meaning that some of them are systematically high, others systematically low,
due to flaws in the representation of the physics; most probably related to discretization / parametrization effects for
clouds and / or
aerosols).
However, there is a price of sorts — while locally the Asian Brown
Cloud amplifies the greenhouse effect, globally it masks the greenhouse effect
due to the
aerosol - induced global dimming.
The details of the physics of different forcings (i.e. ozone effects
due to solar, snow albedo and
cloud effects
due to
aerosols etc.) do vary the feedbacks slightly differently though.
Natural
clouds eventually drifted into view under the manmade over-story but they did not have the usual majestic appearance as they were «melted» into engineered
clouds above
due to the
aerosol saturation.
Progress with respect to modelling the indirect effects
due to
aerosol -
cloud interactions is detailed in Section 2.4.5 and Section 7.5.
The brownish color of the
cloud (which is visible when looking at the horizon) is
due to absorption of solar radiation at short wavelengths (green, blue, and UV) by organic and black carbon
aerosols as well as by NOx.
An increased greenhouse effect
due to humidity, CO2,
aerosols or
clouds is expected to produce a relative increase of the minima with respect to the maxima and a decrease of the diurnal range.
[~ 17 model years](Motivation: Variation in the climate response across models will be a function of (a) different climate sensitivity in the GCMs, (b) different impact of
aerosols on climate (
due to location with respect to
clouds, water uptake, natural
aerosols, mixing, etc), and (c) different 3D constituent fields from the composition models.
In understanding that there is a difference between climate in a bottle [add CO2] and climate in a complex world with negative feedbacks
due to
aerosols and
cloud albedo.
Taylor, J.P., and A.S. Ackerman, 1999: A case - study of pronounced perturbations to
cloud properties and boundary - layer dynamics
due to
aerosol emissions.
You could also ask Andrew Revkin to withdraw his still - standing claim that most of the
aerosols in atmospheric brown
clouds are
due to biomass burning.