Studying the atmospheric aerosol particles, which impact cloud formation and particles, above a pristine forests, researchers discovered that when left alone the Amazon acts as its own «bioreactor»: clouds and precipitation are produced by the abundance of plant materials.
Not exact matches
«This is a cutting - edge
study in the field of cloud -
aerosol - precipitation interactions that includes an interdisciplinary group of
atmospheric chemists and meteorologists,» he said.
Mission leaders were relieved and eager to begin their
studies of cloud and haze effects, which «constitute the largest uncertainties in our models of future climate — that's no exaggeration,» says Jens Redemann, an
atmospheric scientist at NASA's Ames Research Center in Mountain View, California, and the principal investigator for ObseRvations of
Aerosols above CLouds and their IntEractionS (ORACLES).
Studying clouds and
aerosols won't just help scientists
study the climate, it's also a chance to investigate air quality and how
atmospheric particles affect daily life.
That's the conclusion of a team of scientists using a new approach to
study tiny
atmospheric particles called
aerosols that can influence climate by absorbing or reflecting sunlight and seeding clouds.
This mission is fulfilled by operating
atmospheric observatories around the world that collect massive amounts of
atmospheric measurements to provide data products that help scientists
study the effects and interactions of clouds and
aerosols and their impact on the earth's energy balance.
The NASA Plankton,
Aerosol, Cloud, Ocean Ecosystem (PACE) mission, with a target launch within the next 5 years, aims to make measurements that will advance ocean and
atmospheric science and facilitate interdisciplinary
studies involving the interaction of the atmosphere with ocean biological systems.
A team of scientists led by Pacific Northwest National Laboratory
atmospheric researcher Dr. Susannah Burrows and collaborator Daniel McCoy, who
studies clouds and climate at the University of Washington, reveal how tiny natural particles given off by marine organisms — airborne droplets and solid particles called
aerosols — nearly double cloud droplet numbers in the summer, which boosts the amount of sunlight reflected back to space.
The CLOUD experiment consists of a large instrumented chamber in which the atmosphere can be precisely simulated, and the formation and growth of
aerosol particles and the clouds they seed can be
studied under precisely controled
atmospheric conditions.
This method tries to maximize using pure observations to find the temperature change and the forcing (you might need a model to constrain some of the forcings, but there's a lot of uncertainty about how the surface and
atmospheric albedo changed during glacial times... a lot of
studies only look at dust and not other
aerosols, there is a lot of uncertainty about vegetation change, etc).
There were lots of
studies of
atmospheric transmission (and hence
aerosol optical depth) starting with the work of Marvin and later Hand of the National Weather Service.
Can you point me to a
study which examines paleoclimatic temperature, CO2 and
atmospheric aerosols and reconciles them with present day temperature, CO2 and
atmospheric aerosols?
«Climate models consider anthropogenic forcings like greenhouse gases and tiny
atmospheric particles known as
aerosols, but they can not
study a specific climate event like the current hiatus,» said Yu Kosaka, co-author of the Nature paper.
This capability is also important for
atmospheric chemistry and
aerosol studies where the emission sources are localized and non-uniformly distributed.
28 29 7.4.5.2 Physical Mechanisms Linking Cosmic Rays to Cloudiness 30 31 The most widely
studied mechanism proposed to explain the possible link between GCR and cloudiness is 32 the «ion -
aerosol clear air» mechanism, in which
atmospheric ions produced by GCR facilitate
aerosol 33 nucleation and growth ultimately impacting CCN concentrations and cloud properties (Carslaw et al., 2002; 34 Usoskin and Kovaltsov, 2008).
The most widely
studied mechanism proposed to explain the possible link between GCR and cloudiness is the «ion -
aerosol clear air» mechanism, in which
atmospheric ions produced by GCR facilitate
aerosol nucleation and growth ultimately impacting CCN concentrations and cloud properties (Carslaw et al., 2002; http://www.sciencemag.org/content/298/5599/1732.abstract
Surely after decades of satellite measurements, countless field experiments, and numerous finescale modeling
studies that have repeatedly highlighted basic deficiencies in the ability of comprehensive climate models to represent processes contributing to
atmospheric aerosol forcing, it is time to give up on the fantasy that somehow their output can be accepted at face value.»
However, this
study focused on the warming effects of black carbon, and did not compare them to the cooling effects of
atmospheric aerosols.
The
study, published in Nature Geoscience found that humans have caused at least three - quarters (74 percent) of current warming, while also determining that warming has actually been slowed down by
atmospheric aerosols, including some pollutants, which reflect sunlight back into space.
Microphysical theories regarding CR - cloud links via ion - mediated nucleation are well developed, and several
studies have attempted to incorporate these effects within
atmospheric models to estimate the magnitude of potential affects to
aerosols and clouds.
Yet observational and modeling
studies have shown that these
aerosols have led to large regional changes in surface and
atmospheric temperatures, the surface energy budget, and rainfall (Ramanathan et al., 2001a; Chung et al., 2002; Menon et al., 2002b).
This mission is fulfilled by operating
atmospheric observatories around the world that collect massive amounts of
atmospheric measurements to provide data products that help scientists
study the effects and interactions of clouds and
aerosols and their impact on the earth's energy balance.
In the article «Global
atmospheric particle formation from CERN CLOUD measurements,» sciencemag.org, 49 authors concluded «
Atmospheric aerosol nucleation has been
studied for over 20 years, but the difficulty of performing laboratory nucleation - rate measurements close to
atmospheric conditions means that global model simulations have not been directly based on experimental data.....
I also predict it will be accompanied by
studies showing either: a) The quantity of
atmospheric aerosol from the 40's -70's is much less than previously thought b) The cooling effect of
aerosols is much less significant than previously thought
Sensors on board would have contributed to the
study of clouds, solar radiation, and (most significantly)
atmospheric aerosols.
While multiple
studies have shown the Northern Hemisphere plays a stronger role than the Southern Hemisphere in transient climate change, this had not been included in calculations of the effect of
atmospheric aerosols on climate sensitivity.
The research from top scientists
studying a decade of
atmospheric data has shown how cloud and weather development are affected by
aerosols in the atmosphere.