My earlier research has concerned, among others things, the use and the reliability of LES, the application of nonlinear time series analysis on flow fields, and the inclusion of marine organic
aerosol sources in global climate models.
Not exact matches
China «could cause some decreases [
in stratospheric
aerosols] if that is the
source,» Neely says, adding that growing SO2 emissions from India could also increase cooling if humans are the dominant cause of injecting
aerosols into the atmosphere.
These
aerosols outweigh all other human
sources of fine - particulate air pollution
in much of the United States, Europe, Russia and China, according to new research.
«Current emission inventories do not account for cultural burning practices
in Asia as
aerosol sources,» said Chakrabarty, who is originally from the Northeastern region of India.
When Rajan Chakrabarty, Ph.D., an assistant research professor at the Desert Research Institute, began looking into the regional inventories of human - produced
sources of carbon
aerosol pollution
in South Asia, considered to be a climate change hot spot, he knew something was missing.
There had been no «blowtorch effect»
in which the flame erupted outward when the
aerosol vapor was applied close to a fire
source.
Forest fires
in the lower latitudes, however, are actually beneficial
sources of black carbon because it is coupled with organic
aerosols and ends up reflecting light and heat, causing the surrounding area to cool.
Two important
aerosol species, sulfate and organic particles, have large natural biogenic
sources that depend
in a highly complex fashion on environmental and ecological parameters and therefore are prone to influence by global change.
In one of the first studies of its kind, scientists have found that tar sands production in Canada is one of North America's largest sources of secondary organic aerosols — air pollutants that affect the climate, cloud formation and public healt
In one of the first studies of its kind, scientists have found that tar sands production
in Canada is one of North America's largest sources of secondary organic aerosols — air pollutants that affect the climate, cloud formation and public healt
in Canada is one of North America's largest
sources of secondary organic
aerosols — air pollutants that affect the climate, cloud formation and public health.
The study, published Wednesday
in the journal Nature, showed that the production of tar sands and other heavy oil — thick, highly viscous crude oil that is difficult to produce — are a major
source of
aerosols, a component of fine particle air pollution, which can affect regional weather patterns and increase the risk of lung and heart disease.
Since Thornton's and his colleagues» study was published, Ilan Koren and Orit Altaratz at the Weizmann Institute of Science
in Israel and colleagues have found, using the WWLLN, that more intense lightning is connected with
aerosol sources over land.
The cooling effect of
aerosols can partly offset global warming on a short - term basis, but many are made of organic material that comes from
sources that scientists don't fully understand, said Joost de Gouw, a research physicist at NOAA's Earth System Research Laboratory
in Boulder, Colo., who is unaffiliated with the studies.
«Microorganisms are
in a constant fight for territory, for food
sources, for their place
in that microbial community,» says Karen Bartlett of the University of British Columbia, an expert
in the behavior of biological
aerosols.
Aerosols are solid or liquid particles suspended
in the atmosphere, consisting of (
in rough order of abundance): sea salt, mineral dust, inorganic salts such as ammonium sulfate (which has natural as well as anthropogenic
sources from e.g. coal burning), and carbonaceous
aerosol such as soot, plant emissions, and incompletely combusted fossil fuel.
To deal with that, most sucessful scientists develop networks of «trusted»
sources — people you know and get along with, but who are specialists
in different areas (dynamics, radiation, land surfaces,
aerosols, deep time paleo etc.) and who you can just call up and ask for the bottom line.
In particular she works with natural and anthropogenic greenhouse gases and
aerosols and their
sources, concentrations and long term trends.
Wang, M. Gao, Q. Zhang, K. He, G. Carmichael, U. Pöschl and H. Su: Reactive nitrogen chemistry
in aerosol water as a
source of sulfate during haze events
in China, Science Advances 2 (12), e1601530, doi: 10.1126 / sciadv.1601530, 2016.
The complexity of various physical and chemical processes
in the atmosphere makes it very difficult to identify
sources of these carbon - containing
aerosols.
Aerosols are one of the greatest
sources of uncertainty
in climate science.
Because much of Earth's land mass is covered by plants, there is a large
source of these biogenic
aerosol particles that need to be accounted for
in climate change prediction.
Scientists employed methods developed
in this study to tag each
source of
aerosol, such as fossil - fuel burning from vehicles and power plants, or biomass burning, and follow its path
in the model.
The PNNL study measured how,
in the atmosphere, these
aerosols interact with and mix with other volatile or semi-volatile organic compounds, the carbon - centric chemicals that evaporate from both natural and human - made
sources.
The Intergovernmental Panel on Climate Change (IPCC) considers that the increase
in aerosols and clouds since pre-industrial times represents one of the largest
sources of uncertainty
in climate change5.
These layers are caused by seasonal changes
in the
source, transport, and deposition of
aerosols.
In fact, a subsequent study conducted by Liu et al. (2015) and published in Nature Communications, contrasts the CARES measurements with those obtained from the 2012 Clean Air for London (ClearfLo) campaign to show that aerosol coatings influence black carbon absorption and the form and structural details of the mixing state may be specific to the source and region where the mixing occur
In fact, a subsequent study conducted by Liu et al. (2015) and published
in Nature Communications, contrasts the CARES measurements with those obtained from the 2012 Clean Air for London (ClearfLo) campaign to show that aerosol coatings influence black carbon absorption and the form and structural details of the mixing state may be specific to the source and region where the mixing occur
in Nature Communications, contrasts the CARES measurements with those obtained from the 2012 Clean Air for London (ClearfLo) campaign to show that
aerosol coatings influence black carbon absorption and the form and structural details of the mixing state may be specific to the
source and region where the mixing occurs.
Valuable reference
source for students, researchers, college and university professors, and specialists working
in the fields of nanoparticle technology, surface science, chemistry, nanotechnology, solid - state physics, materials science, polymer science, colloid science,
aerosol technology, environmental science, pharmacy, biotechnology, etc..
Secondary organic
aerosols are formed through complex physical and chemical interactions between pre-existing
aerosols in the atmosphere and trace organic gases emitted from both human - caused and natural
sources.
Researchers from the University of Miami (UM) Rosenstiel School of Marine and Atmospheric Science and colleagues analyzed the dust concentrations
in aerosol samples from two locations, French Guiana's capital city Cayenne and the Caribbean islands of Guadeloupe, to understand the amount,
source regions, and seasonal patterns of airborne dust that travels across the North Atlantic Ocean.
Expectations of decreases
in large
source regions such as China [195] may be counteracted by
aerosol increases other places as global population continues to increase.
In general, the risk of
aerosol transmission increases with proximity and duration of exposure to the
source; however, once aerosolized, certain pathogens may remain infective over long distances, depending on particle size, the nature of the pathogen, and such environmental factors as temperature and humidity.3
Perhaps surprisingly, the key innovation
in this experimental set up is not the presence of the controllable ionisation
source (from the Proton Synchrotron accelerator), but rather the state - of - the - art instrumentation of the chamber that has allowed them to see
in unprecedented detail what is going on
in the
aerosol nucleation process (this is according to a couple of
aerosol people I've spoken about this with).
Maybe one could add instead: «This downward radiation from greenhouse gases (and some fine solid air particles («
aerosols») e.g. can be measured at the surface
in nights with clear sky and no other radiation
sources in the atmosphere (e.g. Philipona and Dürr 2004 doi / 10.1029 / 2004GL020937).
If you «use all of the data» you can't detect any change
in trend from forcings known to make a difference (e.g. sulfate
aerosols, which peaked
in the 1940 - 1970 range from US
sources and again later from Chinese).
Thus the influence of
aerosols must be visible mainly
in the NH and specifically
in regions downwind the
sources where the largest change
in emissions has happened.
My question is: does the retroreflectivity of the larger droplets, i.e. back towards the light
source, play into the sulfur
aerosol issue or is it simply averaged out by the bulk effect of all the
aerosol particles present
in the apparently white haze?
They will have a serious impact and will delay advances
in understanding carbon dioxide
sources and sinks (OCO), natural and man - made
aerosols (Glory), and solar climate forcing (Glory).
Possible candidates are an as - yet - unquantified increase
in aerosol forcings from Asian
sources.
It predicts an annual global mean first indirect forcing of -1.5 W m - 2 from an anthropogenic sulfate burden of 0.59 Tg S. Most of the cooling occurs
in norhtern hemisphere (NH), where most anthropogenic
sources of
aerosol are located.
«Impact of interannual variations
in sources of insoluble
aerosol species on orographic precipitation over California's central Sierra Nevada.»
In reality, there are a host of both natural and anthropogenic
aerosols, ranging from sea salt (the major
source of cloud nuclei over the ocean) to biogenic
aerosols from forests (the «smoke» of the Great Smoky Mountains of the Eastern US) to partially burnt organic materials (the «brown cloud» over Asia, generally absorptive / warming) to various sulfur compounds (generally reflective / cooling).
There are other factors involved
in cooling, of course (e.g., recent La Nina's), but
aerosols are probably the most significant
source of uncertainty on timescales longer than a few years..
On the contrary,
in the face of new evidence (of an unexpected
source of
aerosols) they are revising their understanding of the climate.
In particular she works with natural and anthropogenic greenhouse gases and
aerosols and their
sources, concentrations and long term trends.
I also placed
in one manmade
aerosol source on October 1943 to indicate the start of the massive bombing campaign during WWII.
DMS is the primary
source in the sulfate mass budget over the remote ocean west of 80 ° W. • The first
aerosol indirect effect has been observationally quantified over the SEP, with cloud thinning of the more polluted coastal clouds mitigating the overall radiative impact.
On a 20 ° S transect
aerosols from different
sources have a role
in the creation and maintenance of bistable open and closed cell clouds.
It is well known that the ERFaero, the sum of direct
aerosol forcing (ERFari) and ERFaci is by far the greatest
source of uncertainty when it comes to observationally based estimates about the transient sensitivity (TCR) and the expected warming
in this century.
Yet, over rapidly developing countries such as China and India, significant increasing trends
in AOD are seen
in these
source regions and their surrounding downwind oceans, particularly during the dry winter / postmonsoon months when the atmosphere is relatively stable, thus favoring accumulation of
aerosols.
Warming
in the tropics and the southern hemisphere has been quite steady, even though there are plenty of
aerosols there (although they are different, the major
sources in the SH being sea spray and
in the tropics sand from the Sahara as well as agricultural burning
in Brazil and Africa.
The main
source of skill
in temperature is the trend, which is primarily forced by greenhouse gases and
aerosols.