Topics have included sensitivity analysis, calibration, and optimization for cloud and convection systems as well
as aerosol processes.
Not exact matches
The
process may also play a part in the mixing between atmosphere and oceans,
as smaller bubbles tend to absorb gas faster than big ones and are better at spitting out
aerosol droplets when they pop.
These chemical compounds were once emitted by dry cleaning
processes, old refrigerators, and
aerosols such
as hairspray.
While a large amount of
aerosols that exist in the Earth's atmosphere are naturally occurring — created by
processes such
as mechanical suspension by wind or sea spray — much is produced
as a result of industrialization.
This should be taken with a grain of salt, given that our understanding of the small scale
processes such
as clouds and
aerosols as feedbacks are fairly poor.
PNNL researchers play a key role in reducing uncertainty through improved
process understanding and modeling of climate
processes such
as clouds and
aerosols.
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.
As a package, it evaluates the performance of
aerosol process modules across a wide range of field measurements.
This statement on its own would be an acknowledgement that climate engineering
processes are underway and now we can not turn back
as switching off the
aerosols would be more damaging than any other course of action.
The aci effect (associated with clouds) is either specified in the model
as forcing, or the model allows the
aerosols to interact directly with the cloud microphysical
processes.
I was told by one semi-expert climate scientist (someone who was in the
process of changing fields to climate science from a different numerical modeling field,
as so possibly still catching up) that although globally
aerosols played the most important role in this period, there was also around the same time period (maybe beginning slightly earlier?
nevertheless, both states can coexist for a wide range of environmental conditions.5, 7
Aerosols, liquid or solid particles suspended in the atmosphere, serve
as Cloud Condensation Nuclei (CCN) and therefore affect the concentration of activated cloud droplets.8 Changes in droplet concentration affect key cloud properties such
as the time it takes for the onset of significant collision and coalescence between droplets, a
process critical for rain formation.»
Aerosols, liquid or solid particles suspended in the atmosphere, serve
as Cloud Condensation Nuclei (CCN) and therefore affect the concentration of activated cloud droplets.8 Changes in droplet concentration affect key cloud properties such
as the time it takes for the onset of significant collision and coalescence between droplets, a
process critical for rain formation.»
New evidence shows that the ocean also acts
as a source of organic matter from biogenic origin -LSB-...] Surface - active organic matter of biogenic origin -LSB-...] enriched in the oceanic surface layer and transferred to the atmosphere by bubble - bursting
processes, are the most likely candidates to contribute to the observed organic fraction in marine
aerosol.
temperature, other climatic variables, and concentrations of
aerosols and trace gases; and (2) making raw and
processed atmospheric measurements accessible in a form that enables a number of different groups to replicate and experiment with the
processing of the more widely disseminated data sets such
as the MSU tropospheric temperature record.
The formation of cloud droplets and cloud ice crystals is associated with suspended
aerosols, which are produced by natural
processes as well
as human activities and are ubiquitous in Earth's atmosphere.
«In order to develop climate models, we have to consider microphysical
processes, such
as how a cloud droplet gets formed and how such droplets and physical conditions inside and outside of a cloud are changed by the presence of
aerosols,» she said.
Today she is an inspired investigator of severe storms,
as well
as an ascendant expert in modeling cloud -
aerosol interactions at the
process scale.
However, the precise
processes and feedback mechanisms have not yet been fully understood, so that the interaction between
aerosol particles, their suitability
as cloud condensation nuclei, and the sunlight reflected off the earth's surface represented one of the greatest uncertainties in the calculation of climatic activity.
While it is impossible to know what decisions are made in the development
process of each model, it seems plausible that choices are made based on agreement with observations
as to what parameterizations are used, what forcing datasets are selected, or whether an uncertain forcing (e.g. mineral dust, land use) or feedback (indirect
aerosol effect) is incorporated or not.
... The observed patterns of change over the past 50 years can not be explained by natural
processes alone, nor by the effects of short - lived atmospheric constituents (such
as aerosols and tropospheric ozone) alone.
The NIPCC report exaggerates the uncertainty in climate science, but seems to put a lot of faith in elusive and hardly quantified
processes such
as natural
aerosol feedbacks coming to our rescue.
This should be taken with a grain of salt, given that our understanding of the small scale
processes such
as clouds and
aerosols as feedbacks are fairly poor.
Interactions with the hydrological cycle, and additional impacts on the radiation budget, occur through the role of
aerosols in cloud microphysical
processes,
as aerosol particles act
as cloud condensation nuclei (CCN) and ice nuclei (IN).
Knowledge of the basic physical
processes seems to be in flux
as well: how long ago was the importance of the ozone layer and
aerosols discovered?
But a reminder, you are doing V&V on the dynamic core, the bottom boundary conditions (like orography), each individual parameterization (e.g. radiative transfer, convection, boundary layer, clouds, etc), and in the case of coupled models the ocean module, the sea ice module, the land
process module, the
aerosol module (and in future the ice sheet module), in stand alone mode
as well
as when coupled in the climate model.
For anyone doubting the existence of the phenomenon called «chemtrails», please take the time to read through this extensive list of patents from the U.S. Patent and Trade Mark Office on equipment and
processes used in
aerosol spraying programs commonly referred to
as «chemtrails» but scientifically called «weather geoengineering.»
My studies range from detailed
aerosol processes such
as the formation of secondary organic
aerosols (SOA), to centennial time scale climate variability related to natural variability and external forcings.
Topics that I work on or plan to work in the future include studies of: + missing
aerosol species and sources, such
as the primary oceanic
aerosols and their importance on the remote marine atmosphere, the in - cloud and
aerosol water aqueous formation of organic
aerosols that can lead to brown carbon formation, the primary terrestrial biological particles, and the organic nitrogen + missing
aerosol parameterizations, such
as the effect of
aerosol mixing on cloud condensation nuclei and
aerosol absorption, the semi-volatility of primary organic
aerosols, the importance of in - canopy
processes on natural terrestrial
aerosol and
aerosol precursor sources, and the mineral dust iron solubility and bioavailability + the change of
aerosol burden and its spatiotemporal distribution, especially with regard to its role and importance on gas - phase chemistry via photolysis rates changes and heterogeneous reactions in the atmosphere,
as well
as their effect on key gas - phase species like ozone + the physical and optical properties of
aerosols, which affect
aerosol transport, lifetime, and light scattering and absorption, with the latter being very sensitive to the vertical distribution of absorbing
aerosols +
aerosol - cloud interactions, which include cloud activation, the
aerosol indirect effect and the impact of clouds on
aerosol removal + changes on climate and feedbacks related with all these topics In order to understand the climate system
as a whole, improve the
aerosol representation in the GISS ModelE2 and contribute to future IPCC climate change assessments and CMIP activities, I am also interested in understanding the importance of natural and anthropogenic
aerosol changes in the atmosphere on the terrestrial biosphere, the ocean and climate.
For a comprehensive GCM I can count oceans, land, atmosphere, ice, biological
processes, organic and inorganic chemical
processes, human - made sources and other effects, radiative energy transport, conduction and convective heat transfer, phase change, clouds and
aerosols,
as some of the important system components, phenomena, and
processes.