Review the development of
atmospheric models for use in weather prediction and climate studies on all scales, including the diagnosis of shortcomings.
The observations are best described by
atmospheric models for which most of the incident energy is re-radiated away from the day side.
On March 19, 2008, astronomers using the Hubble Space Telescope announced confirmation of the presence of water and the detection of more methane in the atmosphere of the planet than would be predicted by conventional
atmospheric models for «hot Jupiters» (Hubble news release and videos; ESA news release and videos; and Swain et al, 2008 — more below).
«A lot of
atmospheric models for Mars are very simple,» says Dan Cziczo, the Victor P. Starr Associate Professor of Atmospheric Chemistry at MIT.
He is a member of the Department of Energy's Accelerated Climate Modeling for Energy (ACME) project council and co-lead in developing
an atmospheric model for the project.
In a paper on the Energy & Environmental Science web site (17/7/12), meteorologist John Ten Hoeve and environmental engineer Mark Jacobson, both at Stanford University in California have calculated that, based on estimates of the radioactive nuclides released at Fukuhima, a three - dimensional global
atmospheric model for radioactive fallout patterns and the linear no - threshold (LNT) model for resultant cancers, there would be between 15 and 1100 linked cancer deaths, with their best estimate being 130 deaths.
F - 930 the company Intel, in cooperation with DKRZ, presented an interactive visualization based on a cloud - resolving
atmospheric model for Germany, which was calculated at DKRZ as part of project HD (CP) ².
Not exact matches
Now, to find out how the glaciers formed in the first place, scientists created
models that simulated
atmospheric circulation on the dwarf planet
for the last 50,000 years (a mere 200 orbits around the sun
for Pluto).
To figure out how to look
for actual proof of extrasolar lightning, Helling combined Drift's code with another
atmospheric model called Phoenix, created by astrophysicists at the University of Hamburg.
When Douglas MacMartin of the California Institute of Technology in Pasadena approached the National Science Foundation
for support on a
modeling effort on [albedo modification], officials told him the work was too theoretical
for the engineering division and too applied
for the
atmospheric science program.
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).
To determine whether declining pollutants deserve credit
for the recovery, the researchers used a 3D
atmospheric model to separate the effects of the chemicals from those of weather, which can affect ozone loss through winds and temperature, and volcanic eruptions, which deplete ozone by pumping sulfate particles into the upper atmosphere.
According to Klippenstein, this research improves
models for atmospheric chemistry.
The researchers developed
atmospheric models of the equilibrium chemistry
for a brown dwarf at 250 degrees Kelvin and calculated the resulting spectra under different assumptions, including cloudy and cloud - free
models.
The computer
model, designed by research fellow Iain Couzin, could lead to improved guidance systems
for clusters of robots, such as those used to gather oceanographic and
atmospheric data.
After a painstaking analysis that
modeled all known sources of acceleration
for Juno, including the minute contributions from sunlight warming the spacecraft, Iess's team found a large north - south asymmetry in Jupiter's gravitational field — a clear sign of material flowing beneath the cloud tops on deep
atmospheric winds.
For example, the
model predicts that production of carbon dioxide must increase with time, a finding that goes against the conventional wisdom that carbon fluxes and
atmospheric carbon dioxide levels have steadily decreased over the last 4 billion years.
«In our study we used satellite data
for sea ice and sea surface temperatures to run some coordinated hindcast experiments with five different
atmospheric models,» Ogawa says.
The
model also accounted
for natural drivers of change, including the direct influence of increased carbon dioxide on ocean - carbon uptake and the indirect effect that a changing climate has on the physical state of the ocean and its relationship to
atmospheric carbon dioxide.
Even
models that correctly capture cloud behavior may fail to fully account
for other climate feedbacks from factors like changing snow and sea ice cover,
atmospheric water vapor content, and temperature.
Determining the structure of these molecules, she said, «is paving the way
for future spectroscopic detection and
atmospheric chemistry
modeling.»
The UM Rosenstiel School researchers used historical observations of cloud cover as a proxy
for wind velocity in climate
models to analyze the Walker circulation, the
atmospheric air flow and heat distribution in the tropic Pacific region that affects patterns of tropical rainfall.
For example, in a simulated world where the
atmospheric CO2 levels were double today's values — a scenario many scientists believe likely —
models predict that Earth will warm by more than 2 °C.
Those data, to be collected this year and next, could improve climate
models, which account poorly
for these
atmospheric interactions and contain «horrific» uncertainties about the levels and behaviour of water vapour at stratospheric altitudes, Austin says.
«It would be like trying to predict El Niño with a sophisticated
atmospheric model, but with the Sea Surface Temperatures taken from external, independent projections by,
for example, the United Nations,» said Kalnay.
Both
models help mission team members plan when and where to look
for unusual
atmospheric disturbances as Titan summer approaches.
Air pollutant emission inventories are essential in measuring the impact of pollution on air quality and the climate, as they are fed into
atmospheric and climate
models to make projections
for the future.
For the study, Gentine and Lemordant took Earth system models with decoupled surface (vegetation physiology) and atmospheric (radiative) CO2 responses and used a multi-model statistical analysis from CMIP5, the most current set of coordinated climate model experiments set up as an international cooperation project for the International Panel on Climate Chan
For the study, Gentine and Lemordant took Earth system
models with decoupled surface (vegetation physiology) and
atmospheric (radiative) CO2 responses and used a multi-
model statistical analysis from CMIP5, the most current set of coordinated climate
model experiments set up as an international cooperation project
for the International Panel on Climate Chan
for the International Panel on Climate Change.
They were Jorge Sarmiento, an oceanographer at Princeton University who constructs ocean - circulation
models that calculate how much
atmospheric carbon dioxide eventually goes into the world's oceans; Eileen Claussen, executive director of the Pew Center
for Global Climate Change in Washington, D.C.; and David Keith, a physicist with the University of Calgary in Alberta who designs technological solutions to the global warming problem.
A recent trend in GCMs is to extend them to become Earth system
models, that include such things as submodels
for atmospheric chemistry or a carbon cycle
model to better predict changes in carbon dioxide concentrations resulting from changes in emissions.
With respect to solvers, in 1993, he developed the world's fastest ordinary differential equation solver in a three - dimensional
model for a given level of accuracy and applied it to
atmospheric chemistry.
Regional trends are notoriously problematic
for models, and seems more likely to me that the underprediction of European warming has to do with either the
modeled ocean temperature pattern, the
modelled atmospheric response to this pattern, or some problem related to the local hydrological cycle and boundary layer moisture dynamics.
Model simulations of 20th century global warming typically use actual observed amounts of
atmospheric carbon dioxide, together with other human (
for example chloroflorocarbons or CFCs) and natural (solar brightness variations, volcanic eruptions,...) climate - forcing factors.
As R139 appears to be the most massive binary system known to contain two evolved Of supergiants, it will provide an excellent test
for atmospheric and evolutionary
models.
The finding suggests that
models used to gauge the impact of drought on ecosystems should be refined to more accurately account
for the role of low
atmospheric humidity.
Sally, who was nominated by Dr. Beat Schmid, Associate Director,
Atmospheric Sciences and Global Change Division, was honored
for her exceptional contribution in the field of
atmospheric science, particularly in her efforts to improve understanding of the radiative effect of clouds and aerosols on the Earth's atmosphere and their representation in climate
models.
Results: Researchers at Pacific Northwest National Laboratory — in collaboration with NERSC, Argonne National Laboratory, and Cray — recently achieved an effective aggregate IO bandwidth of 5 Gigabytes / sec
for writing output from a global
atmospheric model to shared files on DOE's «Franklin,» a 39,000 - processor Cray XT4 supercomputer located at NERSC.
The second is the
Model for OZone and Related chemical Tracers, or MOZART, a three - dimensional atmospheric chemical transport m
Model for OZone and Related chemical Tracers, or MOZART, a three - dimensional
atmospheric chemical transport
modelmodel.
In this work, using a simple time - dependent 1D
model, we demonstrate that radiative cloud feedback can drive spontaneous
atmospheric variabilities in both temperature and cloud structures under conditions appropriate
for brown dwarfs and directly imaged EGPs.
NGIMS can provide a basis
for models of present and past
atmospheric loss.
To derive the climate projections
for this assessment, we employed 20 general circulation
models to consider two scenarios of global carbon emissions: one where
atmospheric greenhouse gases are stabilized by the end of the century and the other where it grows on its current path (the stabilization [RCP4.5] and business - as - usual [RCP8.5] emission scenarios, respectively).
For the last five years, he helped to lead the technical development team for the next generation of the atmospheric component of the Community Climate System Model Project, one of the major climate modeling activities in the United Stat
For the last five years, he helped to lead the technical development team
for the next generation of the atmospheric component of the Community Climate System Model Project, one of the major climate modeling activities in the United Stat
for the next generation of the
atmospheric component of the Community Climate System
Model Project, one of the major climate
modeling activities in the United States.
He promoted the use of water stable isotopomers
for reconstructing past climate changes from ice cores and with associated
atmospheric modelling using both dynamically simple and General Circulation
Models (GCMs).
For the hydrological modelling of the Thames river catchment done at CEH we showed that the changes in atmospheric circulation and precipitation caused higher peak 30 - day river flow, while flood risk mapping revealed a small increase in flood risk for properties in the Thames catchme
For the hydrological
modelling of the Thames river catchment done at CEH we showed that the changes in
atmospheric circulation and precipitation caused higher peak 30 - day river flow, while flood risk mapping revealed a small increase in flood risk
for properties in the Thames catchme
for properties in the Thames catchment.
In his career - long support of CESM, Rasch was formerly co-chair of the
Atmospheric Model Working Group and team lead
for the version five development of CESM's
atmospheric component, called the Community Atmosphere
Model (CAM5).
In addition, he praised her leadership with the National Center
for Atmospheric Research in advancing the Weather Research and Forecasting
model for climate research, and in projects such as the North American Regional Climate Change Assessment Program, as demonstration of her prominence in the
atmospheric and climate science community.
This information is vital
for numerical
models, and answers questions about how dynamic ice sheets are, and how responsive they are to changes in
atmospheric and oceanic temperatures.
The real «equilibrium climate sensitivity,» which is the amount of global warming to be expected
for a doubling of
atmospheric CO2, is likely to be about 1 °C, some three times smaller than most
models assumed.
For latitudes above 60 ° N, emissions are estimated to be 18 — 29 Tg CH4 per year on the basis of top - down
atmospheric model approaches.
Therefore, what Hansen's
models and the real - world observations tell us is that climate sensitivity is about 40 % below 4.2 °C, or once again, right around 3 °C
for a doubling of
atmospheric CO2.