Not exact matches
The team compiled data from many studies
and for the first time synthesized
observations and numerical model output to develop a cohesive view of the carbon cycle in a large coastal region.
«We gradually increased the physical complexity of
numerical models based on high - resolution
observations,
and it is really a success story for the approach we've taken with IRIS.»
«Our job is to collect as many
observations as we can to send to the National Hurricane Center in Miami,
and to NOAA's
numerical models center in Washington.»
Combining satellite
observations with ocean
numerical modeling, Khazendar
and his colleagues developed a hypothesis that reductions in the volume of brine would increase Totten's thinning
and melting.
The successful applicant will work with world leading experts in advanced analytical /
numerical modelling, analysis of high - resolution
observations obtained by cutting - edge ground
and space based instruments.
Xie, P.,
and P.A. Arkin, 1997: Global precipitation: A 17 - year monthly analysis based on gauge
observations, satellite estimates,
and numerical model outputs.
Potential topics include: (1) Advanced
numerical modelling of magnetic flux tubes / loops in the low solar atmosphere (2) Forward
modelling of spectroscopic
and narrowband EUV
observations of the low solar atmosphere, (3) Solar Rotational Tomography of EUV
and / or coronagraph coronal
observations, (4) Automated detection
and prediction of coronal mass ejections, (5) Analysis of solar wind turbulence
observations by in situ spacecraft, (6) Eclipse instrumentation,
observations and data analysis.
Space research at our institute is conducted within two Research Programmes: planetary research
and numerical modelling in Earth Observation,
and ground - based
observations and space weather applications in Arctic Research.
It is very clear that changes to certain aspects of the mathematical
models,
numerical solution methods,
and application procedures are in fact based on «the match to
observations».
This claim is complemented with a broad literature synthesis of past work in
numerical weather prediction,
observations, dynamical theory,
and modeling in the central U.S. Importantly, the discussion also distills some notoriously confusing aspects of the super-parameterization approach into clear language
and diagrams, which are a constructive contribution to the literature.
Dong, S., M. O. Baringer, G. J. Goni, C. S. Meinen,
and S. L. Garzoli, 2014: Seasonal variations in the South Atlantic Meridional Overturning Circulation from
observations and numerical models.
Most notably, in a global study Wahl et al (2017) considered both extreme value analysis
and numerical models that were used to simulate storm surges at coastline stretches where no
observations exist to quantify ESL
and their uncertainties.
The same
observations and numerical tools that enable new scientific discoveries have the potential to transform
modeling of the climate system.
The meeting will mainly cover the following themes, but can include other topics related to understanding
and modelling the atmosphere: ● Surface drag
and momentum transport: orographic drag, convective momentum transport ● Processes relevant for polar prediction: stable boundary layers, mixed - phase clouds ● Shallow
and deep convection: stochasticity, scale - awareness, organization, grey zone issues ● Clouds
and circulation feedbacks: boundary - layer clouds, CFMIP, cirrus ● Microphysics
and aerosol - cloud interactions: microphysical
observations, parameterization, process studies on aerosol - cloud interactions ● Radiation: circulation coupling; interaction between radiation
and clouds ● Land - atmosphere interactions: Role of land processes (snow, soil moisture, soil temperature,
and vegetation) in sub-seasonal to seasonal (S2S) prediction ● Physics - dynamics coupling:
numerical methods, scale - separation
and grey - zone, thermodynamic consistency ● Next generation
model development: the challenge of exascale, dynamical core developments, regional refinement, super-parametrization ● High Impact
and Extreme Weather: role of convective scale
models; ensembles; relevant challenges for
model development
Descriptive physical oceanography seeks to research the ocean through
observations and complex
numerical models, which describe the fluid motions as precisely as possible.
The SIO produces reports in June, July,
and August containing a variety of perspectives on Arctic sea ice — from
observations of current conditions, to advanced
numerical models, to qualitative perspectives from citizen scientists.
In our work we use
observations as well as a hierarchy of
numerical models to study dynamical processes in the atmosphere,
and climate variability.
Individual responses were based on a range of methods: statistical,
numerical models, comparison with previous
observations and rates of ice loss,
and composites of several approaches.
It costs little to field the
observations — the satellites
and the radars, the surface in situinstruments, etc. to monitor conditions
and their changes; to assimilate the data into variety of
numerical models, to run these
and form ensemble averages; to disseminate the findings.
The July 2010 Sea Ice Outlook Report is based on a synthesis of 17 individual pan-Arctic estimates using a wide range of methods: statistical,
numerical models, comparison with
observations and rates of ice loss, composites of several approaches.
• Calibrate the retrospective simulations of ice thickness from our
numerical model against the aggregate of all the observation systems by removing the mean difference between the model and the observations to create a Calibrated Model Ice Thickness Re
model against the aggregate of all the
observation systems by removing the mean difference between the
model and the observations to create a Calibrated Model Ice Thickness Re
model and the
observations to create a Calibrated
Model Ice Thickness Re
Model Ice Thickness Record.
This activity also includes new interactions with NOAA NESDIS scientists regarding satellite
observations of the Antarctic ozone layer, their comparison to ground - based
and balloon - borne
observations,
and their interpretation with
numerical modeling and analysis tools.
This is what makes paleoreconstructions possible,
and what makes it possible to initialize global
numerical weather prediction
models with so few
observations.)
The individual responses were based on a range of methods: statistical,
numerical models, comparison with previous
observations and rates of ice loss, or composites of several approaches; details can be found in the individual outlooks available at the bottom of this page.
The individual responses were based on a range of methods: statistical,
numerical models, comparison with previous
observations and rates of ice loss, or composites of several approaches; details can be found in the individual outlooks available at the end of this report.
And different models may project different outcomes even under the same assumptions, due to the variety of «equally plausible numerical representations, solutions and approximations for modelling the climate system, given the limitations in computing and observations» [AR5, FAQ 12.1, p. 103
And different
models may project different outcomes even under the same assumptions, due to the variety of «equally plausible
numerical representations, solutions
and approximations for modelling the climate system, given the limitations in computing and observations» [AR5, FAQ 12.1, p. 103
and approximations for
modelling the climate system, given the limitations in computing
and observations» [AR5, FAQ 12.1, p. 103
and observations» [AR5, FAQ 12.1, p. 1036].
The studies are accomplished through the use of
observations and numerical models.
The Sea Ice Outlook, an activity of the Sea Ice Prediction Network
and a contribution to SEARCH, produces reports in June, July,
and August containing a variety of perspectives on Arctic sea ice — from
observations of current conditions, to advanced
numerical models, to qualitative perspectives from citizen scientists.
There are many drivers for increased resolution (spatial
and temporal) surface
observations, not least being new high resolution
numerical weather prediction (NWP)
models.
Convective
and mesoscale processes, intensity change, rainfall, airborne Doppler radar
observations, dropsondes,
numerical modeling
In it,
observations and a
numerical model that simulates one or more aspects of the Earth system are combined objectively to generate a synthesized estimate of the state of the system.
Boundary layer structure
and dynamics, turbulence
observations and theory, air - sea interaction,
numerical modeling and physical parameterizations
20th Century Reanalysis: Methods
and Applications To better understand
and model the observed variability of the earth system, one can rapidly expand the available record by objectively combining disparate
observations with
numerical model - generated guesses.
This would be a sterile activity indeed without the input of experimental
observation to guide the development of theoretical prediction methods
and to keep the relevant
numerical models «honest».
The predictions may match the
observations for a while, but very soon random fluctuations smaller than the distance between the measurements (they are called «sub-grid-scale eddies» in the vernacular of
numerical modellers) grow in size
and — as far as the
model is concerned — appear out of nowhere
and swamp the eddies we thought we knew something about.
Observations and numerical modeling reveal large fluctuations in the ocean heat available in the adjacent bay
and enhanced sensitivity of ice - shelf melting to water temperatures at intermediate depth, as a seabed ridge blocks the deepest
and warmest waters from reaching the thickest ice.
A combination of
numerical models, palaeoclimate data
and modern
observations indicated that ocean saltiness was key to understanding it.
Her work combines mathematical
and numerical modelling in comparison with
observations.
The IPCC's methodology relies unduly — indeed, almost exclusively — upon
numerical analysis, even where the outputs of the
models upon which it so heavily relies are manifestly
and significantly at variance with theory or
observation or both.
Your process will highlight your strengths in key competencies:
numerical and verbal reasoning, communication
and presentation, listening
and observation,
and understanding of business
models and concepts.