These include fundamental climate research,
improved observations and modeling, increased computational capability, and very importantly, education of the next generation of climate scientists.
Not exact matches
Medvigy
and Jeong found that prediction
modeling for the entire United States indeed
improves dramatically when the analyses include data from macro-scale
observations, meaning from multiple sites spread over a large area.
They go on to suggest that «lowering levels of TNF may be an effective strategy in
improving host defense against S. pneumoniae in older adults,»
and that, «although it may be counterintuitive to limit inflammatory responses during a bacterial infection, [some existing] clinical
observations and our animal
model indicate that anti-bacterial strategies need to be tailored to the age of the host.»
These real - world
observations will help USGS scientists fine - tune their
models and improve their damage predictions before the next big storm.
This
observation required a revision of common theoretical
models describing the photoemission from solids, i.e. this initial intra-atomic interaction had to be taken into account
and sets a new cornerstone for future
improved models of the photoemission process from solids.
According to the researchers, to better understand if Matthew's intensification was aided by the warm - water eddies
and the residing barrier layer in the Caribbean Sea's upper ocean, more ambient
and in - storm upper ocean
observations in this basin are needed to
improve forecast
models for the region.
New
observations and new
models contributed to this certainty, ranging from Antarctic ice cores to
improved understanding of solar fluxes.
«As astrophysical
observations and simulations
improve, we're doing increasingly precise comparisons between the
models of how galaxies form
and the
observations of what galaxies actually look like,» Carroll says.
The ARM Climate Research Facility is managed to ensure it fulfills its mission to provide
observation data to
improve the understanding of climate processes
and the representation of those processes in climate
models.
The
models need to be tested against
observations, to make way for new
and improved models.
All these
observations will be combined to
improve climate
models, which will provide an estimate of present - day
and future surface melt on the East Antarctic ice shelves.
Over five days, the conference will offer a fruitful meeting of observers involved in various ground -
and space - based programs with modelers
and theoreticians, in order to raise new
observations and new
models to
improve our comprehension
and knowledges of exoplanets.
The effort uses innovative ARM radar
observations from the MC3E field campaign to evaluate a series of high - resolution simulations, which results in an
improved understanding of cloud transitions
and how to diagnose these transitions in
models.
The meeting presentations will focus on synergies among various approaches
and provide recommendations on how to
improve the use of earth
observations, ground data
and modeling techniques for the
improved understanding of land use sources
and sinks.
Individual components continue to be
improved via systematic evaluation against
observations and against more comprehensive
models.
To
improve parameterization, the researchers propose developing Earth system
models that learn from the rich data sets now available (thanks, in large part, to satellite
observations)
and high - resolution simulations on local scales.
The ARM Aerosol Measurement Science Group (AMSG) coordinates ARM Climate Research Facility
observations of aerosols
and atmospheric trace gases with user needs to ensure advanced, well - characterized observational measurements
and data products — at the spatial
and temporal scales necessary — for
improving climate science
and model forecasts.
The Southern Ocean Carbon
and Climate
Observations and Modeling project, which involves Climate Central staff
and aims to track changes underway surrounding Antarctica, has developed
improved pH sensors that could operate for five years or more on autonomous diving instruments.
A wide variety of quantitative scientists (computational biologists, statisticians, mathematicians, computer scientists, engineers,
and physicists) are working to
improve the quality of these approaches
and to create, refine,
and retest the
models to accurately reflect
observations.
(2) A program must use information from paragraph (b)(1) of this section with informal teacher
observations and additional information from family
and staff, as relevant, to determine a child's strengths
and needs, adjust strategies to better support individualized learning
and improve classroom practices in center - based
and family child care settings
and improve home visit strategies in home based
models.
To meet both the objectives of a PDS
model and to
improve the diversity of field experiences, the GOALS
model uses two concurrent quasi-PDS partnerships: the distance - learning
observation partnership
and the PK - 12 school practica partnership.
Still besides empirical
observations and good inferences, the
models are what are available to work with,
and they serve several purposes quite well
and they are the basis for
improved models in the future.
Improving observations to better characterize that state, and improving models to carry this information forward in time is our best hope to improve seasonal predic
Improving observations to better characterize that state,
and improving models to carry this information forward in time is our best hope to improve seasonal predic
improving models to carry this information forward in time is our best hope to
improve seasonal predictability.
The available tools are time - dependent
model forecasts which incorporate the
improved observations of changes in the ocean
and simulate its likely influence on the short - to medium - term future.
eg pg xii To
improve our predictive capability, we need: • to understand better the various climate - related processes, particularly those associated with clouds, oceans
and the carbon cycle • to
improve the systematic
observation of climate - related variables on a global basis,
and further investigate changes which took place in the past • to develop
improved models of the Earth's climate system • to increase support for national
and international climate research activities, especially in developing countries • to facilitate international exchange of climate data
Progress in the longer term depends on identifying
and correcting
model biases, accumulating as complete a set of historic
observations as possible,
and developing
improved methods of detection
and correction of observational biases.»
Penn State
and the University of Hawaii both shared a grant of $ 770,000 for a research project called «
Improved Projections of the Climate Response to Anthropogenic Forcing: Combining Paleoclimate Proxy
and Instrumental
Observations with an Earth System
Model».
Improving the representation of feedbacks in climate
models,
and checking them against
observations, is probably the most important area of climate
modelling research at present.
We also need to
improve the systematic
observation of climate - related variables on a global basis; to investigate further past changes; to develop
improved models of the Earth's climate system; to increase support for national
and international climate research activities, especially in developing countries;
and to facilitate the international exchange of climate data.
If only let's say 90 % of the budgets spent on computer
modeling had gone on more extensive, more detailed
observations since 1979 (the date of that sensitivity of 3 plus or minus 1.5 which seems to have so influenced the modelers
and proven so hard for them to
improve upon much).
But ideas (geometry)
and instruments (telescopes) provided
observations that
improved the accuracy of the
model.
To
improve parameterization, the researchers propose developing Earth system
models that learn from the rich data sets now available (thanks, in large part, to satellite
observations)
and high - resolution simulations on local scales.
We demonstrate that the combination of lower estimates of the 20th century GMSL rise (up to 1990)
improved modeling of the GIA process
and that the correction of the eclipse record for a signal due to angular momentum exchange between the fluid outer core
and the mantle reconciles all three Earth rotation
observations.
There are some source of predictability that are still not fully resolved (including those dealing with
improving climate
models, but also related to unexplored initial conditions or driving conditions),
and a great benefit of these predictability studies is that they mimic the practice of weather prediction by confronting
models with
observations at the relevant time
and spatial scales, leading to the necessary inspiration for this
model improvement.
These two projects
and cooperative partners will
improve sea ice
observation and modelling on regional
and local scale as well as support to climate research in the Polar Regions.
The present scope includes accurately monitoring column ozone with Dobson spectrophotometers globally, monitoring the ozone profile at key sites, monitoring all relevant chlorine -
and bromine - containing compounds globally,
improving and developing new instrumentation, conducting laboratory studies of newly proposed chemicals,
and using statistical
models to test the
observations for signs of ozone layer recovery.
This project will advance our understanding of seasonal ice zone (SIZ) cloud - ice feedbacks
and our ability to forecast SIZ weather
and ice conditions through the combination of carefully designed
model experiments,
observations,
and technology developments which are targeted to validate
and improve the
models.
Such adjustments, even if they
improve the match between
model output
and observations, do not mean that we have
improved the
model.
For what it's worth, I have talked to
model developers at length about this
and I've been involved in
improving the way that
observations are used to challenge
models.
Removing the influence of two major modes of natural internal variability (the Arctic Oscillation
and Pacific Decadal Oscillation) from
observations further
improves attribution results, reducing the
model -
observation discrepancy in cold extremes.
However, the heat island effect, if present, would in fact
improve rather than worsen the agreement between
models and observations (without it, the temperature in the most recent years would be lower, while GCMs predict a rise of temperature).
Climate change researchers can not hide behind the need to
improve models and observations any longer.
Furthermore, high - resolution satellite
observations are increasingly being used to validate
and improve model realism.
Identify new sources of predictive skill
and improve predictions of weather, water,
and climate through
observations, understanding,
and modeling of physical processes
and phenomena of the coupled Earth system.
Higher resolution
observations have recently become available,
and model A could possibly be
improved in future studies.
A study by Mitrovica et al. (2015) has demonstrated that the combination of lower estimates of the GMSL rise between 1900
and 1990 (~ 1.2 mm yr - 1),
improved modeling of the GIA process
and the signal due to core - mantle coupling in ancient eclipse
observations resolves «Munk's enigma.»
Develop interagency
and international support for enhanced
observations of the arctic atmosphere via buoys, soundings, etc. in order to constrain, evaluate,
and improve operational
model performance in the central Arctic.
Predictions of sea ice changes will have large uncertainties without sustained
observations;
improved understanding of ice, ocean, land,
and atmospheric processes;
and advances in coupled
and system
models.
The ARM Climate Research Facility is managed to ensure it fulfills its mission to provide
observation data to
improve the understanding of climate processes
and the representation of those processes in climate
models.