The analysis uses methods that have already been peer - reviewed, including examining the change in occurrence of such extreme rains in the historical record and in climate models, as well as using finer -
scale regional climate models to compare the current climate to one without warming.
Not exact matches
Better predictions would require improved
climate - measurement tools, more sophisticated
climate models that work on
regional scales, and a better organized system to integrate all the data, the report concludes.
«This new high - resolution
climate model is able to simulate
regional -
scale precipitation with considerably improved accuracy compared to previous generation
models,» said Tom Delworth, a research scientist at NOAA's Geophysical Fluid Dynamics Laboratory in Princeton, N.J., who helped develop the new
model and is co-author of the paper.
But the critical coastal process, which actually generates more of the deep water, occurs on smaller
scales and is only captured in high - resolution
regional climate models, Knudson said.
Those findings will be integrated into an atmospheric
model that will assess the implications of the findings on local and
regional climate scales.
Scientists are involved in the evaluation of global -
scale climate models,
regional studies of the coupled atmosphere / ocean / ice systems,
regional severe weather detection and prediction, measuring the local and global impact of the aerosols and pollutants, detecting lightning from space and the general development of remotely - sensed data bases.
January 2004: «Directions for
Climate Research» Here, ExxonMobil outlines areas where it deemed more research was necessary, such as «natural climate variability, ocean currents and heat transfer, the hydrological cycle, and the ability of climate models to predict changes on a regional and local scale.
Climate Research» Here, ExxonMobil outlines areas where it deemed more research was necessary, such as «natural
climate variability, ocean currents and heat transfer, the hydrological cycle, and the ability of climate models to predict changes on a regional and local scale.
climate variability, ocean currents and heat transfer, the hydrological cycle, and the ability of
climate models to predict changes on a regional and local scale.
climate models to predict changes on a
regional and local
scale.»
What's Next: PNNL scientists are using a
regional model at a much finer
scale than conventional
climate models to understand the processes that determine the time -
scales of MJO and the roles of various types of clouds in its energy cycle.
These programs focus on
climate, aerosol and cloud physics; global and
regional scale modeling; integrated assessment of global change; and complex
regional meteorology and chemistry.
He has had a central role in PNNL's global aerosol, chemistry, and
climate modeling, and in
modeling studies of aerosols and cloud - aerosol interactions at local and
regional scales.
High - resolution simulations are being performed that resolve the local and
regional variations of particulate characteristics to obtain a better understanding of important aerosol processes that need to be incorporated into larger -
scale climate models.
Our
climate forcing
models account for 18 — 88 % (ave = 0.60) of the annual variability at the local
scale, and 66 — 77 % (ave = 0.71) at the
regional scale when nesting data from 1954 — 2009 are considered (Table S1).
Within the integrated Earth system science paradigm, our major research thrusts include the physics and chemistry of aerosols, clouds and precipitation; integrating our understanding of
climate, energy, and other human and natural systems through the development and application of
models that span a wide range of spatial
scales; and determining the impacts of and informing responses to
climate and other global and
regional environmental changes.
Concerning
climate - change forecasting, we can not expect that increased computer power and improved
climate models will in the future «give more precise probability distributions of outcomes at the
regional and decadal
scales».
And of course there's still substantial uncertainty in
climate models at the
regional scale in war - prone places (again, a prime example is the set of countries along the southern fringe of the Sahara Desert, where
models still clash on which areas will grow drier or wetter; see my Somalia posts.)
We quantify sea - level commitment in the baseline case by building on Levermann et al. (10), who used physical simulations to
model the SLR within a 2,000 - y envelope as the sum of the contributions of (i) ocean thermal expansion, based on six coupled
climate models; (ii) mountain glacier and ice cap melting, based on surface mass balance and simplified ice dynamic
models; (iii) Greenland ice sheet decay, based on a coupled
regional climate model and ice sheet dynamic
model; and (iv) Antarctic ice sheet decay, based on a continental -
scale model parameterizing grounding line ice flux in relation to temperature.
Finally, simulations having finer spatial detail (i.e., «downscaled»
climate model projections) do not necessarily have greater accuracy than coarser - resolution simulations; they add contextual detail related to factors such as
regional topography and coastlines but may still retain the same basic climatic features simulated at larger
scales.
Can the
models provide skillful predictions of changes in
regional climate statistics on multi-decadal time
scales?»
This is one of the more challenging aspects of
modeling of the
climate system because precipitation involves not only large -
scale processes that are well - resolved by
models but also small -
scale process, such as convection, that must be parameterized in the current generation of global and
regional climate models.
Global and
regional climate models have not demonstrated skill at predicting
regional and local
climate change and variability on multi-decadal time
scales.
Climate models are also used on regional scales in attempts to figure out way climate models don't perform well on regional
Climate models are also used on
regional scales in attempts to figure out way
climate models don't perform well on regional
climate models don't perform well on
regional scales.
By putting
models through their paces in an all - water world, scientists at Pacific Northwest National Laboratory found highly
scale - sensitive issues in
regional climate modeling.
«This new high - resolution
climate model is able to simulate
regional -
scale precipitation with considerably improved accuracy compared [continue reading...]
They can't even predict the next decade, much less ten decades; despite tuning they only poorly replicate the historical
climate; their equations can't be shown to converge; the number of tunable parameters is far too large for comfort; they show absolutely no skill at
regional scales; their results for things they are not tuned to replicate (e.g. rainfall) are abysmal — in short they are glorified Tinkertoy ™
models which have one common characteristic... they don't work well.
Contribution from working group I to the fifth assessment report by IPCC TS.5.4.1 Projected Near - term Changes in
Climate Projections of near - term climate show small sensitivity to Green House Gas scenarios compared to model spread, but substantial sensitivity to uncertainties in aerosol emissions, especially on regional scales and for hydrological cycle var
Climate Projections of near - term
climate show small sensitivity to Green House Gas scenarios compared to model spread, but substantial sensitivity to uncertainties in aerosol emissions, especially on regional scales and for hydrological cycle var
climate show small sensitivity to Green House Gas scenarios compared to
model spread, but substantial sensitivity to uncertainties in aerosol emissions, especially on
regional scales and for hydrological cycle variables.
Part of this is a resolution issue, but the more important issue is the modes of natural internal variability, which the
climate models do a so - so job on in a large -
scale sense, but not in translating the impacts to a
regional level.
David, I don't think
climate models are very useful for the
regional scale applications of relevance for hydrological applications.
While
regional climate downscaling yields higher spatial resolution, the downscaling is strongly dependent on the lateral boundary conditions and the methods used to constrain the
regional climate model variables to the coarser spatial
scale information from the parent global
models.
There are numerous studies where
regional climate model studies have increased our understanding of the mechanism of the
climate system acting on a
regional scale.
To present
regional multi-decadal
climate projections to the impact communities as part of their driving forces and boundary conditions (for their
models and process studies), when there is NO skill on this time
scale at predicting changes in
climate statistics, is a serious misleading application of the scientific method.
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.
Roger states that one can not consider
climate model predictions (his type 4) at the
regional scale when their predictive skill in hindcast mode is not demonstrated.
«We do argue, however, that
regional climate models can provide useful information about
climate change as long as there is some value in the large -
scale infor ¬ mation provided by the multimodel GCM ensembles.
My bottom line is that while the global
climate models, when run with added CO2 and other greenhouse gases, show that this is a warming effect, they are inadequate tools to assess the consequences of these human
climate forcings on the
regional and local
scale.
The growing interest in GCM performance at
regional scales, rather than global, has come from at least two different directions: the
climate modelling community and the
climate change adaptation community.
As they have matured,
climate models are being increasingly used to provide decision - relevant information to end users and policy makers, whose needs are helping define the focus of
model development in terms of increasing prediction skill on
regional and decadal time
scales.
The inability of global
climate models to match the timing or placement of short - term or
regional precipitation patterns such as the West African monsoon may be alleviated by «downscaling» to use smaller
scale climate models with increased area resolution.
The mechanics of the
models produce
regional scale results, but, until the multi-decadal
regional predictions of changes in
climate statistics can be shown to be skilful, the added spatial resolution provides an erroneous illusion of skill.
Probably the stronger demand for
regional scale information from
climate models is coming from the
climate change adaptation community.
The reasons for the
regional differences in historical
scaled - interannual and future 30 - year trend regressions are unclear, since as noted above the
model's interannual NAO variability does not appear to be affected by
climate change between 1850 and 2045.
NorACIA have both used the facts from the IPCC and local data and
scaled down global
climate models to
regional effects.»
In terms of longer timescales (decadal to century), once the focus becomes
regional rather than global, historical and paleo data becomes more useful than global
climate model simulations (no matter what type of «right -
scaling» methods are attempted).
Analyses of tide gauge and altimetry data by Vinogradov and Ponte (2011), which indicated the presence of considerably small spatial
scale variability in annual mean sea level over many coastal regions, are an important factor for understanding the uncertainties in
regional sea - level simulations and projections at sub-decadal time
scales in coarse - resolution
climate models that are also discussed in Chapter 13.
Methodological advances since the TAR have focused on exploring the effects of different ways of downscaling from the
climate model scale to the catchment
scale (e.g., Wood et al., 2004), the use of
regional climate models to create scenarios or drive hydrological
models (e.g., Arnell et al., 2003; Shabalova et al., 2003; Andreasson et al., 2004; Meleshko et al., 2004; Payne et al., 2004; Kay et al., 2006b; Fowler et al., 2007; Graham et al., 2007a, b; Prudhomme and Davies, 2007), ways of applying scenarios to observed
climate data (Drogue et al., 2004), and the effect of hydrological
model uncertainty on estimated impacts of
climate change (Arnell, 2005).
But running point
scale intercomparisons of the sort Koutsoyiannis did tells you little about the validity of the
model with respect to the purpose for which it is designed; but does underline the limits of global
models for
regional climate work.
Key remaining uncertainties relate to the precise magnitude and nature of changes at global, and particularly
regional,
scales, and especially for extreme events and our ability to simulate and attribute such changes using
climate models.
The most critical shortcomings of the assessment are the attempt to extrapolate global -
scale projections down to
regional and sub-
regional scales and to use two
models which provide divergent projections for key
climate elements.»
Second, nearly every impact of importance is driven by what is liable to happen to the
climate on the
regional to local
scale, but it is well known that current global -
scale models have limited ability to simulate
climate effects as this degree of spatial resolution.
One approach to this problem is «downscaling,» a procedure in which
climate changes in large -
scale atmosphere and ocean conditions predicted by a global
model are used as input to a fine -
scale regional model that does resolve tropical cyclones.
The
climate models got scores far worse than a random walk, indicating a complete failure to provide valid forecast information at the
regional level, even on long time
scales.