Attribution scientists
compare model simulations that include both manmade and natural factors against simulations that include only natural factors.
Not exact matches
«Therefore, we are always trying to
compare the
simulations with real phenomena to improve the
models.
She then created a computer
model of wind patterns and
compared the
simulations to the data to find out what information she still needed.
When they
compared the 2 - D results against those of the 3 - D
simulations, they found that the 2 - D
model underestimated how quickly the flood wave moved across land and overestimated the time at which the maximum flood occurred.
Unfortunately, current
simulation models, which combine global climate
models with aerosol transport
models, consistently underestimate the amount of these aerosols in the Arctic
compared to actual measurements during the spring and winter seasons, making it difficult to accurately assess the impact of these substances on the climate.
They then
compared their yearly September ozone measurements with
model simulations that predict ozone levels based on the amount of chlorine that scientists have estimated to be present in the atmosphere from year to year.
For the RCP8.5 projections, which represents stronger increases in greenhouse gas concentrations than RCP4.5, there was a striking level of consistency in the magnitude of change in AR frequency — all
models showed an approximate doubling of the number of future ARs
compared to the
simulations for 1980 — 2005.
«And when we
compare the
models to the data, there's a stunning similarity between the star - forming showers we observe and ones that occur in
simulations.
Changes in fall - winter rainfall from observations (top panel) as
compared to
model simulation of the past century (middle panel), and a
model projection of the middle of the 21st century.
Computer
simulation is similar, it's reductionist; you've got these parts, you want to see how they interact, so you build a
model and
compare it to the real world.
Until now this type of analysis has been a tedious process that involves
comparing actual images of lenses with a large number of computer
simulations of mathematical lensing
models.
However, unlike the climate
model simulations, the new precipitation reconstruction does not show an increase of wet and dry anomalies in the twentieth century
compared to the natural variations of the past millennium.
In a unique study set - up, the scientists first
compared simulation results from a large ensemble of wheat crop growth
models with experimental data, including artificial heating experiments and multi-locational field trials.
To better understand the physical mechanisms of rapid ocean adjustment, the data was
compared with a climate
model simulation which covers the same period.
A particular emphasis of Hayward's research is on combining hydrodynamic
simulations of galaxy formation with radiative transfer calculations to create «forward
models» of observable quantities, such as images and spectra, that can be directly
compared with data from telescopes such as the Hubble Space Telescope.
Running future
simulations in climate
models with present - day emissions, Cai and his colleagues find 73 per cent increase in extreme La Niña events in the twenty - first century when
compared to the twentieth.
It is a pity that they stopped the
simulation before the CO2 decrease (111,000 - 106,000 BP), to see what the
model produces for further cooling,
compared to reality...
To understand the role of human - induced climate change in these new records they
compare simulations of the Earth's climate from nine different state - of - the - art climate
models and the very large ensemble of climate
simulations provided by CPDN volunteers for the weather@home ANZ experiments for the world with and without human - induced climate change.
They
compared the empirical data to the
model simulations of the MJO, where much of the MJO processes are currently represented with parameterizations, a way to express complex climate systems in a computationally efficient way.
Detailed
simulations of blend
models composed of an eclipsing binary plus a third star diluting the eclipses were
compared with the observed light curve and used to derive the properties of the three components.
They
compared these methods against a detailed
model estimate to see how they measured up against the benchmark
simulations.
Working with Tom Chase, a colleague at the institute, the researchers were
comparing climate
simulations from the Community Land
Model — part of a select group of global
models used in the Intergovernmental Panel on Climate Change's 2007 climate change report — against observations.
Two groups of students, those who used real equipment and those who used a computer
simulation that explicitly
modeled electron flow, were
compared in terms of their mastery of physics concepts and skills with real equipment.
Compared to the previous Ridgeline
model, the coefficient of drag x area (CdA) is reduced 15 percent, as determined by CFD
simulations.
When looking for SYSTEMATIC deviations between data and
model simulations, one calculates the mean and the standard deviation of the mean for each and
compares.
«By
comparing the response of clouds and water vapor to ENSO forcing in nature with that in AMIP
simulations by some leading climate
models, an earlier evaluation of tropical cloud and water vapor feedbacks has revealed two common biases in the
models: (1) an underestimate of the strength of the negative cloud albedo feedback and (2) an overestimate of the positive feedback from the greenhouse effect of water vapor.
With error bars provided, we can use the PIOMAS ice volume time series as a proxy record for reality and
compare it against sea - ice
simulations in global climate
models.
The authors
compared recently constructed temperature data sets from Antarctica, based on data from ice cores and ground weather stations, to 20th century
simulations from computer
models used by scientists to simulate global climate.
Decadal hindcast
simulations of Arctic Ocean sea ice thickness made by a modern dynamic - thermodynamic sea ice
model and forced independently by both the ERA - 40 and NCEP / NCAR reanalysis data sets are
compared for the first time.
In a related paper, Santer et al
compare the surface / lower - troposphere coupled tropical variability at different timescales in the data and in
model simulations performed for the new IPCC assessment.
As a check of this, one could
comparing the climate
model simulations of temperature change using the historical forcing runs with the temperature change produced by the same
models under CO2 - only forcing runs * at times of equivalent total forcing change *.
I did so, and in so doing pointed out a number of problems in the M&N paper (
comparing the ensemble mean of the GCM
simulations with a single realisation from the real world, and ignoring the fact that the single GCM realisations showed very similar levels of «contamination», misunderstandings of the relationships between
model versions, continued use of a flawed experimental design etc.).
Vecchi et al.
compared the observed trend in the Walker circulation between 1861 and 1992 to that yielded by
simulations from the GFDL CM2 general circulation
model, run with and without anthropogenic forcing.
Julie Hargreaves has a new paper out on this precise question and shows that the early
model simulations had substantial skill
compared to any naive
model.
A detailed reanalysis is presented of a «Bayesian» climate parameter study (Forest et al., 2006) that estimates climate sensitivity (ECS) jointly with effective ocean diffusivity and aerosol forcing, using optimal fingerprints to
compare multi-decadal observations with
simulations by the MIT 2D climate
model at varying settings of the three climate parameters.
http://journals.ametsoc.org/doi/abs/10.1175/JCLI-D-16-0628.1 In our discussion exploring the (very minor) differences in results when using different datasets we said: - «Dataset creation approaches that infill missing data areas may give overconfidence to climate changes in regions where there are no direct measurements, when
compared with
model simulations that have data in those regions.»
It is a pity that they stopped the
simulation before the CO2 decrease (111,000 - 106,000 BP), to see what the
model produces for further cooling,
compared to reality...
Interestingly, the long - term variations indicated by the
model simulations compared remarkably well with those documented by the tree - ring reconstruction, showing no obvious sign of the potential biases in the estimated low - frequency temperature variations that have been the focus of much previous work (see e.g. this previous RealClimate review).
Forest et al. 2006
compares observations of multiple surface, upper air and deep - ocean temperature changes with
simulations thereof by the MIT 2D climate
model run at many climate parameter settings.
The aim of increasing resolution in AGCMs is generally to improve the
simulation of surface climatology
compared to coarser resolution
models (Cubash et al., 1995).
Both periods had a substantially different climate
compared to the present, and there is relatively good information from data synthesis and
model simulation experiments (Braconnot et al., 2004; Cane et al., 2006).
Judith, I think falling best estimates for aerosol offsets in the SOD (
compared to AR4) and simultaneous continued use of earlier (larger) aerosol offsets in the climate
model simulations borders on daft.
The most popular observationally - constrained method of estimating climate sensitivity involves
comparing data whose relation to S is too complex to permit direct estimation, such as temperatures over a spatio - temporal grid, with
simulations thereof by a simplified climate
model that has adjustable parameters for setting S and other key climate properties.
We can therefore again
compare the Scenario A2 multi-
model global surface warming projections to the observed warming, in this case since 2000, when the AR4
model simulations began (Figure 9).
In
model's
simulations, the drop in central pressure is relatively more in the months of May, June, September and October during 2071 — 2100
compared with that during 1961 — 1990.
However,
model physics process representations that are supposed to account for the eddy moisture transport effects on convection significantly underestimate them
compared to
simulations that explicitly resolved eddy moisture transport without using convective representations.
These reconstructions are highly relevant when
comparing ocean data with
model simulations of global and regional climate change.
I saw a poster a at a meeting last year that
compared a
simulation with prescribed SST to another with a slab ocean
model (SOM) and the results were very striking, so I started thinking that I need to explore this type of
modelling more.
> A major advance of this assessment of climate change projections
compared with the TAR is the large number of
simulations available from a broader range of
models.
In your blog post you mentioned a lot of recently published papers that show
model simulations don't do well
compared to observations even in hindcast.