FMI has been involved in research project, which evaluated the simulations of long - range transport of BB aerosol by the Goddard Earth Observing System (GEOS - 5) and four other global aerosol models over the complete South African - Atlantic region using Cloud - Aerosol Lidar with Orthogonal Polarization (CALIOP) observations to find any distinguishing or
common model biases.
Not exact matches
Thus, the agreement between the new semi-empirical
model and the physical
models could be taken as suggesting that both share a
common historical
bias.
Though ancestral Boule may have also functioned in oogenesis, our findings that bilaterian Boule homologs tend toward male -
biased expression, taken together with the similar spermatogenesis arrest phenotypes in both Drosophila and mouse mutants, supports the
model of a
common origin of bilaterian spermatogenesis.
«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.
Crichton seems unaware that the discussion of climate
model validation is a
common feature of publications utilizing these
models and
model errors and
biases are often explicitly quantified and described.
I have been worrying that even
common properties of all present climate
models and
models than can be developed in near future may
common bias towards such stability that is not necessarily true for the real Earth system.
This indicates possible
common errors among GCMs although we can not exclude the possibility that the discrepancy between
models and observations is partly caused by
biases in satellite data.
Unless these nine
models share
common systematic
biases, it is thus expected that the average 2014 September Arctic sea ice extent will be in the range 3.95 - 5.6 million km ², and likely above the trend line (5.1 million km ²), a situation similar to 2013.
Po Chedley say: «The apparent
model - observational difference for tropical upper tropospheric warming represents an important problem, but it is not clear whether the difference is a result of
common biases in GCMs,
biases in observational datasets, or both.»
Because poor simulation of meteorological variables is
common in climate
models, a determination that meteorological variability is more important for certain variables than leaf variability may point to meteorological
bias correction as a more fruitful development path — for certain
model applications — than the development of a dynamic phenological routine.
• These results could arise due to errors
common to all
models; to significant non-climatic influences remaining within some or all of the observational data sets, leading to
biased long - term trend estimates; or a combination of these factors.
A
common misconception is that climate
models are
biased towards exaggerating the effects from CO2.