There are many
other atmospheric observations and models we need to look at to see how this entire process works.»
EWeLiNE combines these data with
other atmospheric observations — from ground - based weather stations, radar and satellites — and sophisticated computer models predict power generation over the next 48 hours or so.
All
the other atmospheric observation - derived estimates include elements of causation and correlation mixed in.
Not exact matches
Other than in previous publications, optical rogue waves in this system are clearly ruled by
atmospheric turbulence in a gas cell, effectively enabling the
observation of a storm in a test tube.
This discovery, and
other observations made by the Penn State team, provide insight into the complexity of weather and
atmospheric composition on exoplanets, and may someday be useful for gauging the habitability of Earth - size planets.
Your statement that «Thus it is natural to look at the real world and see whether there is evidence that it behaves in the same way (and it appears to, since model hindcasts of past changes match
observations very well)» seems to indicate that you think there will be no changes in ocean circulation or land use trends, nor any subsequent changes in cloud responses thereto or
other atmospheric circulation.
Other types of
atmospheric pollution can interfere with astronomic
observations as well.
This method tries to maximize using pure
observations to find the temperature change and the forcing (you might need a model to constrain some of the forcings, but there's a lot of uncertainty about how the surface and
atmospheric albedo changed during glacial times... a lot of studies only look at dust and not
other aerosols, there is a lot of uncertainty about vegetation change, etc).
Your statement that «Thus it is natural to look at the real world and see whether there is evidence that it behaves in the same way (and it appears to, since model hindcasts of past changes match
observations very well)» seems to indicate that you think there will be no changes in ocean circulation or land use trends, nor any subsequent changes in cloud responses thereto or
other atmospheric circulation.
«Ion - induced nucleation [cosmic ray action] will manifest itself as a steady production of new particles [molecular clusters] that is difficult to isolate in
atmospheric observations because of
other sources of variability but is nevertheless taking place and could be quite large when averaged globally over the troposphere [the lower atmosphere].»
William: Yes, however, there are sets of
other observations that logically supports the assertion that the majority of the warming in the last 150 years was due to solar magnetic cycle changes rather than the increase in
atmospheric CO2 and that the planet is about to significantly cool due to the current solar magnetic cycle change.
The synoptic surface
atmospheric observations assimilated by ERA - Interm are reported as dewpoints and the synoptic message that contains the dew points also reports temperature and surface pressure, whose values are needed to compute
other humidity variables.
GLOBALVIEW data products are designed to enhance the spatial and temporal distribution of
atmospheric observations of CO2, CH4 and
other related
atmospheric measurements.
Program areas at GISS may be roughly divided into the categories of climate forcings; climate model development; Earth
observations;
atmospheric radiation;
atmospheric chemistry; climate impacts; planetary atmospheres, exoplanets, and astrobiology; paleoclimate; and
other disciplines.
In addition to treating cloud transmission based only on the measurements at the local time of the TOMS
observations, the results from
other satellites and weather assimilation models can be used to estimate
atmospheric UV irradiance transmission throughout the day.
Wang, 5.0 (± 0.27), Modeling A projected September Arctic sea ice extent of 5.0 million km2 is based on a NCEP ensemble mean CFSv2 forecast initialized from the NCEP Climate Forecast System Reanalysis (CFSR) that assimilates observed sea ice concentrations and
other atmospheric and oceanic
observations.
The behaviour of temperature, along with a lot of
other observations, is all backing up the general picture of the planet shifting climate to get into balance with the new
atmospheric composition.
As ARM's newest
observation facility, the Eastern North Atlantic began operations in September 2013 and mirrors ARM's
other long - term
atmospheric measurement facilities around the world.
Evaluating the quality and consistency of
atmospheric Reanalysis is not a goal of this study, but we use it as a secondary data source when no
other suitable
observations readily exist.
One
other factor over the period post-1945 to 1963 which limited and affected SST
observations in the Pacific Ocean were the various nuclear test series, for numerous military, political, physical and biohazard reasons, and the consequential local hydrophysical, hydrobiological, and
atmospheric perturbations such testing occasioned.
Measured decreases in the fraction of
other forms of carbon (the isotopes 14C and 13C) and a small decrease in
atmospheric oxygen concentration (
observations of which have been available since 1990) show that the rise in CO2 is largely from combustion of fossil fuels (which have low 13C fractions and no 14C).
Three - dimensional (3D) planetary general circulation models (GCMs) derived from the models that we use to project 21st Century changes in Earth's climate can now be used to address outstanding questions about how Earth became and remained habitable despite wide swings in solar radiation,
atmospheric chemistry, and
other climate forcings; whether these different eras of habitability manifest themselves in signals that might be detected from a great distance; whether and how planets such as Mars and Venus were habitable in the past; how common habitable exoplanets might be; and how we might best answer this question with future
observations.
So do many
other independent
observations of changes in temperature, the hydrological cycle,
atmospheric circulation, and the cryosphere (41, 42).