They have far more
mass than the atmosphere so they contain far more of the additional energy.
Not exact matches
Because they are much smaller
than other solar eruptions — like flares or coronal
mass ejections — prominences had previously been thought to have a relatively minor effect on the sun's
atmosphere, and therefore also on the solar wind.
Its higher
mass may give it a thicker
atmosphere and more cloud cover
than Earth has.
Computer simulations show that planets similar to or larger in
mass than the Earth that are born with thick envelopes of hydrogen and helium are likely to retain their stifling
atmospheres.
As a comparison, our
atmosphere accounts for less
than one - millionth of Earth's
mass.
The data allowed them to confirm the
mass of the planet as well as determine the approximate metallicity (a number of elements heavier
than hydrogen and helium within a celestial body), and the primary composition of the planet's
atmosphere.
In 2010, a new study (which included better model
atmosphere fitting) argued that the system is around six billion years old, even older
than estimates of 3.7 to 4.3 billion years derived from a 2009 study based on
mass and evolutionary models for the two brown dwarf companions Ba and Bb (Liu et al, 2010; and King et al, 2009), which are much older
than an earlier age estimate of between 0.8 and 2.0 billion years based on the star's rotational speed (press release; Scholz et al, 2003; and Lachaume et al, 1999).
While that may not sound like much, Earth's
atmosphere, by comparison, is less
than one millionth the
mass of the planet.
While larger planets could have sufficient gravity to attract a massive hydrogen - helium
atmosphere, smaller planets — like Mars or Mercury that have less
than half the Earth's
mass — located in or near their star's habitable zone may lose their initial life - supporting
atmosphere because of low gravity and / or the lack of plate tectonics needed to recycle heat - retaining carbon dioxide gas back into the
atmosphere (Kasting et al, 1993).
TRAPPIST - 1c is similarly rocky but with a thinner
atmosphere, and 1d is the lightest, with less
than a third of the
mass of Earth.
By surveying the whole sky, we will find systems that orbit stars 10 times closer and 100 times brighter
than those found by Kepler — opening up new possibilities for measuring planet
masses and densities, studying their
atmospheres, characterizing their host stars, and establishing the full nature of the systems in which the planets reside.
All territorial clashes, aggressive cryptograms, and death threats were nullified into a
mass of spray - painted gestures that had become nothing more
than atmosphere, their violent disputes transposed into an immense, outdoor, nonrepresentational mural.
Basically what we are saying is that normal greenhouse is based on having less thermal
mass to heat
than the
atmosphere as whole due to seperation from that
atmosphere, and to a lesser extent on insulation due to the air not moving as much.
A stronger gravitational field will produce a lower, denser, warmer surface
than a weaker gravitational field since the amount of solar energy retained by the
atmosphere will be focused into a smaller volume and that amount of energy will be determined by the amount of
mass available to absorb it at any given level of solar irradiation.
The
atmosphere of Venus is mostly CO2 but the atmospheric heat arises as a result of the
mass and density of the Venusian
atmosphere (apparently more
than 90 times that of the Earth) not just the absorption characteristics of CO2.
If the surface and lower
atmosphere become warmer
than the temperature set by insolation, gravity and
mass they will emit more energy to space, there will be more energy outgoing
than incoming and the system will cool back to the earlier temperature.
So the whole rising air
mass experiences less cooling
than it would in a dry
atmosphere.
First, the surface temperature of the Earth is roughly 60 F higher
than it would otherwise be thanks to a few greenhouse gasses that collectively make up only about 3 percent of the
mass of our
atmosphere.
You say that the descending air would heat up more
than the «surrounding
atmosphere»... but the air mixes and descends over the entire area and the entire air
mass warms, there is no «surrounding
atmosphere» in the sense you mean.
Add to that the thinning of 14C in the
atmosphere by the release of 14C free fossil fuels and thinning by the increase of total CO2
mass, and it is clear that the 14C as tracer is going down much faster
than what an extra 12C / 13C
mass does.
Argon
mass fraction in the
atmosphere is more
than 20 times higher
than CO2
mass fraction.
Given its large
mass and high heat capacity, the ability of the Ocean to absorb heat is 1000 times larger
than that of the
atmosphere.
They found that the vast majority of energy released from the sun during this coronal
mass ejection was reflected back up into space rather
than deposited into Earth's lower
atmosphere.
This is because thermal
mass of the oceans is vastly greater
than the
atmosphere.
In an
atmosphere with moving gases, hot air
masses rise and are radiating more strongly
than the gases at the altitude they are moving through.
In that way we can allow factors other
than mass, gravity and insolation to affect V without affecting T because T is determined only by the amount of KE needed to keep the
mass of the
atmosphere off the surface at a given height and in turn that is determined by
mass (m) and the individual gas constant for the particular atmospheric composition (Rspecific).
We need to find an equation that allows factors other
than mass, gravity and insolation to affect V without affecting T because according to the Gas Laws T is determined only by the amount of KE needed to keep the
mass of the
atmosphere off the surface at a given height over and above that required for top of
atmosphere radiative balance.
Even without the above lack of alternatives, the
mass balance still holds: as long as the increase in the
atmosphere is less
than what humans emit, then nature as a whole is a net sink for CO2, doesn't add anything to the total
mass of CO2 in the
atmosphere, even if it circulates 10, 100 or 1,000 times more CO2 over the seasons.
I am giving the control to what has the
mass and has hung onto 40 times more joules
than the
atmosphere.
These reductions are more
than just visual impressions but can dramatically alter the exchanges of
mass, energy, and momentum between the
atmosphere and ocean.
Given the fact that internally the earth itself has large temperature changes which melts the upper mantle and deep crust producing volcanic eruptions at the surface, it is not difficult to see that the thermal energy involved and the
mass of the earth itself, that the earth's own internal temperature fluctuations might have bigger effect on the
atmosphere's temperature
than the sun.
Ideal gas which has no
mass therefore no weight under gravity because there is nothing on which gravity can pull; which has no volume therefore does not expand or condense changing its weight under reduced and increased pressure or heat and cold and so does not become lighter or heavier
than air under gravity; with no attraction therefore merely capable of bouncing off another and not capable of undergoing chemical changes, such as water and carbon dioxide in the
atmosphere forming carbonic acid.
My curiosity is built around the assumption that the warmer air
mass must have transferred heat to the ocean (warmer to colder) and that raises the thought that the
atmosphere would have to get colder
than the ocean for it (the air) to be warmed by the sea.
NCEP / NCAR was demonstrated by Trenberth & Smith in 2005 to be worse
than ERA40 — via the dry
mass of the
atmosphere.
«The total mean
mass of the
atmosphere is 5.1480 × 1018 kg with an annual range due to water vapor of 1.2 or 1.5 × 1015 kg depending on whether surface pressure or water vapor data are used; somewhat smaller
than the previous estimate.
The article attributes a lack of accounting for the heat capacity of the
mass of the
atmosphere to the higher
than expected temperatures.
--- Atmospheric
mass and composition: approx. 510 trillion m ^ 2 (surface area) * 0.1013 MPa (surface pressure) / 9.81 m / s ^ 2 = 5.266 E18 kg = 5.266 million Gt Hartmann, «Global Physical Climatology», p. 8 gives 5.136 million Gt (the difference could be due to actual average surface pressure being lower
than average sea level pressure; counteracting that, gravity decreases with height (not much over most of the
mass of the
atmosphere) and I think global average g may be less
than 9.81 (maybe 9.80?)
BPL: CO2 is well - mixed by turbulence throughout the troposphere and stratosphere, which together account for more
than 99 % of the
mass of the
atmosphere.
I don't know how accurate 510 million km2 is for Earth's surface area; taking 4 * pi * 6371 ^ 2 km2 ~ = 510.064 million km2; but I don't know the formula for an ellipsoid (polar radius is slightly smaller
than equatorial radius)(for what it's worth, 4 * pi * 6381 ^ 2 km2 ~ = 511.667 million km2, which gives a sense of why most of the
mass of the
atmosphere can be approximated as having the same horizontal area as at sea level (a 1 % increase in area is reached at a height of about 31.8 km)-RRB-.
Ray (under comment 16) suggests that burning biomass and sequestering the carbon might be a more benign approach
than pumping
masses of sulphates into the
atmosphere.
The radiating back cools the low -
mass atmosphere far more
than it warms the high -
mass surface.
The
mass of the earth is one trillion, that's 1 followed by 12 zeros, greater
than the
mass of carbon dioxide in the
atmosphere.
The
mass of CO2 in the
atmosphere is much less
than is indicated by the current methods of analysis.