Any additional heat in the atmosphere, therefore, will tend to radiate out into space (an infinite heat - sink) or into the oceans (which, being 1000 times
denser than the atmosphere and having an enormous volume, are a near - infinite heat - sink).
Not exact matches
Although the gas is at a chilly minus 63 degrees Fahrenheit (minus 53 degrees Celsius) and is 300 trillion times less
dense than Earth's
atmosphere, it's still five times hotter and 10 to 100 times
denser than what's typical in galaxies like the Milky Way.
Titan's
atmosphere is far
denser than Earth's, its gravity just one - seventh as strong, and its average temperature a chilly — 289 degrees Fahrenheit.
So another model, proposed in 2015, assumes the impact was extremely violent, so violent that the impactor and Earth's mantle vaporized and mixed together to form a
dense melt / vapor mantle
atmosphere that expanded to fill a space more
than 500 times bigger
than today's Earth.
Akatsuki's 2 - year mission aims to peel away some of the mystery of Venus's
dense, cloudy
atmosphere, which sweeps over the planet at speeds exceeding 300 kilometers per hour, or 60 times faster
than Venus itself rotates.
At another extreme, Saturn's giant moon Titan seems more like a planet in its own right, larger
than Mercury and cloaked in a
dense atmosphere.
Microclimate is the climate near the ground which can be colder or warmer
than in the free
atmosphere, depending on local topography (e.g. north vs. south side of a hill, higher vs. lower elevation) and vegetation (e.g. young sparse vs. old
dense forest).
Using diamond anvil cells (DAC), the team applied 2.5 GPa of pressure (25 thousand
atmospheres) to pre-compress water into the room - temperature ice VII, a cubic crystalline form that is different from «ice - cube» hexagonal ice, in addition to being 60 percent
denser than water at ambient pressure and temperature.
Using climate models at the Laboratoire de Météorologie Dynamique, François Forget (CNRS) and Martin Turbet (UPMC) show that, with a cold climate and an
atmosphere denser than it is today, ice accumulated at around latitude 25 ° S, in regions corresponding to the sources of now dry river beds.
And while Martian winds can kick up sky - blotting dust storms like those that plagued the Spirit and Opportunity rovers this summer, the
atmosphere of Mars is 100 times less
dense than that of Earth.
Although the difference in altitude doesn't sound much, the differences between the inner and outer
atmosphere are actually quite pronounced, with the
atmosphere 10 times
denser at 125 km
than it is as 150 km.
Upon your arrival to the second planet from the sun, you'd be greeted by surface temperatures comparable to those in a pizza oven, and a carbon - dioxide
atmosphere more
than 90 times
denser than ours here on Earth.
TRAPPIST - 1b, the innermost planet, and TRAPPIST - 1c likely have rocky interiors and
atmospheres denser than Earth's, according to the study.
Coronal holes are gaps in the Sun's outermost
atmosphere which are less
dense and cooler
than their surroundings.
This orbits places the planet near the inner edge of its host star's habitable zone, where liquid water could exist in liquid form under favorable conditions such as an albedo of 0.52 with an orbital eccentricity of 0.11 and more
than 52 percent cloud cover under a sufficiently
dense atmosphere of water, carbon dioxide, and molecular nitrogen like Earth's (ESO science release; Pepe et al, 2011; and Kaltenegger et al, 2011 — more below).
Venus has a much higher albedo (reflectivity)
than Earth because of its thick cloud cover (and would even have a high albedo without the clouds due to Rayleigh scattering from the
dense CO2
atmosphere).
simply put — planets with thick (
denser)
atmospheres are warmer
than ones with thinner
atmospheres — independent of the constituent gases in the
atmosphere!
While partially deforested areas exhibited a less unstable
atmosphere than the neighbouring
dense forest, the team found that shallow clouds formed over them.
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 very
dense so the surface is much hotter
than it otherwise would be.
Their model was based on the observation that in the troposphere (the lower and
denser layer of the
atmosphere, with pressures greater
than 0.2 atm) the heat transfer is mostly by convection and the temperature distribution is close to adiabatic.
In the heavier
denser liquid water of the ocean transit is slowed down even further, some fourteen times more
than in our
atmosphere, as water being a transparent medium for visible light transmits it through unchanged but delays it in each encounter as it tries to absorb it but can't.
Mars: thin
atmosphere (albeit composed of 95 % CO2)-- > no «greenhouse effect» Earth:
denser atmosphere — > some real «atmospheric effect» Venus: 95x
denser atmosphere than on Earth — > powerful «atmospheric effect» No
atmosphere — no «greenhouse effect»
At low altitude and high temperatures (greater
than 30 °C or 86 °F), over the ocean, it can reach 4.3 % or more of the
atmosphere and is less
dense than dry air, causing it to rise.
And so today we have a carbon dioxide
atmosphere on Venus which is 92 times more
dense than Earth's
atmosphere at the surface.
Factor in the fact that soils amd water are at least ~ 1000 times more
dense than air and the idea that gases can heat warmer surfaces like soils and especially water whilst most of the
atmosphere is actually much colder just seems - well — ludicrous.
It is lucky that it is
denser than air, if not then all the methane generated near the surface of the terrasphere would whisk its way off into the
atmosphere.
All that is needed is to add heat carried upwards past the
denser atmosphere (and most CO2) by convection and the latent heat from water changing state (the majority of heat transport to the tropopause), the albedo effects of clouds, the inability of long wave «downwelling» (the blue balls) to warm water that makes up 2 / 3rds of the Earth's surface, and that due to huge differences in enthalpy dry air takes far less energy to warm
than humid air so temperature is not a measure of atmospheric heat content.
So isn't the whole issue really revolving around how
dense the
atmosphere is at any given time and has
atmosphere during the latest warm spell been
denser than say in the 1970s during that cold spell?
There is clearly a lot of
atmosphere above the effective radiating height albeit much less
dense than the troposphere.
However, if we add the solar wind and moon slow stipping of the
atmosphere, which show that
atmosphere must have been
denser in the past
than now, a simpler and more logical explaination, that the giant flying critters could fly due to the
denser atmosphere then extant, is warrented.
This, plus some stripping away from the gravitational effects of the moon, strongly suggests that the
atmosphere formerly used to be
denser than it is now.
Bionic leaves that could produce energy -
dense fuels from nothing more
than sunlight, water and
atmosphere - warming carbon dioxide, with no byproducts other
than oxygen, represent an ideal alternative to fossil fuels but also pose numerous scientific challenges.
This means that it takes longer for it to lose that heat (cool)
than the less
dense atmosphere at higher altitudes.