Sentences with phrase «through top of atmosphere»

Did it go back out into space through the top of the atmosphere?

If there were too much UV light, no water could survive on the surface because the water molecules would break up and escape through the top of the atmosphere as hydrogen and oxygen gas.

Acting as a safety valve of sorts, this response creates a negative radiative feedback that allows more of the accumulating heat to be released into space through the top of the atmosphere.

Not exact matches

While your friends lose control of their drones, you'll still be speeding through the atmosphere, coming out on top for stamina and persistence.

Two recent models for the formation of the Moon, one that allows exchange through a silicate atmosphere (top), and another that creates a more thoroughly mixed sphere of a supercritical fluid (bottom), lead to different predictions for potassium isotope ratios in lunar and terrestrial rocks (right).

A proton with energy of 100 GeV interact at the top of the atmosphere and produces a cascade of secondary particles who ionize molecules when traveling through the air.

Refraction severely flattens the top of the sun, but its light is brighter because of a shorter trip through the atmosphere.

Namely these factors are CAPE, which is Convective Available Potential Energy, which is the maximum amount of energy that a rising parcel (which [is] an arbitrary amount of mass) can have as it's rising through the atmosphere; wind shear, which is the difference in wind [vectors] at the top and bottom of the atmosphere; and specific humidity, which is the ratio of water to the total mass of a moist system.

To explain the discrepancy, Tamara Goldin of the University of Vienna and Jay Melosh of Purdue University in Indiana studied how ejecta falling through the atmosphere might affect heat transfer from the top of the atmosphere to the ground.

Surfing complete21 February 2018 Slowed by skimming through the very top of the upper atmosphere, ESA's ExoMars has lowered itself into a planet - hugging orbit and is about ready to begin sniffing the Red Planet for methane.

The Trace Gas Orbiter has reached its final orbit after a year of «aerobraking» that ended in February.This exciting operation saw the craft skimming through the very top of the upper atmosphere, using drag on its solar wings to transform its initial highly elliptical four - day orbit of about 200 x 98 000 km into the final, much lower and near - circular path at about 400 km.

For the last few months, Cassini has been looping through Saturn's inner ring system and sampling the top of the planet's atmosphere, which is «like dipping our toe in Saturn's atmosphere, in preparation for the final plunge,» Spilker said during the news briefing.

Despite the flat - out sprints, the drag racing, the donuts, the top - speed runs, and dicing through traffic like there's a jet pack strapped to the trunk, Pacific Gas and Electric — which generated power for the Tesla — released into the atmosphere the same amount of carbon dioxide as would a gasoline - powered car getting 99 mpg.

The high characteristic roof construction and the huge window frame with a view over the park / through to the ocean determine the atmosphere of the Top Room (42 m2).

What Lee has accomplished with single lines transforms inanimate, everyday inks into vibrant fields of color with trailing edges that sway through a luminous atmosphere, seemingly with no top or bottom.

What happens at the «top of atmosphere» — the level where outgoing radiation leaves for space, not itself a very easy concept — is the restoration of equilibrium, the increase in temperature that, through Helmholtz - Boltzmann at the Earth's brightness temperature 255K, restores the balance between incoming and outgoing energies.

The outgoing longwave radiation is composed not just of the radiation that leaks through to the top from the warm lower layers, but also of the «cold» radiation emitted from the upper atmosphere.

Here on Earth, from the base of the crust upwards, the mix of elements as elements or compounds, up through to the top of the atmosphere are not at chemical equilibrium.

Now if you were an Astrophysicist that has never really don't anything productive in the real world, you would consider that the top of the atmosphere emissivity of 0.69 and that 5.35 is the correct multiplier for the surface because through your Web Hubble Telescope all you can see is albedo and emissivity which has to equal absorption.

In attempting to substantiate this internal variability hypothesis, Spencer & Braswell (2011) assumed that the change in top of the atmosphere (TOA) energy flux due to cloud cover changes from 2000 to 2010 was twice as large as the heating of the climate system through ocean circulation.

There is no net loss of energy as one goes up through an atmosphere because a molecule at the surface has the same total energy as a molecule at the top of an atmosphere.

We've also been through a deep solar minimum and in early 2009 also announced the lowest value ever measured for the top of the atmosphere.

Once the appropriate planetary temperature increase has been set by the delay in transmission through the atmosphere then equilibrium is restored between radiant energy in and radiant energy out at the top of the atmosphere.

On top of a very polluting and extraction process (especially if happening through hydraulic fracturing) the the phenomenon of methane leakage make so that over a period of twenty years, methane is eighty times more pollutant for the atmosphere and the climate than CO2.

The average global temperature is then given by the total Outgoing Long Wave radiation (OLR) at the top of the atmosphere through stefan bolltzman's law = e * sigmaTeff ** 4.

Spencer & Braswell (2011) assumed that the change in top of the atmosphere (TOA) energy flux due to cloud cover changes from 2000 to 2010 was twice as large as the heating of the climate system through ocean circulation.

An atmosphere that is perfectly transparent to incoming and outgoing radiation can not radiate and all its heat content comes from conduction from the surface and is transported through the atmosphere solely by convection with no loss of energy to space except for the tiny fraction of atoms at the top of the atmosphere that exceed escape velocity.

The first is the original «invisible something barrier» at the top of the atmosphere, TOA, like the glass of a greenhouse, preventing the longwave infrared from the Sun from entering, but allowing the mainly visible light to reach the surface and directly heat it and the second is that the Sun produces insignificant amounts of longwave infrared and none of this gets through TOA.

But in a given model you can often find ways of altering the model's climate sensitivity through the sub-grid convection and cloud schemes that affect cloud feedback, but you have to tread carefully because the cloud simulation exerts a powerful control on the atmospheric circulation, top - of - atmosphere (TOA) and surface radiative flux patterns, the tropical precipitation distribution, etc..

MIT's Sallie «Penny» Chisholm, one of the world's top biological oceanographers, finds the idea of geo - engineering the earth's atmosphere through oceanic iron fertilization to be anathema.

So, we then have the solar input passing straight through yet a further 33 being recycled up and down through the atmosphere which gives a warmer surface but no change in top of atmosphere energy balance.

The emissivity and absorptivity of the ocean are set to 1, there are no ocean currents, the atmosphere doesn't heat up and cool down with the ocean surface, the solar radiation value doesn't change through the year, the top layer was 5 mm not 1μm, the cooler skin layer was not modeled, a number of isothermal layers is unphysical compared with the real ocean of continuously varying temperatures..

As I understand it, this is the total solar radiation passing through a square metre facing the sun at the top of the Earth's atmosphere.

He sent infrared radiation through a tube filled with carbon dioxide, containing somewhat less gas in total then would be found in a column of air reaching to the top of the atmosphere.

The surface temperature basically ends up being determined by the top - of - the - atmosphere energy budget plus the lapse rate that is basically constrained come through convection, evaporation / condensation, etc..

Hence, the easiest way to figure out what is going to happen to the surface temperature is actually to look at the energy budget at the top of the atmosphere (where we know the only energy transfers are via radiation) and then to incorporate convection and latent heat transfer essentially through understanding the constraints that they set on the lapse rate.

We define the TOA (top of atmosphere) to be where optical thickness, τ = 0, and it increases through the atmosphere to reach a maximum of τ = τA at the surface.

The forcing aspect of the indirect effect at the top of the atmosphere is discussed in Chapter 2, while the processes that involve feedbacks or interactions, like the «cloud lifetime effect» [6], the «semi-direct effect» and aerosol impacts on the large - scale circulation, convection, the biosphere through nutrient supply and the carbon cycle, are discussed here.

Real world says that the energy received on top of the atmosphere incomes through the atmosphere and is attenuated by the atmosphere from the average of 1368 W / m ^ 2 down to the average of 342 W / m ^ 2.

The solid red area is what actually gets through the Atmosphere to the surface, which includes cloud - tops and the white roof of Energy Secretary Chu's home.

The average geothermal heat flow through the earth's crust is roughly 0.1 W / m ²; the average annual solar radiation arriving at the top of the Earth's atmosphere is roughly 1365 W / m ².

With this, AGW says that the energy emitted by the Sun is attenuated through the space between the Earth and the Sun from 9.66 x 10 ^ 25 W to 342 W / m ^ 2, on the very top of the Earth's atmosphere.

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