Not exact matches
Forming in the system's colder
outer regions, where volatile compounds such
as water and carbon dioxide freeze out, makes it possible that the planets incorporated those ices and carried them along to a warmer place where they could melt, evaporate, and become oceans and
atmospheres.
Scientists believe that these ions, which the SELENE spacecraft (better known
as Kaguya) detected, drifted over geologic time from the
outer layers of Earth's
atmosphere and became embedded in the moon's regolith, a loose top layer of soil and rock.
Hess concluded that a powerful radiation originates in
outer space and enters the Earth's
atmosphere, diminishing in intensity
as it passes through the air.
The radiation belts are two donut - shaped regions of highly energetic particles trapped in the Earth's magnetic field — the inner, located just above our
atmosphere and extending 4,000 miles into space; and the
outer, from 8,000 to 26,000 miles out — and are named for their discoverer (
as are the probes), the late James A. Van Allen of the University of Iowa.
As the Lynx approaches the
outer atmosphere, the rocket engines will be shut down and the pilot and passenger will feel weightless until they begin their 20 - minute descent.
As the exoplanet passes in front of its host star, as seen from Earth, some of this starlight travels through the planet's outer atmospher
As the exoplanet passes in front of its host star,
as seen from Earth, some of this starlight travels through the planet's outer atmospher
as seen from Earth, some of this starlight travels through the planet's
outer atmosphere.
As it passes through the
outer atmosphere, friction will slow the vehicle to below the speed of sound in less than two minutes.
As the companion enters the bloated star's
outer atmosphere, it gobbles up material.
Adaptive optics have proved so successful that the
atmosphere «no longer limits our resolution,» Ghez says — that is, the telescopes can see just
as well
as they could if they were in
outer space.
One of three main
outer layers that make up the sun's
atmosphere, the chromosphere often appears red
as superheated hydrogen emits light.
As the bloated star ages, this extended
outer atmosphere cools and contracts, then soaks up more energy from the star and again puffs out: with each successive cycle of expansion and contraction the
atmosphere puffs out a little farther.
It's sort of hard to define exactly where the
atmosphere ends and
outer space begins (since the
atmosphere gradually falls off
as you go up in altitude), but one popular choice is the so - called «Karman line» at a height of 100 km (or around 62 miles) above sea level.
Called «NASA's Leadership and America's Future in Space,» the report said that studying the
outer gas giant planets (such
as Saturn) help scientists learn about their
atmospheres and internal structure.
I'm still holding out for the news that reads: «Second Earth Found» -[this exoplanet] will have all the right ingredients: orbit its star inside the habitable zone, spectroscopic analysis will reveal a nitrogen - rich
atmosphere, evidence of water, roughly the same mass
as our planet and it will belong in a system with a couple of gas giants shepherding the
outer system.
«The composition and chemistry of ice giant
atmospheres provides clues about their formation, evolution and current state,» explained a research paper referenced
as part of NASA's
Outer Planets Assessment Group Meeting in Laurel, Maryland.
X-rays are emitted from a star's corona — the «
outer atmosphere» of a stellar body that forms
as the result of complex interactions between a stellar body's magnetic fields and its turbulent
outer layer.
The moss observations are thus helping to locate the
as yet elusive energy source that is responsible for heating the Sun's
outer atmosphere.
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.
The
outer boundary is defined by the «maximum greenhouse limit,» where the greenhouse effect fails
as CO2 begins to condense out of the
atmosphere and the surface becomes too cold for liquid water.
On Jan. 14, 2005, the Huygens entry probe became the first spacecraft to land on a planetary surface in the
outer solar system, carrying out various physical and chemical measurements of Titan's
atmosphere and transmitting high - resolution images
as it descended by parachute.
We know that the magnetosphere is filled with plasma from solar wind but for more than two decades it has been theorised that the innermost part of the Earth's magnetosphere — a region centred around the Earth's equator and surrounding our planet's
atmosphere known
as the plasmasphere — also plays a vital role in replenishing the
outer magnetosphere with fresh plasma.
As a now - frequent vacationer in the
Outer Banks, I wanted to give readers a taste of this relaxing
atmosphere, but from the point of view of a family that calls the coast home.
I have seen a statement that the
outer edge of the earth's
atmosphere receives approximately 14,000 x
as much energy in solar radiation
as we currently generate from fossil fuels.
The premise of Lindzen's hypothesis was that
as the climate warms, the area in the
atmosphere covered by high cirrus clouds will contract to allow more heat to escape into
outer space, similar to the iris in a human eye contracting to allow less light to pass through the pupil in a brightly lit environment.
But that's actually an understatement by Gallup, since more than 97 % of the world's climatologists say that those carbon gases, which are given off by humans» burning of carbon - based fuels, are causing this planet's temperatures to rise over the long term,
as those carbon gases accumulate in the
atmosphere and also block the heat from being radiated back into
outer space.
Greenhouse gases such
as carbon dioxide accumulate in the
atmosphere and trap heat that normally would exit into
outer space.
The ModTran tool provides a direct indication of total energy radiated to
outer space (or to some high altitude receptor)
as a function of the
atmosphere, weather conditions, and temperature offset that you select.
If CO2 and H2O molecules now are cooled below the previous equilibrium point by having their radiation allowed to escape to
outer space, then I believe these molecules must then tend to absorb more energy than yield energy with each interaction with the other components of the
atmosphere until that
atmosphere as a whole reaches a new thermal equilibrium where the net radiation going out and the net radiation coming in (primarily from the sun and the surrounding
atmosphere) is the same.
(1) The UF6 gas at the
outer rim of a gas centrifuge is at many
atmospheres of pressure and room temperature (or optionally a little warmer,
as supplied by a heating coil), per these pictures of an operating centrifuge cascade.
Additionally, while nearly 80 percent of the sunlight reflected from a roof can escape to
outer space, the «thermal infrared» energy radiated by a hot, dark roof is trapped by greenhouse gases, such
as CO2 and water vapor, warming the
atmosphere.
Greenhouse Effect
As sunlight enters the Earth's
atmosphere, some of the radiation from the sun is reflected back into
outer space But, some of that radiation.
I think you are actually saying the same thing
as Joel is: the only way that energy can actually move from the
atmosphere to
outer space is through radiation.
So, the
atmosphere acts to cool the surface by absorbing and reradiating energy from the Sun, with the attendant losses,
as energy is converted from one form to another, and some escapes
as waste to
outer space.
The key to this understanding are the concepts of a «torque» and the of natural power of «swirling vortices»
as these phenomena that relate to the role of the
atmosphere, the oceans, the Earth's «molten
outer core,» and formation of Earth's magnetic field on climate change.