THE solar wind is a hurricane of charged particles that blows from the Sun's
outer atmosphere into deep space at a million miles per hour.
Near the end of its life, a huge star blasts much of its bloated
outer atmosphere into space — a torrent of gas equal to Earth's mass each year, racing outward at 10 million kilometers per hour.
Not exact matches
On Earth, the brightest auroras (the high - altitude glows often called the northern and southern lights) are generated when electrons in
outer space near Earth are accelerated by large electrical potentials, or voltages, along the lines in our planet's magnetic field and slam
into gas molecules in the upper
atmosphere above polar regions.
The release of CO2
into the
atmosphere contributes to the trapping of heat that would otherwise be emitted
into outer space.
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.
Most of the gas cascades back onto the sun, but a small fraction may escape
into the
outer atmosphere to feed the solar wind — a steady stream of particles that blows far
into space.
Waves in the jet then transport material and energy
into the
outer atmosphere of the Sun and the wider Solar System.
Scientists suspect water on the surface of Mars evaporates, rises
into the upper
atmosphere, breaks
into hydrogen and oxygen atoms, and is then swept
into outer space by the solar wind.
The
outer layers of the star — the stellar «
atmosphere» — absorb this excess and swell outward
into the characteristic distended figure of a red giant.
About every five minutes, spicules shoot red hot streams of charged particles
into the corona, the
outer layer of the solar
atmosphere, at around 150 kilometres per second.
If the energy delivered to Earth by the Sun or by impacts (or both) were 40 % greater, the Earth would experience a runaway greenhouse.3 That is, more water would evaporate from Earth's surface, so too much heat trying to escape
into outer space would be blocked by water vapor in the
atmosphere.
In particular, both olive oil and oleic acid have been shown to increase trans - epidermal water loss (TEWL), which in scientific terms is the quantity of water that passes through the
outer epidermis
into the
atmosphere.
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.
About 30 percent of the sunlight that beams toward Earth is deflected by the
outer atmosphere and scattered back
into space.
The exosphere, the highest layer, is extremely thin and is where the
atmosphere merges
into outer space.
Air warmed at the surface naturally tends to rise above the majority of the (blocking)
atmosphere and it can not descend until it has cooled by the emission of IR
into the cool of
outer space.
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.
The evidence here comes from satellite measurements of infrared radiation escaping from the earth
into outer space, from measurements of sunlight reflected from clouds and from measurements of the temperature the earth's surface or of the troposphere, the roughly 10 km thick layer of the
atmosphere above the earth's surface that is filled with churning air and clouds, heated from below at the earth's surface, and cooled at the top by radiation
into space.
It means how HIGH up in the
atmosphere heat radiation occurs
into outer space.