We suspect that water, the constituent of Saturn's deepest cloud deck, can suppress convection in
the lighter hydrogen atmosphere for a period of decades, until finally buoyancy wins out and a large convective outburst ensues.
Not exact matches
Heaven is that planet 35000
light - years from earth, ten times as big made of
hydrogen and oxygen for water, gold as
atmosphere (yes we're taking the gold) But to desist as soul when given the chance in hell if you truly believe seems impassible for me to fathom.
For instance, if the earth were slightly larger,
hydrogen, a
light gas, could not escape into the
atmosphere at its prescribed rate (due to an increase in the earth's gravitational field), and over time would build up and cause life to cease.
If the earth were slightly larger, having a stronger gravitational force, it would prevent
hydrogen, a
light gas, from escaping at a specified rate, building up in our
atmosphere and eventually rendering our planet lifeless.
As expected, scientists observed
light, charged particles like
hydrogen and helium ions leaving Venus's
atmosphere.
At altitudes above 50 kilometers, ultraviolet
light from the sun easily penetrates the Red Planet's thin
atmosphere and breaks down water's chemical bonds between
hydrogen and oxygen.
Essentially composed of
hydrogen, it absorbs the ultra violet
light emitted by the star and the phenomenon remains invisible on Earth because the ultra violet
light is blocked by the
atmosphere.
Huygens will sample methane in the
atmosphere and measure the relative abundance of
light hydrogen and heavy
hydrogen to produce a chemical fingerprint that will enable scientists to compare Titan's composition with that of comets.
«While we expected to see some red in Saturn's aurora because
hydrogen emits some red
light when it gets excited, we also knew there could be color variations depending on the energies of the charged particles bombarding the
atmosphere and the density of the
atmosphere,» Dyudina said.
Such physical changes to the
atmosphere might last only hours or days, he notes, but any subtle chemical changes — including those resulting from the extra
hydrogen added to the air when ultraviolet
light breaks down the water vapor — would persist much longer.
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.
The favoured idea is that water is responsible, but some argue that
hydrogen peroxide and ozone, which might be created when ultraviolet
light breaks down the carbon dioxide and oxygen in the Martian
atmosphere, could be involved.
Phase V
hydrogen, created by crushing Earth's
lightest element with mind - boggling pressures, gives the physicists a glimpse of the inner
atmosphere of a gas giant, where pressures reach millions of (Earth)
atmospheres
The storms can vault water vapor up to 80 kilometers into the planet's
atmosphere, where ultraviolet
light breaks down the vapor into
hydrogen and oxygen.
Smaller planets like ours have lost the
light elements in their
atmospheres, such as
hydrogen and helium, but the greater gravity of 55 Cancri e has held onto them.
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 particles journeyed around Earth, the
lighter hydrogen particles were lost in collisions with the
atmosphere, leaving an oxygen - rich plasma.
With too much UV
light, no water could persist on the surface because its molecules would break down into
hydrogen and oxygen gas and escape through the
atmosphere.
Since the
lighter version escapes more often, over time, the Martian
atmosphere has less and less
hydrogen compared to the amount of deuterium remaining.
C. Carreau, ASPERA - 4 & MAG teams, Venus Express, ESA Annotated image illustrating loss of
hydrogen through plasma wake Venus may have lost oceans of water due to a runaway greenhouse effect which evaporated water into the upper
atmosphere, where ultraviolet
light dissociated water into ionized atomic
hydrogen and oxygen (some later incorporated into carbon dioxide) that were blown away by the Solar wind due to the lack of a strong magnetic field like the Earth's (more).
The results quantify the nature of gas molecules containing carbon,
hydrogen, and sulfur in the earliest
atmosphere, but they shed no
light on the much later rise of free oxygen in the air.
It says nothing about CO2 ′ s greenhouse effect because it reports the upper
atmosphere absorbing high velocity helium and
hydrogen and other particles, not infra - red
light.
Once this happens, it is easy for the water vapor to decompose in the upper
atmosphere, whereafter the
light hydrogen escapes and oxygen either escapes or reacts with rocks.
When water molecules rise high in an
atmosphere, ultraviolet radiation split the water molecules into its component gases, oxygen and
hydrogen, and the
lighter hydrogen molecules escape into space.