Приклади вживання The martian atmosphere Англійська мовою та їх переклад на Українською
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The Martian atmosphere.
Determine the ratio of stable isotopes in the Martian atmosphere.
Where did the Martian atmosphere go?
Curiosity also hasconfirmed sharp seasonal increases of methane in the Martian atmosphere.
The Martian atmosphere behaves as one.
The martian atmosphere is extremely thin.
The Martian atmosphere was stripped by solar wind.
Planting unit weight of385 pounds was preceded by deceleration in the Martian atmosphere, which began at a distance of about 125 kilometers from the planet's surface.
The Martian atmosphere is protected from the solar wind.
Scientists describe the discovery of seasonal variations in methane in the Martian atmosphere over the course of nearly three Mars years, which is almost six Earth years.
Then the Martian atmosphere was dissipated by the solar wind.
Scientists described the discovery of seasonal variations in methane in the Martian atmosphere over the course of nearly three Mars years, which is almost six Earth years.
The Martian atmosphere is made up of 96 percent carbon dioxide gas molecules.
It was found that therewas seasonal variations in methane levels in the Martian atmosphere over the course of almost three Martian years, which equates to close to six Earth years.
The Martian atmosphere is thin relative to Earth's and with much lower atmospheric pressure.
Slow down about the Martian atmosphere TGO will be about a year.
The Martian atmosphere is cold and sparse, resembling those of the earth at high altitudes.
Methane is suspected to be stable in the Martian atmosphere for only about 300 years, so whatever is generating this gas did so recently.
Observations of the Martian atmosphere over the next few months will test whether the forecast is correct.
It is assumed that methane is stable in the Martian atmosphere is only 300 years old, but who or what could generate this gas so long ago- remains a mystery.
It is assumed that methane is stable in the Martian atmosphere is only 300 years old, but who or what could generate this gas so long ago- remains a mystery.
To Lovelock, the stark contrast between the Martian atmosphere and chemically-dynamic mixture of that of our Earth's biosphere was strongly indicative of the absence of life on the planet.