warmed the atmosphere - перевод на испанский
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warmed the atmosphere - перевод на испанский

VERY SCANT PRESENCE OF GASES SURROUNDING THE MOON
Atmosphere of the moon; Lunar atmosphere; Lunar exosphere; Lunar Atmostphere; The moon’s atmosphere; Moon’s atmosphere
  •  access-date=Aug 8, 2022}}</ref>.

warmed the atmosphere      
Avivó la atmosfera (consiguió que la atmósfera sea alegre)
air         
  • An idealised view of three pairs of large circulation cells.
  • Composition of Earth's atmosphere by molecular count, excluding water vapor. Lower pie represents trace gases that together compose about 0.0434% of the atmosphere (0.0442% at August 2021 concentrations<ref name="CO2" /><ref name="methane" />). Numbers are mainly from 2000, with {{CO2}} and methane from 2019, and do not represent any single source.<ref name="handbook" />
  • standard atmosphere]] model (the eight dotted lines in each "decade" are at the eight cubes 8, 27, 64, ..., 729)
  • access-date=2014-06-10}}</ref>
  • Rough plot of Earth's atmospheric [[transmittance]] (or opacity) to various wavelengths of electromagnetic radiation, including [[visible light]].
  • Earth's atmosphere. Lower four layers of the atmosphere in three dimensions as seen diagonally from above the exobase.  Layers drawn to scale, objects within the layers are not to scale. Aurorae shown here at the bottom of the thermosphere can actually form at any altitude in this atmospheric layer.
  • [[Afterglow]] of the [[troposphere]] (orange), the [[stratosphere]] (blue) and the mesosphere (dark) at which [[atmospheric entry]] begins, leaving smoke trails, such as in this case of a [[spacecraft]] reentry.
  • year=2016 }}</ref><ref>[https://www.nap.edu/openbook/0309100615/gifmid/30.gif Graph: Atmospheric Oxygen and CO2 vs Time]</ref>
  • Animation shows the buildup of tropospheric {{CO2}} in the Northern Hemisphere with a maximum around May. The maximum in the vegetation cycle follows in the late summer. Following the peak in vegetation, the drawdown of atmospheric {{CO2}} due to photosynthesis is apparent, particularly over the [[boreal forests]].
GAS LAYER SURROUNDING EARTH
Earth atmosphere; Atmospheric stratification; Earth’s atmosphere; Early atmosphere; Air; Atmospheric layers; Atmospheric Layers; Upper-atmosphere dynamics; Atmospheric gases; Atmospheric gasses; Air (mixture of gases); Composition of the earths atmosphere; Atmospheric gas; Standard Dry Air; Terran Atmosphere; Earths atmosphere; Earth's Atmosphere; Atmosphere of the earth; Layers of the atmosphere; Layers of Earth's atmosphere; Atmospheric Gas; Earth's atmosphere; Refractive index of air; Atmospheric layer; Air qualities; Qualities of air; Material properties of air; Air (properties); Third atmosphere; Atmospheric air; Evolution of Earth's atmosphere; Atmosphere of earth; Atmosphere of early Earth; Terrestrial atmosphere; Terran atmosphere; Atmosphere of the Earth
el aire
air         
  • An idealised view of three pairs of large circulation cells.
  • Composition of Earth's atmosphere by molecular count, excluding water vapor. Lower pie represents trace gases that together compose about 0.0434% of the atmosphere (0.0442% at August 2021 concentrations<ref name="CO2" /><ref name="methane" />). Numbers are mainly from 2000, with {{CO2}} and methane from 2019, and do not represent any single source.<ref name="handbook" />
  • standard atmosphere]] model (the eight dotted lines in each "decade" are at the eight cubes 8, 27, 64, ..., 729)
  • access-date=2014-06-10}}</ref>
  • Rough plot of Earth's atmospheric [[transmittance]] (or opacity) to various wavelengths of electromagnetic radiation, including [[visible light]].
  • Earth's atmosphere. Lower four layers of the atmosphere in three dimensions as seen diagonally from above the exobase.  Layers drawn to scale, objects within the layers are not to scale. Aurorae shown here at the bottom of the thermosphere can actually form at any altitude in this atmospheric layer.
  • [[Afterglow]] of the [[troposphere]] (orange), the [[stratosphere]] (blue) and the mesosphere (dark) at which [[atmospheric entry]] begins, leaving smoke trails, such as in this case of a [[spacecraft]] reentry.
  • year=2016 }}</ref><ref>[https://www.nap.edu/openbook/0309100615/gifmid/30.gif Graph: Atmospheric Oxygen and CO2 vs Time]</ref>
  • Animation shows the buildup of tropospheric {{CO2}} in the Northern Hemisphere with a maximum around May. The maximum in the vegetation cycle follows in the late summer. Following the peak in vegetation, the drawdown of atmospheric {{CO2}} due to photosynthesis is apparent, particularly over the [[boreal forests]].
GAS LAYER SURROUNDING EARTH
Earth atmosphere; Atmospheric stratification; Earth’s atmosphere; Early atmosphere; Air; Atmospheric layers; Atmospheric Layers; Upper-atmosphere dynamics; Atmospheric gases; Atmospheric gasses; Air (mixture of gases); Composition of the earths atmosphere; Atmospheric gas; Standard Dry Air; Terran Atmosphere; Earths atmosphere; Earth's Atmosphere; Atmosphere of the earth; Layers of the atmosphere; Layers of Earth's atmosphere; Atmospheric Gas; Earth's atmosphere; Refractive index of air; Atmospheric layer; Air qualities; Qualities of air; Material properties of air; Air (properties); Third atmosphere; Atmospheric air; Evolution of Earth's atmosphere; Atmosphere of earth; Atmosphere of early Earth; Terrestrial atmosphere; Terran atmosphere; Atmosphere of the Earth
aire
tonada
ventilar
airear
to put on airs: darse tono

Определение

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Википедия

Atmosphere of the Moon

The atmosphere of the Moon is a very scant presence of gases surrounding the Moon. For most practical purposes, the Moon is considered to be surrounded by vacuum. The elevated presence of atomic and molecular particles in its vicinity compared to interplanetary medium, referred to as "lunar atmosphere" for scientific objectives, is negligible in comparison with the gaseous envelopes surrounding Earth and most planets of the Solar System. The pressure of this small mass is around 3×10−15 atm (0.3 nPa), varying throughout the day, and in total mass less than 10 metric tonnes. Otherwise, the Moon is considered not to have an atmosphere because it cannot absorb measurable quantities of radiation, does not appear layered or self-circulating, and requires constant replenishment due to the high rate at which its gases get lost into space.

Roger Joseph Boscovich was the first modern astronomer to argue for the lack of atmosphere around the Moon in his De lunae atmosphaera (1753).