The combined absorption spectra of the gases in the atmosphere leave "windows" of low opacity, allowing the transmission of only certain bands of light. The optical window runs from around 300nm ( ultraviolet-C) up into the range humans can see, the visible spectrum (commonly called light), at roughly 400–700nm and continues to the infrared to around 1100nm. There are also infrared and radio windows that transmit some infrared and radio waves at longer wavelengths. For example, the radio window runs from about one centimetre to about eleven-metre waves. Since I also have the original "The Earth From The Air", which has the same author and features many of the same photos, I will also be comparing these two books with each other. The exosphere is too far above Earth for meteorological phenomena to be possible. However, Earth's auroras—the aurora borealis (northern lights) and aurora australis (southern lights)—sometimes occur in the lower part of the exosphere, where they overlap into the thermosphere. The exosphere contains many of the artificial satellites that orbit Earth.

from the air Aerial View - Views from the air

Cox, Arthur N., ed. (2000), Allen's Astrophysical Quantities (Fourthed.), AIP Press, pp.258–259, ISBN 0-387-98746-0 , which rounds N 2 and O 2 to four significant digits without affecting the total because 0.004% was removed from N 2 and added to O 2. It includes 20 constituents. If the entire mass of the atmosphere had a uniform density equal to sea level density (about 1.2kg per m 3) from sea level upwards, it would terminate abruptly at an altitude of 8.50km (27,900ft). this is a tremendous and inspirential awe inspiring exhibition.Well worth a visit and best of all it was accessable ad free of charge. You must see it. This layer is completely cloudless and free of water vapor. However, non-hydrometeorological phenomena such as the aurora borealis and aurora australis are occasionally seen in the thermosphere. The International Space Station orbits in this layer, between 350 and 420km (220 and 260mi). It is this layer where many of the satellites orbiting the Earth are present.

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Temperatures drop with increasing altitude to the mesopause that marks the top of this middle layer of the atmosphere. It is the coldest place on Earth and has an average temperature around −85 °C (−120 °F; 190 K). [26] [27]

Earth from the Air - 365 Days: (expanded edition ) The Earth from the Air - 365 Days: (expanded edition )

Journal of the Atmospheric Sciences (1993). "stratopause". Archived from the original on 2013-10-19 . Retrieved 2013-10-18. There is a big chance that your city can be viewed, just insert a name of a city or a place and try aerial view! Exosphere - overview". UCAR. 2011. Archived from the original on 17 May 2017 . Retrieved April 19, 2015.For combustion to occur, there needs to be a fuel, heat and oxygen. This is represented by the fire triangle . As of 2023, by mole fraction (i.e., by number of molecules), dry air contains 78.08% nitrogen, 20.95% oxygen, 0.93% argon, 0.04% carbon dioxide, and small amounts of other gases. [8] Air also contains a variable amount of water vapor, on average around 1% at sea level, and 0.4% over the entire atmosphere. Air composition, temperature, and atmospheric pressure vary with altitude. Within the atmosphere, air suitable for use in photosynthesis by terrestrial plants and breathing of terrestrial animals is found only in Earth's troposphere. [ citation needed]

The Earth from the Air - Yann Arthus-Bertrand - Google Books

That leaves approximately 1%, which is made up of atoms of unreactive argon, and molecules of carbon dioxide. Air pollution is the introduction into the atmosphere of chemicals, particulate matter or biological materials that cause harm or discomfort to organisms. [57] Stratospheric ozone depletion is caused by air pollution, chiefly from chlorofluorocarbons and other ozone-depleting substances.Air Composition". The Engineering ToolBox . Retrieved 2017-07-04. The composition of air is unchanged until elevation of approximately 10.000 m The greenhouse effect is directly related to this absorption and emission effect. Some gases in the atmosphere absorb and emit infrared radiation, but do not interact with sunlight in the visible spectrum. Common examples of these are CO 2 and H 2O.

Earth From The Air Photos and Premium High Res Pictures Earth From The Air Photos and Premium High Res Pictures

The relative concentration of gases remains constant until about 10,000m (33,000ft). [17] Stratification 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. States, Robert J.; Gardner, Chester S. (January 2000). "Thermal Structure of the Mesopause Region (80–105 km) at 40°N Latitude. Part I: Seasonal Variations". Journal of the Atmospheric Sciences. 57 (1): 66–77. Bibcode: 2000JAtS...57...66S. doi: 10.1175/1520-0469(2000)057<0066:TSOTMR>2.0.CO;2. Face of the Earth as Seen from the Air A Study in the Application of Airplane Photography to Geography NASA explores the unknown in air and space, innovates for the benefit of humanity, and inspires the world through discovery. Other layers The volume fraction of the main gases in Earth's atmosphere according to height. The boundary between the homosphere (left) and heterosphere (right) is at about 100 km. The outermost layer of the exosphere (off the chart) is dominated by hydrogen. [32]Taken from the air, the pictures show a bird's-eye view of the extraordinary patterns and colours created in landscapes all over the world. Some are the result of human activity - farming, industry or habitation. Others are entirely sculpted by nature itself. Sketches from Mr. Mathews at home! : an excellent collection of recitations, anecdotes, songs, &c. &c. In the popular entertainments of Air, earth, and water!--Country cousins!--Mail coach adventures, &c. &c. : as delivered with unprecedented success 1822 Detlev Möller: Luft: Chemie, Physik, Biologie, Reinhaltung, Recht. Walter de Gruyter, 2003, ISBN 3-11-016431-0, S. 173. (View in Google Books). From the outset, any photography taken in our study of lions was merely intended to complement the text. The real objective was to produce a scientific thesis. When I Am Laid in Earth (Air, "Dido's Lament" from the opera Dido and Aeneas): Sheet (Keyboard Ensemble Series) [Soft Cover ]