Fil:NASA Earth radiation thermal balance energy budget atmosphere.jpg

NASA_Earth_radiation_thermal_balance_energy_budget_atmosphere.jpg(720 × 507 piksler, filstørrelse: 86 KB, MIME-type: image/jpeg)


Wikimedia Commons' logo

Beskrivelse

Beskrivelse
English: The atmosphere radiates the equivalent of 59% of incoming sunlight back to space as thermal infrared energy, or heat. Where does the atmosphere get its energy? The atmosphere directly absorbs about 23% of incoming sunlight, and the remaining energy is transferred from the Earth’s surface by evaporation (25%), convection (5%), and thermal infrared radiation (a net of 5-6%). The remaining thermal infrared energy from the surface (12%) passes through the atmosphere and escapes to space. (NASA illustration by Robert Simmon. Astronaut photograph ISS017-E-13859.) See also NASA Earth’s Energy Budget and The NASA Earth's Energy Budget Poster
Kilde http://earthobservatory.nasa.gov/Features/EnergyBalance/page6.php
Opphavsperson NASA Earth Observatory

Lisensiering

Public domain This file is in the public domain in the United States because it was solely created by NASA. NASA copyright policy states that "NASA material is not protected by copyright unless noted". (See Template:PD-USGov, NASA copyright policy page or JPL Image Use Policy.)
Warnings:

Filhistorikk

Klikk på et tidspunkt for å vise filen slik den var på det tidspunktet.

Dato/klokkeslettMiniatyrbildeDimensjonerBrukerKommentar
nåværende20. apr. 2014 kl. 16:54Miniatyrbilde av versjonen fra 20. apr. 2014 kl. 16:54720 × 507 (86 KB)Prokaryotes{{subst:Upload marker added by en.wp UW}} {{Information |Description = {{en|Just as the major atmospheric gases (oxygen and nitrogen) are transparent to incoming sunlight, they are also transparent to outgoing thermal infrared. However, water vapor, ca...

Den følgende siden bruker denne filen:

Global filbruk

Følgende andre wikier bruker denne filen: