Back Aarde se atmosfeer Afrikaans Erdatmosphäre ALS ከባቢ አየር Amharic غلاف الأرض الجوي Arabic পৃথিৱীৰ বায়ুমণ্ডল Assamese Atmósfera terrestre AST हवा AWA Yerin atmosferi Azerbaijani یئرین آتموسفری AZB Ер атмосфераһы Bashkir
The Earth's atmosphere is the layer of gasses around the Earth. It is held in place by Earth's gravity. It is today made up mainly of nitrogen (78.1%). It also has plentiful oxygen (20.9%) and small amounts of argon (0.9%), carbon dioxide (~ 0.035%), water vapor, and other gases. The atmosphere protects life on Earth by absorbing (taking) ultraviolet rays from the Sun. It makes our days cooler and our nights warmer.
Solid particulates, including ash, dust, volcanic ash, etc. are small parts of atmosphere. They are important in making clouds and fog.
The atmosphere does not end at a specific place. The higher above the Earth, the thinner the atmosphere. There is no clear border between the atmosphere and outer space, though the Kármán line is sometimes treated as a border. Even higher, for some purposes the edge of the magnetosphere is treated as a border. 75% of the atmosphere is within 11 kilometres (6.8 miles) of the Earth's surface.