earth’s atmosphere
DESCRIPTION
This presentation is all about the Earth's atmosphere, its composition, layers and the air pollutants.TRANSCRIPT
![Page 1: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/1.jpg)
EARTH’S ATMOSPHERE
![Page 2: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/2.jpg)
INTRODUCTION• The atmosphere of Earth is a layer of gases
surrounding the planet Earth.• The atmosphere protects life on Earth.• The atmosphere becomes thinner and thinner
with increasing altitude, with no definite boundary between the atmosphere and outer space.
![Page 3: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/3.jpg)
COMPOSITION
• 78% nitrogen• 20%oxygen• 2% other gases
![Page 4: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/4.jpg)
LAYERS of the
ATMOSPHERE
![Page 5: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/5.jpg)
![Page 6: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/6.jpg)
TROPOSPHERE• begins at the surface and extends to between
9 km (30,000 ft) at the poles and 17 km (56,000 ft) at the equator
• mostly heated by transfer of energy from the surface
• TROPOPAUSE - is the boundary between the troposphere and stratosphere.
![Page 7: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/7.jpg)
![Page 8: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/8.jpg)
STRATOSPHERE• extends from the tropopause to about 51 km
(32 mi; 170,000 ft). • Temperature increases with height• STRATOPAUSE - is the boundary between the
stratosphere and mesosphere which, typically is at 50 to 55 km (31 to 34 mi; 160,000 to 180,000 ft).
![Page 9: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/9.jpg)
![Page 10: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/10.jpg)
OZONE LAYER
• is contained within the stratosphere and is mainly located in the lower portion of the stratosphere from about 15–35 km (9.3–22 mi; 49,000–110,000 ft)
![Page 11: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/11.jpg)
NACREOUS CLOUDS• called mother-of-pearl clouds• they are filmy sheets slowly curling and
uncurling, stretching and contracting in the semi-dark sky.
• are seen mostly during winter at high latitudes like Scandinavia, Iceland, Alaska and Northern Canada. Sometimes, however, they occur as far south as England.
![Page 12: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/12.jpg)
![Page 13: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/13.jpg)
MESOSPHERE
• extends from the stratopause to 80–85 km (50–53 mi; 260,000–280,000 ft)
• MESOPAUSE - the temperature minimum that marks the top of the mesosphere
![Page 14: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/14.jpg)
![Page 15: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/15.jpg)
NOCTILUCENT CLOUDS• are tenuous cloud-like phenomena that are
the "ragged-edge" of a much brighter and pervasive polar cloud layer called polar mesospheric clouds in the upper atmosphere.
• They are made of crystals of water ice.• are most commonly observed in the summer
months at latitudes between 50° and 70° north and south of the equator.
![Page 16: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/16.jpg)
![Page 17: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/17.jpg)
![Page 18: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/18.jpg)
THERMOSPHERE• the inversion is a result of the extremely low
density of molecules.• The International space Station orbits in this
layer, between 320 and 380 km (200 and 240 mi).
• TURBOPAUSE – where homsphere and heterosphere divides.
• Homosphere and heterosphere are defined by whether the atmospheric gases are well mixed.
• EXOBASE - The top of the thermosphere is the bottom of the exosphere
![Page 19: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/19.jpg)
![Page 20: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/20.jpg)
IONOSPHERE• the part of the atmosphere that is ionized by
solar radiation• stretches from 50 to 1,000 km (31 to 620 mi;
160,000 to 3,300,000 ft) • typically overlaps both the exosphere and the
thermosphere. It forms the inner edge of the magnetosphere.
![Page 21: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/21.jpg)
AURORA
![Page 22: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/22.jpg)
![Page 23: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/23.jpg)
![Page 24: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/24.jpg)
EXOSPHERE
• The outermost layer of Earth's atmosphere extends from the exobase upward
• mainly composed of hydrogen and helium
![Page 25: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/25.jpg)
POLLUTANTSin the
ATMOSPHEREPOLLUTANT - A substance in the air that can cause harm to humans and the environment is known as an air pollutant. Pollutants can be in the form of solid particles, liquid droplets, or gases. In addition, they may be natural or man-made.
![Page 26: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/26.jpg)
CLASSES OF POLLUTANTS• Sulphur Oxide - produced by volcanoes and in various
industrial processes• Nitrogen Oxide - emitted from high temperature
combustion, and are also produced naturally during thunderstorms by electrical discharge.
• Carbon Monoxide - is a colourless, odorless, non-irritating but very poisonous gas.
• Carbon Dioxide - a colourless, odorless, non-toxic greenhouse gases emmited from sources such as combustion, cement production, and respiration.
![Page 27: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/27.jpg)
• Volatile Organic Compounds - divided into the separate categories of methane (CH4) and non-methane. Methane contributes to enhanced global warming.
• Particulate Matter - are tiny particles of solid or liquid suspended in a gas.
• Chlorofluorocarbon - harmful to the ozone layer emitted from products currently banned from use.
• Ammonia - from agricultural processes. • Radioactive Pollutants - produced by nuclear
explosion, nuclear events, war explosives, and natural processes such as the radioactive decay of radon.
• Toxic metals, such as lead, cadmium and copper.
![Page 28: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/28.jpg)
Prepared by: MAS, Pamela Bianca E.
MANAHAN, Sophia Nicole A.LOPEZ, Realyn
LIBRES, Mary GraceJAINAR, Glaisa Mae
GAMIAO, Allan Craig W.PSYCH 1-D
![Page 29: Earth’s Atmosphere](https://reader036.vdocument.in/reader036/viewer/2022062419/557c2764d8b42aa77f8b4b0d/html5/thumbnails/29.jpg)
END OF SLIDE-END OF SLIDE-END OF SLIDE-END OF SLIDE-END OF SLIDE-END OF SLIDE