The Earth's atmosphere:
gas mixture to suspend certain solids and liquids.
gas mixture to suspend certain solids and liquids.
Three common constant in the atmosphere:
-Ice
-Dust
-Salt - from Ocean Spray
Gas composition of the atmosphere:
- Nitrogen - 78% of atmosphere
- Oxygen - 21% of atmosphere
- Trace gases - 1% - Neon, Helium, Hydrogen, Methane, Carbon Dioxide
Creating the atmosphere:
The atmosphere is the result of a planetary degassing, a process in which gases such as carbon dioxide, water vapor, sulfur dioxide and nitrogen were released from inside the Earth and volcanoes other processes.
Structure of the Earth's atmosphere: (With the basis of space.)
Troposphere-ok. ground to 10 km (about 7 miles up)
- Where is the layer of the Earth.
- It contains 75% of our atmosphere of greenhouse gases
- Weather and clouds of smog occur in the troposphere
Stratosphere - 10 km - 45 km (about 7 miles, 30 miles)
- The ozone layer is here
- jet can be found here
- Little or no water vapor
- The ozone layer is here
- jet can be found here
- Little or no water vapor
Mesosphere - 45 km -95 km at the top (30 to 50 miles)
the coldest part of the atmosphere
the coldest part of the atmosphere
Thermosphere - about 95 km to 500 km (50 miles up)
1. Hottest layer of the atmosphere.
lower layer called the ionosphere thermosphere
- Ionosphere with charged particles electronically.
- reflects radio waves
- The day of this layer distorts the radio waves emitted by the charges for a large number of particles of solar energy and causes a lot of static problems.
- At night, it is less loaded. Therefore, it is easier to hear the AM radio late at night
1. Hottest layer of the atmosphere.
lower layer called the ionosphere thermosphere
- Ionosphere with charged particles electronically.
- reflects radio waves
- The day of this layer distorts the radio waves emitted by the charges for a large number of particles of solar energy and causes a lot of static problems.
- At night, it is less loaded. Therefore, it is easier to hear the AM radio late at night
Exosphere - approximantly 500 km and beyond
The outer layer of the atmosphere over
Very few air molecules in this layer
The lack of clear boundaries between the layers and space
via williamsclass
The outer layer of the atmosphere over
Very few air molecules in this layer
The lack of clear boundaries between the layers and space
via williamsclass
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