Chapter 4 Flashcards
The Atmosphere
Absolute zero
The point of the kelvin scale where molecules have no kinetic energy. -273 degrees C
Heat
Measures the total kinetic energy of the molecules in a mass of gas.
1 atmosphere (atm)
The average pressure of the atmosphere at sea level is about 101355 Pa or 101 kPa (kilopascals)
Adiabatic
The rise if air rises rapidly enough, it may neither gain nor lose heat.
Adiabatic lapse rate
The rate of cooling as rising air cools.
Karman Line
Upper limit of national airspace. 100 km above earth.
Mesopause
Atmosphere 80 km above the Earth’s surface with temperature falls to a minimum
Thermosphere
Above the Mesopause. Both are parts of the ionosphere where solar radiation removes electrons from atoms and molecules, producing charged ions. Aurora borealis is produced in the thermosphere.
Stratopause
Below 50 km above the Earth’s surface. Oxygen and ozone high enough to trap incoming ultraviolet radiation. Temperature is similar to Earth’s surface.
Mesosphere
Stratopause is at the base of the mesosphere .
Troposphere
Bottom part of the atmosphere and is heated from below. . Temperature decreases upward to a boundary about 10-15 km above land or ocean surface, known as tropopause. Almost all weather occurs in troposphere.
Dalton’s Law of partial pressures
States that the total pressure of the mixed gas is the sum of the partial pressures of each gas in the mixture.
Nitrogen
Most abundant gas in Earth’s atmosphere. Mostly unreactive.
Oxygen
Represents 21% of Earth’s atmosphere. Essential to all animal life and many plants.
Ozone
O3. forms by the action of ultraviolet radiation on oxygen in the atmosphere.