Chapter 4 Flashcards

The Atmosphere

1
Q

Absolute zero

A

The point of the kelvin scale where molecules have no kinetic energy. -273 degrees C

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2
Q

Heat

A

Measures the total kinetic energy of the molecules in a mass of gas.

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3
Q

1 atmosphere (atm)

A

The average pressure of the atmosphere at sea level is about 101355 Pa or 101 kPa (kilopascals)

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4
Q

Adiabatic

A

The rise if air rises rapidly enough, it may neither gain nor lose heat.

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5
Q

Adiabatic lapse rate

A

The rate of cooling as rising air cools.

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6
Q

Karman Line

A

Upper limit of national airspace. 100 km above earth.

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7
Q

Mesopause

A

Atmosphere 80 km above the Earth’s surface with temperature falls to a minimum

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8
Q

Thermosphere

A

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.

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9
Q

Stratopause

A

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.

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10
Q

Mesosphere

A

Stratopause is at the base of the mesosphere .

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11
Q

Troposphere

A

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.

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12
Q

Dalton’s Law of partial pressures

A

States that the total pressure of the mixed gas is the sum of the partial pressures of each gas in the mixture.

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13
Q

Nitrogen

A

Most abundant gas in Earth’s atmosphere. Mostly unreactive.

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14
Q

Oxygen

A

Represents 21% of Earth’s atmosphere. Essential to all animal life and many plants.

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15
Q

Ozone

A

O3. forms by the action of ultraviolet radiation on oxygen in the atmosphere.

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16
Q

Saturation vapour pressure

A

the maximum amount of water that can exist in the air if it’s in equilibrium with liquid water or (below freezing) with solid ice.

17
Q

Argon

A

4th most abundant component in atmosphere. It is inert.

18
Q

Aerosols

A

Small solid particles and liquid drops in the Atmosphere.

19
Q

Equilibrium

A

State reached when the rate transfer of molecules is the same in each direction.

20
Q

Dew Point

A

The temperature that is cold enough for a deposit of water, know as dew, to form on exposed surfaces.

21
Q

Nucleation energy

A

Extra energy taken out to achieve the first condensation of a very small water drop.

22
Q

Clouds

A

Formed by aerosol typically scatter the light. If there is more than one drop per cubic millimetre of Atmosphere, frequent collisions between droplets form larger droplets and those raindrops fall as rain.