Lecture 9 Flashcards

1
Q

General Circulation

A

The long-term(usually decadal scales) average winds(directions and speed) in the atmoshpere as a function of location.

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2
Q

Climate

A

The long-term average state of the atmoshpere.

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3
Q

Weather

A

The instantaneous state of the atmosphere.

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4
Q

Sensible Heat

A

The energy contained in the molecules as a result of their random kinetic energy.

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5
Q

Thermal conduction

A

The transfer of sensible heat through materials or gases that are in contact as a result of the collision of hot molecules with cool molecules. Note no transfer of mass required.

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6
Q

Thermal convection and advection

A

The transfer of sensible heat by movement(or exchange) of mass. Convection usually refers to vertical movement and advection to horizontal.

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7
Q

Is the energy budget in balance in all locations of the earth?

A

No

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8
Q

What types of forces is air usually subject to?

A

1) Gravity

2) Pressure

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9
Q

In respect to the atmosphere, what is the result of imbalances of energy on earth?

A

Movement of energy from tropics to poles

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10
Q

What happens when the net force on air is not balanced?

A

It moves as a function of wind

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11
Q

Horizontal air motion is caused by what forces and why?

A

Just pressure, gravity affects vertical air movement. Air tends to move from regions of high pressure to low pressure.

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12
Q

Pressure Gradient force

A

Change in pressure over some distance

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13
Q

Hydrostatic equilibrium

A

Balance between net upward pressure and downward force of gravity.

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14
Q

Vertical motion of air only is effected by gravity (T/F)

A

F

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15
Q

There is a parcel of air with a lower density than the air around it. What will happen to the parcel and why?

A

The parcel would rise due to its lighter weight than air(force due to gravity). The pressure gradient force would be the same.

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16
Q

Low density air moves…

A

upward

17
Q

High density air moves..

A

downward

18
Q

Convection

A

Density differences due to temperature. P=pRT

19
Q

Coriolis effect

A

Deflection of air westward(north) and eastward (south) due to earth spinning on its axis.

20
Q

Polar front

A

Area of convergence where cold polar air meets warmer air to form a Ferrel cell.

21
Q

Intertropical Convergence Zone

A

The equatorial low where air rises

22
Q

Why are Ferrell Cells “invisible in real time”?

A
  • They are averaged wind flows

- If winds are averaged over decades, flows begin to appear

23
Q

Atmoshperic Scales of Motion (ASM)

A

Motion of energy in the atmosphere characterized by different scales.

24
Q

examples of Planetary ASM

A

Rossby(long) waves

25
Q

examples of Synoptic ASM

A

Lows, Fronts, Hurricanes

26
Q

examples of Meso alpha ASM

A

Squall Lines, MCC

27
Q

examples of Meso beta ASM

A

Large thunderstorms, sea breeze fronts

28
Q

examples of Meso lambda ASM

A

Thunderstorms, tornadoes

29
Q

examples of Micro ASM

A

Dust Devils

30
Q

Why is the measurement of Meso ASM a very modern occurence?

A

Lacked measurement technology in the past