Final Exam Flashcards

1
Q

Dynamic Meteorology involves the development of theoretical physical laws to understand and predict phenomenon in the atmosphere

A

True

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2
Q

When an orthogonal Cartesian coordinate system is used in meteorology, the positive x-axis is orientated such that it points towards the east.

A

True

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3
Q

AxB = ABcos(θ) where θ is the angle between the vectors A and B

A

False

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4
Q

If the velocity divergence at a location is less than zero then convergence is occurring at that location

A

True

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5
Q

If an air parcel is moving towards the west (u>0) and du/dt is greater than zero (>0) then air parcel is speeding up.

A

False

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6
Q

The basis for the derivation of the equation of motion is Newton’s second law (F=m(dava/dt)

A

True

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7
Q

A coordinate system “fixed” to Earth, and therefore rotating with Earth, is referred to as an inertial or absolute coordinate system

A

False

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8
Q

The effective gravity vector used in the equation of motion is the sum of Earth’s gravitational attraction and the Coriolis force that is present due to Earths rotation.

A

False

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9
Q

An air parcel moving in a North-South direction (v does not equal to zero) will experience a Coriolis acceleration in the east-west direction (du/dt does not equal to 0) due to the parcel conserving absolute angular momentum (ωr)

A

True

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10
Q

Horizontal Temperature _________; the local _____ rate of change in temperature due to the horizontal mass ______ of air.

A

Advection, time, movement

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11
Q

Inertial coordinate system

A

Fixed to absolute space

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12
Q

Non-inertial coordinate system

A

Fixed to a rotating body

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13
Q

The absolute angular momentum associated with an air parcel is moving about Earths axis of rotation is determined by (1) angular velocity of the air parcel about Earth’s axis of rotation (ω) and (2) the radius of rotation relative to earth’s axis squared (r^2)

A

True

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14
Q

A system of equations that describes changes in volume of air moving with the volume of air is referred to as a Lagrangian system

A

True

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15
Q

Winds in the horizontal on the synoptic scale are typically order 10^2 m/s

A

False

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16
Q

The friction force acts to reduce the wind speed, and therefore will also reduce the magnitude of the Coriolis force

A

True

17
Q

If the tangential velocity component in the polar coordinate system (vθ) is less than zero, the flow is counter clock wise (cyclonic)

A

False

18
Q

Higher density

A

Weaker P.G.F

19
Q

Lower density

A

Stronger P.G.F

20
Q

Small r

A

Big centrifugal force

21
Q

Big r

A

Small centrifugal force

22
Q

Hydrostatic Balance

A

Vertical pressure gradient force balanced by gravity

23
Q

Geostrophic Balance

A

Horizontal pressure gradient force balanced by the Coriolis force

24
Q

Cyclostrophic Balance

A

A balance between the horizontal pressure gradient force and the centrifugal force; representative of small scale curved flow associated with high wind speeds and phenomenon at low latitudes

25
Q

Small R («1)

A

Small centrifugal force big Coriolis force (Geostrophic Flow)

26
Q

R~1

A

Centrifugal force = Coriolis force

27
Q

Big R (»1)

A

Big centrifugal force, small Coriolis force (Cyclostrophic flow)

28
Q

Thermal Wind

A

A vector that represents the vertical shear of the Geostrophic wind