Atmospheric basics Flashcards

1
Q

wind is a

A

vector quantity

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2
Q

wind has

A

speed and direction

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3
Q

the wind speed is measured in

A

m/s or knots

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4
Q

1 knot =

A

0.51 m/s

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5
Q

The wind direction is measured in ………………. from ……………………………

A

degree angle north (0 degrees / 360 degrees)

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6
Q

Wind direction indicates the direction

A

from which the wind blows.

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7
Q

wind velocity is a ……………. component

A

scalar

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8
Q

The three scalar components of wind in Cartesian (x, y and z) coordinate system

are expressed as

A
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9
Q

The horizontal wind vector can be expressed in terms of scalars as:

A
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10
Q

The two scalar wind components (u and v) can be obtained from

A

wind speed and direction

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11
Q

The two scalar wind components (u and v) can be obtained from the wind speed and direction as follows

A
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12
Q

Synoptic scale motions have a size of approximately

A

1000 km

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13
Q

for synoptic scale motions friction ……

A

can be neglected above the lowest few km

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14
Q

scale analysis for the ………………………………. for ……………………………………. shows that ……………………………………………………….. are in exact balance

A

horizontal momentum equations

mid-latitude synoptic scale disturbance

the horizontal components of coriolis force and pressure gradient force

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15
Q

geostrophic approximation for the x and y direction

A
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16
Q

define Rossby number

A

nondimensional number which gives a measure of the magnitude of the acceleration compared to the Coriolis force

17
Q

how can you obtain the Rossby numbre?

A

by forming the ratio of the characteristic scales of acceleration and the coriolis force terms

18
Q

equation of Rossby number

A
19
Q

the smallness of the Rossby number is

A

a measure of the validity of the geostrophic approximation

20
Q

if Ro<1

A

the coriolis force is a dominant force, and the flow tends to become geostrophic

21
Q

if Ro>1

A

the flow tends to be non-geostophic

22
Q

you can neglect acceleration term in

A

mid latitude

23
Q

geostrophic wind always

A

blows parallel to the isobars with low pressure to the left

24
Q

as density is nearly constant at a given height, …………………………..

A

the geostrophic wind is linearly proportional to the pressure gradient

25
Q

as f—-> 0 near the ………………….., the geostrophic balance is not valid at …………………..

A

equator

low latitudes

26
Q

the vertical momentum equation indicated that

A

the vertical pressure gradient force is in exact balance with the gravity force

27
Q

define hydrostatic equilibrium

A

the pressure at any point is simply equal to the weight of a unit cross-section column of air above that point

28
Q

the hydrostatic approximation may be expressed as

A
29
Q

the higher the PGF the

A

stronger the wind

30
Q

vertical PGF =

A

gravity force