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

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
as f----\> 0 near the ......................., the geostrophic balance is not valid at .......................
equator low latitudes
26
the vertical momentum equation indicated that
the vertical pressure gradient force is in exact balance with the gravity force
27
define hydrostatic equilibrium
the pressure at any point is simply equal to the weight of a unit cross-section column of air above that point
28
the hydrostatic approximation may be expressed as
29
the higher the PGF the
stronger the wind
30
vertical PGF =
gravity force