Chapter 2 part 1 Flashcards

1
Q

Horizontal divergence is expressed mathematically as

A
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2
Q

When thedivergence is positive, the air parcel

A

grows (i.e., its area increases)

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3
Q

If the divergence is negative, it is called

A

convergence, then the air parcel shrinks (i.e., area decreases).

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4
Q

The relationship between horizontal divergence and the change in a parcel’s area
(A) can be expressed as:

A

The above equation states that the fractional change in the area is equal to the
horizontal divergence.

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5
Q

The relationship between horizontal divergence and the vertical velocity can be
obtained from

A

the continuity equation as:

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6
Q

In the troposphere, the vertical velocity is

A

close to zero (w~0) at two altitudes

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7
Q

In the troposphere, the vertical velocity is close to zero (ݓ~0) at two altitudes.

A

The first is Earth’s surface, which forms a solid boundary.
• The second is the tropopause, above which the rapid increase in stratospheric potential temperature strongly inhibits vertical motion.

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8
Q

Divergence aloft is associated with

A

air throughout the troposphere

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9
Q

Divergence aloft is associated with air throughout the troposphere, which
is associated with

A

pressure and at the surface

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10
Q

Convergence aloft is associated with

A

sinking air throughout the troposphere

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11
Q

Convergence aloft is associated with sinking air throughout the troposphere,
which is associated with

A

high pressure and divergence at the surface

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12
Q

So, starting at the surface, the vertical velocity becomes

A

more with height when there is surface convergence, reaches some maximum vertical velocity, and then becomes positive with height becoming divergence aloft

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13
Q

Similarly, starting again at the surface, the vertical velocity becomes more negative
with height when there is

A

surface divergence, reaches some maximum negative velocity, and then becomes less negative with height again near convergence aloft.

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14
Q

When the surface divergence (or convergence) with height changes into

A

upper air convergence (or divergence)

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15
Q

When the surface divergence (or convergence) with height changes into upper air
convergence (or divergence), at some level in the troposphere (called

A

the level of non-divergence, LND), the divergence becomes zero.

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