1
Q
A
2
Q
A
3
Q
A
4
Q
A
5
Q
A
6
Q
A
7
Q
A
8
Q
A
9
Q
In confluent flow, the advective wind will
A
increase
10
Q
When the heights are falling the isallobaric wind is
A
convergent
11
Q
The advective wind is divergent when there is
A
positive vorticity advection
12
Q
Downstream of a trough (region of PVA), the advective wind is
A
divergent
13
Q
Upstream of a propagating trough the isallobaric wind is
A
divergent
14
Q
For upper-level troughs the …………………… wind dominates
A
advective
15
Q
Ahead of the upper-level trough, there is a net
A
divergence
16
Q
Ahead of a low-level trough, there is a net
A
convergence
Atmospheric Dynamics II
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