Secondary cyclone: Difference between revisions

Latest revision as of 16:50, 25 April 2012

secondary cyclone

(Or secondary low.) A cyclone that forms near, or in association with, a primary cyclone.

For example, secondary cyclones often form along the east coast of the United States when a primary cyclone is present in the Great Lakes region. Similarly, secondary cyclones often occur over the Baltic when a primary cyclone is present near the coast of Norway.
See also center jump.

INDEX
A
B
C
D
E
F
G
H
I
J
K
L
M
N
O
P
Q
R
S
T
U
V
W
X
Y
Z
0
1
2
3
4
5
6
7
8
9

@@ Line 9: / Line 9: @@
    </div>
-<div class="definition"><div class="short_definition">(''Or'' secondary low.) A [[cyclone]] that forms near, or in association with, a [[primary  cyclone]].</div><br/> <div class="paragraph">For example, secondary cyclones often form along the east coast of the United States when a  primary cyclone is present in the Great Lakes region. Similarly, secondary cyclones often occur  over the Baltic when a primary cyclone is present near the coast of Norway. <br/>''See also'' [[center jump]].</div><br/> </div>
+<div class="definition"><div class="short_definition">(''Or'' secondary low.) A [[cyclone]] that forms near, or in association with, a [[primary cyclone|primary  cyclone]].</div><br/> <div class="paragraph">For example, secondary cyclones often form along the east coast of the United States when a  primary cyclone is present in the Great Lakes region. Similarly, secondary cyclones often occur  over the Baltic when a primary cyclone is present near the coast of Norway. <br/>''See also'' [[center jump]].</div><br/> </div>
 </div>