Bermuda high: Difference between revisions

Revision as of 15:29, 25 April 2012

Bermuda high[edit | edit source]

The semipermanent subtropical high of the North Atlantic Ocean, so named especially when it is located in the western part of the ocean.

This same high, when displaced toward the eastern part of the Atlantic, is known as the Azores high. On mean charts of sea level pressure, this high is a principal center of action. Warm and humid conditions prevail over the eastern United States, particularly in summer, when the Bermuda high is well developed and extends westward.

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">The semipermanent [[subtropical high]] of the North Atlantic Ocean, so named especially  when it is located in the western part of the ocean.</div><br/> <div class="paragraph">This same [[high]], when displaced toward the eastern part of the Atlantic, is known as the [[Azores  high]]. On [[mean charts]] of [[sea level pressure]], this high is a principal [[center of action]]. Warm  and humid conditions prevail over the eastern United States, particularly in summer, when the  Bermuda high is well developed and extends westward.</div><br/> </div>
+<div class="definition"><div class="short_definition">The semipermanent [[subtropical high]] of the North Atlantic Ocean, so named especially  when it is located in the western part of the ocean.</div><br/> <div class="paragraph">This same [[high]], when displaced toward the eastern part of the Atlantic, is known as the [[Azores high|Azores  high]]. On [[mean charts]] of [[sea level pressure]], this high is a principal [[center of action]]. Warm  and humid conditions prevail over the eastern United States, particularly in summer, when the  Bermuda high is well developed and extends westward.</div><br/> </div>
 </div>