Anticyclogenesis: Difference between revisions

Latest revision as of 21:27, 13 January 2024

Any strengthening or development of anticyclonic circulation in the atmosphere; the opposite of anticyclolysis.

This applies to the development of anticyclonic circulation (or the initial appearance of a high) where previously it was nonexistent, as well as to intensification of existing anticyclonic flow. The most common application of this term is to the formation of a new anticyclone. Care should be taken, however, to distinguish the increase in anticyclonic circulation from the increase in atmospheric pressure (filling), although they usually occur simultaneously.
Compare cyclogenesis.

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 1: / Line 1: @@
+{{Term
+|Display title=anticyclogenesis
-{{TermHeader}}
+|Definitions={{Definition
-{{TermSearch}}
+|Num=1
+|Meaning=Any strengthening or [[development]] of [[anticyclonic circulation]] in the [[atmosphere]];  the opposite of [[anticyclolysis]].
-<div class="termentry">
+|Explanation=This applies to the development of anticyclonic circulation (or the initial appearance of a [[high]])  where previously it was nonexistent, as well as to [[intensification]] of existing [[anticyclonic]] flow.  The most common application of this term is to the formation of a new [[anticyclone]]. Care should  be taken, however, to distinguish the increase in anticyclonic circulation from the increase in  [[atmospheric pressure]] ([[filling]]), although they usually occur simultaneously. <br/>''Compare'' [[cyclogenesis]].
-  <div class="term">
+}}
-== anticyclogenesis ==
+}}
-  </div>
-<div class="definition"><div class="short_definition">Any strengthening or [[development]] of [[anticyclonic circulation]] in the [[atmosphere]];  the opposite of [[anticyclolysis]].</div><br/> <div class="paragraph">This applies to the development of anticyclonic circulation (or the initial appearance of a [[high]])  where previously it was nonexistent, as well as to [[intensification]] of existing [[anticyclonic]] flow.  The most common application of this term is to the formation of a new [[anticyclone]]. Care should  be taken, however, to distinguish the increase in anticyclonic circulation from the increase in  [[atmospheric pressure]] ([[filling]]), although they usually occur simultaneously. <br/>''Compare'' [[cyclogenesis]].</div><br/></div>
-</div>
-{{TermIndex}}
-{{TermFooter}}
-[[Category:Terms_A]]