404 Glossary
When considering the Coriolis effect on winds and water, v
u
is
small, and the vertical component of the Coriolis force is negligible
compared to gravity. Thus, only the horizontal velocity components
matter, and we can write
v
v
v
v
v
=
=
−
e
n
n
e
and F
c
m ( sin )2ω ϕ
(GL6)
From the vector matrix equations above, we can see that if v
n
= 0
and ω and φ > 0, a mass point moving due east experiences a Coriolis
force accelerating it due south. Similarly, setting v
e
= 0, a mass ele-
ment moving due north is acted on by a Coriolis force moving it due
east.
Coulombic efciency (of battery): The coulombic efciency, η
c
, of a battery is
the ratio of the number of charges that enter the battery during charg-
ing to the ...