renges fro
to 170 meters.
It is le
2
. in an ere:
to the
north eof Bikini ané to the eact of Ronzelap Atolls, Yorcetuc a
tonguc like distribution.
The tongue coincides with the acre
boundary of the stream of water that enters ‘he evra on the
southeast corner and moves into the Bikini eddy.
Aricther
locale of shaliow thermocline depths exists in the ncetk cen.
tral part of the area studied.
Areas of Gesp thenmcclines
are found where water enters the northess % coraer aac were it
leaves ths nortnuest corner.
wap tae?
&
extends
le
east-west
.
across
+
the
& bend of in’ eruediate dexthe
ta
eas?
chert
on
+t.
the
a
eae
north
ovens
boundesy
the wain b
o
of
rreg
of this Band reechos soutiny
“Et
COWaeré £3
bt
etolh in tns
nhiespet2.
Bt
meLlers Gop
» bs
sgueezed from beiow into a thinner Laver as Lt move. vesteert
OTL y agate DT
sragatted
a.nd
MOVTLZOMVEL
SELTEGRUINZ
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raphe mt pacas to
COMUSar
net
ote tom
VeuELr
to
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SurPTEents «
es
bt
8]
ct
4 ws
mov cniy by korisontal but eiso vertical veriat:
"i
:
org reeset
5%
ee
aoa
see
ae we Eatin
ah
largeay areas
of fallout
trem a mepaten
weaponse
ic cooconplished
if
2
Ls
«
ow
tt
nga
so
So» Ty
ce
“a
In- somes portions
of the
ares
the
current
in the
lover
part
of
the layer above the thermocline differs from tha vopes part py
a few tens or degrees in direction and by 0.1 to C.2 knot in
~
#45
a
sn%
the two zones shear arart the upper portion af
-
&
?
~
. t
Ww
~l
speed.
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bao
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we
~
'
.
.
von
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the
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