dl that we
ieee
.. -h (Pic. 8).
250 meters
-rface waters are
Even though
warmer om the south than on the north side, the average for
this layer is 1 to 3°C less on the south.
Vortical distribvtion of temperature is chazzcterized bj
a shallow, windestirred layer vsually 90 to 125 meteors deen and
nearly constant in temperature; below tnis the temporeture
decreases abruptly dewn to about 250 to 390 meters
deanuth:
thence it decreases ever more slowly to 1.u° © at 459% meters
teuperature is tne main thermocline; here the densit, elise
submarines found the thermocline to be a
—_— aa
se
ss
7
ture; they wore able to
i
oN
ke
and
+
°
a4
4
‘,
bale iz
*,
205
on
on.
:
the
yee
oy
mf
vy
pe
ood
oh
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a
highhy usefat struc
s
tpene
tacene detection by stoprinsk ell encines
Nim eee, TD
gen
we
-
Veo Laat) BG LLIiS «
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ne:
4
ies
a
a
QQ
i
fa
ens tovard the nerth in the eras stud
th
In general, the thermocline thick~
[=
ne
creases rapidly (Fig. GJ),
.
i448
nas
-*
thaneagir snips bumncing on e lover of
.
a
23
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a
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Mixing
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he
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surtece,
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layer.
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This the
bal
:
thermoclinc
+
7
¥
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- 2
one
rat
a great
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more enerry
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mixing
in tage
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PeTU. FSS
ae
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¢
4
4. peer,
depth
to 4
the tos
offe
ently
the
thermocline is, as « Cirst approximation, a maasure «f the cezen
in the first few davs after detonation.
Based on 1°05 bethyvhermogrann lowerings made durins the
HOREVON's emiise, a cher t
the thermocline
(Pig. 10).
@
bon.
"&
. .
(Over the entire area this derth