268
BIKINI AND NEARBY ATOLLS, MARSIIALL ISLANDS
AaSee
henwth
-
ms
Ow
~~ ~WINd
LAGOON
2SNESop
THICK
—
Se SE
iiskdtie
oH
UPWELLING
vet |
_@ THICKENING SURFACE CURRENT —,
eteNagelnae Ne Cnettet Mamet SE cages
we ee eae See ee
nee ee nee ee see nee
|
i eee ee Oe oe,
SWELL
7
BOTTOM CURRENT
“CORAL” ATOLL
oa
VERTICAL EXAGGERATION —— 42 TIMES
LENGTH OF SECTION — 2! MILES
DEPTH OF SECTION —- 30 FATHOMS
Fravet &&-yNature of wind-driven overturning circulation (schematic).
20°
23’
L_ aoft
io
--
7"
_
a
=“
GE
FOO ae
Sasgis
ose AS
Pn ae
“7
—
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as
35°
_=Zz
.
YU ROCHI
Lea
h
s-
>
165°15
=z
|
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as
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&
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§
4
eee Swe
wa
1
”
-
x
~
BIKINI |
-_
-
|
}— 35'
oe
BOKORORYUR
Lee ote ee
et
DIENYU |
aw
37
=
EXPLANATION
7 ----
Surfoce
j
Water
———pe
.
~~
7
Velaee
Motions
RUKOJI CHANNEL
Bottom
Circulation
ee ee ee
—
Tide Controtted Currents
!
7
I
S000018
on
3°
sae
Slee ae” “= ~-=
BO
oO
Seton
He
AIRUKATNE I
1
——
FicvarAbe—Gcoecralized circulation of Bikini Lagoon in winter.
.
A-17
BIKINI ATOLL
REORAWN FROM CHART
H.0. 6032
.
:
,
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i