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 — -_w as 35° _=Zz . YU ROCHI Lea h s- > 165°15 =z | 1¢ as * & ? § 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 . : , {_. i