. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography hrl- G o in r\ SURFACE VELOCITY Ts= 21°c Ss= 357^ ^$=10245 o U 'l3. I-*â 10&mââº- I GULF STREAM SEA SURFACE GEOID ISOPYCNALS Figure I. Schematic crosa-section of a western boundary current in the northern hemisphere. Hove the exaggeration of the sea surface as compared to the sub- surface feazurcs, where a 102 scale change is used for clarity. one example of that will be discussed later. Asso ther whic Deta full cont euph Thes thet bear
. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography hrl- G o in r\ SURFACE VELOCITY Ts= 21°c Ss= 357^ ^$=10245 o U 'l3. I-*â 10&mââº- I GULF STREAM SEA SURFACE GEOID ISOPYCNALS Figure I. Schematic crosa-section of a western boundary current in the northern hemisphere. Hove the exaggeration of the sea surface as compared to the sub- surface feazurcs, where a 102 scale change is used for clarity. one example of that will be discussed later. Asso ther whic Deta full cont euph Thes thet bear blue tion the asso prop ter i sedi dele wh i c the riated e appe h is a i 1 s of y unde inuous otic z e nutr i c org ing pi light , shif green, ciated c r t i e s iig oi ments ct ed a h also water. with t ars to 1 s o s k e this i! rstood; 1 y b r i n one a]o i e n t s a ani s;;is ants. , and w t the c The p o r g a n i of the light. from th long th. modify l-i) he hori be a ve t c h e d o pwel1 in howeve g n u t r i n g the re ut ] 1 w h i c h a Pigment hen in olor o f hytopla sms cha water Freque c coast e curre the op zon rt i n F g m r, erit eye izc re ed suf th n k t n^c bv n'tl al nt 11C the to motion , c i rcu]at ion, e 1. (â >) n are not effect is to the c edge. photosyn- r o p h >â 11 - culcs absorb ent concentra- a towards nd other optica 1 eased scat- ntrained ons can be a he c r e undaries, properties of When wind and waves run in opposition to the current, the local sea builds higher than when they run in the same direction. Thus the sea "ay be higher or lower in the current depending on the relative wind/cur- rent directions. The latter feature often translates into changes in white cap and foam distributions, changes in glitter patterns, and changes in surface wave refraction patterns. To reiterate, when crossing into the Gulf Stream from the west, one typically encount- ers an increase in temperature, salinity, and perhaps sea state; the colo
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