| OCR Text |
Show 1 nn r wi.j a w !. II tho wind blow directly imrallel to the $cn surface tlio friction may causa an ocean current uillioutuaiedliturb nuee, Asa rule the direction of the wind Is Inclined to tho sea surfaeo, and Its immediate effect Is to produce a do-rcsitlon, do-rcsitlon, which nlleiesltulf bymcans of n WAa to leewaril ami another to wlndwunl 'llils laltir ileration Is opposed op-posed by tho win 1 and gradually i!Ui uwoy, while the Icefanl waro Is cor npoii Ungly accelerated acb undulation undu-lation shelters tlio water under Its Ico from tho wind, which consequently ho-plngos ho-plngos upon thosraalltUaliiaihaiica of tlio newly formed wave, and Ihiiswj get a sorlea of par illel Mhrt Olid hoi-lows, hoi-lows, pruvldod the wind n main steady In direction and Intensity Chambers' Jouriuil |
