CLE SATS — of the atmosrhere, Sustafson . mcacure winds in ozone layer tr QO co < A, gi (a o cr oO q on “3 *t OQ lie a ry oO u @ ct ° E ae! } “T 31,1- Micrevare?TPOp h ry ® Profect Tis was acco..plished by mecsuring at several sites the arrival tires of the shcck wave reflected fron the ozone layer, sites were operated: Five Ujelouc, uc he, Rongerik, Sikini, anc oniwetox, g h site tuo st tions were cpéreted about one mile apart, The differ- ence in arrival times rives the anzle cf incidence of the shock and inforseveral stations nay be combined to sive the winds, Cre recorier cid not operate properly at \ctho on Csase, anc at < Penzerlis no dlstinzuichatle simsal was received because of high exoient ward reise, so cicres™ ene dota probctl: cannot be chtainec fren. the Shay?Ug —— CN SS COp,