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,~ / -, S <br /> ~ rtx <br /> H -~ itAt 212 <br /> A -- <br /> I-s - N-. <br /> ..~. %`Ik <br /> -- 5- * »=2% - - <br /> ¾ Ii ~~«=--~-- ¼ <br /> - *,,d2~ ,.~ -- <br /> 1~ <br /> * 1 tNt' <br /> -<Sr <br /> L N *` <br /> `I `I <br /> I. <br /> - , <br /> TYPICAL SUMMER DAYTIME OCEAN WINDS TYPICAL SUMMER NIGHT DRAINAGE WINDS <br /> (Noon to 7:00 PM) (Midnight to 5:00 AM) <br /> oI A: - <br /> -. , <br /> __ -v-I.. <br /> - r <br /> - ~ - <br /> * S - <br /> O~. <br /> j N-~ -- N' <br /> e <br /> r <br /> MP'~ <br /> a' I-.. <br /> -`I <br /> TYPICAL WINTER DAYTIME OCEAN WINDS TYPICAL WINTER NIGHT DRAINAGE WINOS <br /> a -- <br /> (Noon to 5:00 PM) aLa (Midnight to 7:00AM) <br /> o~ILe <br /> These maps show dominant suMner and winter patterns in <br /> the South Coast Air Basin. For the period of the day shown, the <br /> net transport of air onshore usually Is greater in the summer, <br /> while the net offshore transport as a rule is greater during the <br /> winter. Whether there is air movement or air stagnation during the <br /> morning and evening hours, before these dominant air flow patterns <br /> take effect, is one of the critical factors In determining the <br /> smog situation on any given day. <br /> Source: Title: <br /> SOUTH COAST AIR QUALITY flPICAL WIND PATTERNS IN <br /> MANAGEMENT DISTRICT GENERAL VICINITY OF <br /> PROJECT SITE <br /> lot: