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By Michael M. Benarie

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S. The r e s u l t i s c l e a r s k i e s , w i t h n o r t h e r l y winds a l o f t which o f t e n extend down t o t h e surface. During t h i s period t h e Great Basin surface high (Fig. 3 ) becomes w e l l e s t a b l i s h e d o v e r t h e c o l d e r , h i g h e r desert p l a t e a u , g i v i n g rise t o predominantly n o r t h e r l y winds i n t h e Mohave Valley. These a r e o f t e n l o c a l l y i n t e n s i f i e d i n t h i s a r e a because of t h e t o p o g r a p h i c a l c h a n n e l i n g e f f e c t of t h e Colorado R i v e r Valley.

S. The r e s u l t i s c l e a r s k i e s , w i t h n o r t h e r l y winds a l o f t which o f t e n extend down t o t h e surface. During t h i s period t h e Great Basin surface high (Fig. 3 ) becomes w e l l e s t a b l i s h e d o v e r t h e c o l d e r , h i g h e r desert p l a t e a u , g i v i n g rise t o predominantly n o r t h e r l y winds i n t h e Mohave Valley. These a r e o f t e n l o c a l l y i n t e n s i f i e d i n t h i s a r e a because of t h e t o p o g r a p h i c a l c h a n n e l i n g e f f e c t of t h e Colorado R i v e r Valley.

A i r t r a j e c t o r i e s a r e drawn w i t h s o u r c e s as t h e o r i g i n s o f t h e t r a j e c t o r i e s and t h e d i s p e r s i o n c h a r a c t e r i s t i c s i s s t u d i e d w i t h d i s t a n c e and t i m e . Based on l o n g term m e t e o r o l o g i c a l r e c o r d s , t h e a d v e r s e l y a f f e c t e d zones a r e s t a t i s t i c a l l y i d e n t i f i e d for potential station s i t e s . INTRODUCTION The s p a t i a l and t e m p o r a l v a r i a t i o n s o f t h e p o l l u t a n t s i n t h e atmosphere caused by t h e e m i s s i o n s o u r c e s , which i s complex and dynamic i n n a t u r e , depend upon t h e m e t e o r o l o g i c a l and t o p o g r a p h i c a l c o n d i t i o n s .

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