q The Aleutian, Icelandic, and
Tibetan lows
–The oceanic (continental) lows achieve maximum strength
during winter
(summer) months
–The summertime Tibetan low is important to the east-Asia
monsoon
–
q Siberian, Hawaiian, and
Bermuda-Azores highs
–The oceanic (continental) highs achieve maximum strength
during summer
(winter) months