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