View source for Earth:Okhotsk High

The '''Okhotsk High''' is a semi-permanent high pressure system that forms over the Sea of Okhotsk during the summer months.  Its associated air mass is maritime polar, marked with frequent [[Earth:Marine layer|sea fog]] over ocean areas, and cool and moist conditions over land.  It typically dominates the weather pattern over eastern {{wipe|Russia}}, northern {{wipe|Japan}} and the Korean Peninsula during the spring and summer months.

[[Category:Climate patterns]]

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