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bn:00591327n
Noun Named Entity
Categories: Climate of Greenland, Anticyclones, Climate of Canada
EN
North American High
EN
The North American High is an impermanent high-pressure area or anticyclone created by a formative process that occurs when cool or cold dry air settles over North America. Wikipedia
Definitions
Relations
Sources
EN
The North American High is an impermanent high-pressure area or anticyclone created by a formative process that occurs when cool or cold dry air settles over North America. Wikipedia
IS A
anticyclone
center of action
DESCRIBED BY SOURCE
Armenian Soviet Encyclopedia
Wikipedia
EN
North American High
Wikidata
EN
North American High

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