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Chinook winds, or simply Chinooks, are two types of prevailing warm, generally westerly winds in western North America: Coastal Chinooks and interior Chinooks. The coastal Chinooks are persistent seasonal, wet, southwesterly winds blowing in from the ocean. The interior Chinooks are occasional warm, dry föhn winds blowing down the eastern sides of interior mountain ranges. The coastal Chinooks were the original term, used along the northwest coast, and the term in the interior of North America is later and derives from the coastal term.

• Along the Pacific Northwest coast, where the name is pronounced ('chin'+'uk'), the name refers to wet, warm winds off the ocean from the southwest; this is the original use of the term. The coastal Chinook winds deliver tremendous amounts of moisture both as rain along the coast and snow in the coastal mountains, that sustain the characteristic temperate rainforests and climate of the Pacific Northwest.

1629 (MDCXXIX) was a common year starting on Monday of the Gregorian calendar and a common year starting on Thursday of the Julian calendar, the 1629th year of the Common Era (CE) and Anno Domini (AD) designations, the 629th year of the 2nd millennium, the 29th year of the 17th century, and the 10th and last year of the 1620s decade. As of the start of 1629, the Gregorian calendar was 10 days ahead of the Julian calendar, which remained in localized use until 1923.