Mount Index is located in the marine west coast climate zone of western North America.4 Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall.5 Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below 0 °F (−18 °C) or above 80 °F (27 °C).6 During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.7 Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.8
"Mount Index". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. https://edits.nationalmap.gov/apps/gaz-domestic/public/search/names/1521160 ↩
"Baring Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. https://edits.nationalmap.gov/apps/gaz-domestic/public/search/names/1516135 ↩
Beckey, Fred W. (2003). Cascade Alpine Guide, Vol. 2, Stevens Pass to Rainy Pass (3rd ed.). Mountaineers Books. p. 41. ISBN 978-0-89886-838-8. 978-0-89886-838-8 ↩
Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. ↩