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Chinook winds //, or simply Chinooks, are föhn winds in the interior West of North America, where the Canadian Prairies and Great Plains meet various mountain ranges, although the original usage is in reference to wet, warm coastal winds in the Pacific Northwest.
Chinook is claimed[by whom?] by popular folk-etymology to mean ‘ice-eater’, however it is the name of the people in the region where the usage was first derived. The reference to a wind or weather system, simply ‘a Chinook’, originally meant[by whom?] a warming wind from the ocean into the interior regions of the Pacific Northwest of the USA (the Chinook people lived near the ocean, along the lower Columbia River).
A strong föhn wind can make snow one foot (30 cm) deep almost vanish in one day. The snow partly melts and partly sublimates in the dry wind. Chinook winds have been observed to raise winter temperature, often from below −20 °C (−4 °F) to as high as 10–20 °C (50–68 °F) for a few hours or days, then temperatures plummet to their base levels. The greatest recorded temperature change in 24 hours was caused by Chinook winds on 15 January 1972, in Loma, Montana; the temperature rose from −48 to +9 °C (−54 to +49 °F).
Chinooks are most prevalent over southern Alberta in Canada, especially in a belt from Pincher Creek and Crowsnest Pass through Lethbridge, which get 30–35 Chinook days per year, on average. Chinooks become less frequent further south in the United States, and are not as common north of Red Deer, but they can and do occur annually as far north as High Level in northwestern Alberta and Fort St. John in northeastern British Columbia, and as far south as Las Vegas and occasionally to Carlsbad, both in eastern New Mexico.
In southwestern Alberta, Chinook winds can gust in excess of hurricane force 120 km/h (75 mph). On 19–November 1962, an especially powerful Chinook in Lethbridge gusted to 171 km/h (106 mph).
In Pincher Creek, the temperature rose by 41 °C (74 °F), from −19 to 22 °C (−2 to 72 °F), in one hour in 1962. Trains have been known to be derailed by Chinook winds. During the winter, driving can be treacherous, as the wind blows snow across roadways, sometimes causing roads to vanish and snowdrifts to pile up higher than a metre. Empty semitrailer trucks driving along Highway 3 and other routes in southern Alberta have been blown over by the high gusts of wind caused by Chinooks.
On 27 February 1992, Claresholm, Alberta a small city just south of Calgary; recorded a temperature of 24 °C (75 °F) again the next day 21 °C (70 °F) was recorded. These are some of Canada's highest February temperatures.
The Chinook can seem to do battle with the Arctic air mass at times. It is not unheard of for people in Lethbridge to complain of −20 °C (−4 °F) temperatures while those in Cardston, just 77 km (48 mi) down the road, enjoy 10 °C (50 °F) temperatures. This clash of temperatures can remain stationary, or move back and forth, in the latter case causing such fluctuations as a warm morning, a bitterly cold afternoon, and a warm evening. A curtain of fog often accompanies the clash between warm to the west and cold to the east.
One of its most striking features is the Chinook arch, a föhn cloud in the form of a band of stationary stratus clouds caused by air rippling over the mountains due to orographic lifting. To those unfamiliar with it, the Chinook arch may look like a threatening storm cloud at times. However, they rarely produce rain or snow. They can also create stunning sunrises and sunsets.
The stunning colours seen in the Chinook arch are quite common. Typically, the colours will change throughout the day, starting with yellow, orange, red and pink shades in the morning as the sun comes up, grey shades at midday changing to pink / red colours, and then orange / yellow hues just before the sun sets.
The Chinook is a föhn wind, a rain shadow wind which results from the subsequent adiabatic warming of air which has dropped most of its moisture on windward slopes (orographic lift). As a consequence of the different adiabatic rates of moist and dry air, the air on the leeward slopes becomes warmer than equivalent elevations on the windward slopes.
As moist winds from the Pacific (also called “Chinooks”) are forced to rise over the mountains, the moisture in the air is condensed and falls out as precipitation, while the air cools at the moist adiabatic rate of 5 °C / 1000 m (3.5 °F / 1000 ft). The dried air then descends on the leeward side of the mountains, warming at the dry adiabatic rate of 10 °C / 1000 m (5.5 °F / 1000 ft).
Quite often, when the Pacific Northwest coast is being drenched by rain, the windward side of the Rockies is being hammered by snow (as the air loses its moisture), and the leeward side of the Rockies in Alberta is basking in a föhn Chinook. The three different weather conditions are all caused by the same flow of air, hence the confusion over the use of the name “Chinook wind”.
Two common cloud patterns seen during this time are a chinook arch overhead, and a bank of clouds (also referred to as a cloud wall) obscuring the mountains to the west. It appears to be an approaching storm, but does not advance any further east.
Often, a Chinook is preceded by a “Manyberries Chinook” during the end of a cold spell. This southeast wind was named for the small village Manyberries, now a hamlet, in southeastern Alberta, from where the wind seems to originate. It can be fairly strong and cause bitter windchill and blowing snow. The wind will eventually swing around to the southwest and the temperature rises sharply as the real Chinook arrives.
The term Chinook wind is also used in British Columbia, and is the original usage, being rooted in the lore of coastal tribes and brought to Alberta by the fur-traders. Such winds are extremely wet and warm and arrive off the western coast of North America from the southwest. The winds are also known as the pineapple express, since they are of tropical origin, roughly from the area of the Pacific near Hawaii. The air associated with a west coast Chinook is stable; this minimizes wind gusts and often keeps winds light in sheltered areas. In exposed areas, fresh gales are frequent during a Chinook, but strong gale- or storm-force winds are uncommon (most of the region’s stormy winds come when a fast ‘westerly’ jet stream lets air masses from temperate and subarctic latitudes clash).
When a Chinook comes in when an Arctic air mass is holding steady over the coast, the tropical dampness brought in suddenly cools, penetrating the frozen air and coming down in volumes of powder snow, sometimes to sea level. Snowfalls and the cold spells that spawned them only last a few days during a Chinook; as the warm Chinooks blow from the southwest, they push back east the cold Arctic air. The snow melts quickly and is gone within a week.
The effects on the Interior of British Columbia when a Chinook is in effect are the reverse. In a rainy spell, most of the heavy moisture will be soaked out by the ramparts of mountains before the air mass reaches the Fraser Canyon and the Thompson River-Okanagan area. The effects are similar to those of an Alberta Chinook, though not to the same extreme, in part because the Okanagan is relatively warmer than the Prairies, and because of the additional number of precipitation-catching mountain ranges between Kelowna and Calgary. When the Chinook brings snow to the coast during a period of coastal cold, bright but chilly weather in the interior will give way to a slushy melting of snow, more due to the warm spell than because of rain.
The resulting outflow wind is more or less the opposite of British Columbia / Pacific Northwest Chinook. These are called a squamish in certain areas, rooted in the direction of such winds coming down out of Howe Sound, home to the Squamish people, and in Alaska are called a williwaw. They consist of cold airstreams from the continental air mass pouring out of the interior plateau via certain river valleys and canyons penetrating the Coast Mountains towards the coast.
The word “Chinook” is in common usage among local fishermen and people in communities along the British Columbia Coast and coastal Washington and Oregon. The term is also used in the Puget Sound area of Washington. “Chinook” is not pronounced as it is east of the Cascades – shinook – but is in the original coastal pronunciation tshinook.
In British Columbia and other parts of the Pacific Northwest, the word Chinook was once often pronounced // chi-NUUK. Currently, the common pronunciation throughout most of the Pacific Northwest, Alberta, and the rest of Canada, is // shi-NUUK, as in French. This difference may be because it was the Métis employees of the Hudson's Bay Company, who were familiar with the Chinook people and country, brought the name east of the Cascades and Rockies, along with their own ethnified pronunciation. Early records are clear that tshinook was the original pronunciation, before the word’s transmission east of the Rockies.
Native legend of the Lil'wat subgroup of the St'at'imc tells of a girl named Chinook-Wind, who married Glacier, and moved to his country, which was in the area of today's Birkenhead River. She pined for her warm sea-home in the southwest, and sent a message to her people. They came to her in a vision in the form of snowflakes, and told her they were coming to get her. They came in great number and quarrelled with Glacier over her, but they overwhelmed him and she went home with them in the end.
While on the one hand this tale tells a tribal family-relations story, and family/tribal history as well, it also seems to be a parable of a typical weather pattern of a southwesterly wind at first bringing snow, then rain, and also of the melting of a glacier, namely the Place Glacier near Gates Lake at Birken. Thus, it also tells of a migration of people to the area – or a war, depending on how the details of the legend might be read, with Chinook-Wind taking the part of Helen in a First Nations parallel to the Trojan War.
The frequent midwinter thaws in Great Plains Chinook country are more of a bane than a blessing to gardeners. Plants can be visibly brought out of dormancy by persistent Chinook winds, or have their hardiness reduced even if they appear to be remaining dormant. In either case, they become vulnerable to later cold waves. Many plants which do well at Winnipeg (where constant cold maintains dormancy all winter) are difficult to grow in the Alberta Chinook belt; examples include basswood, some apple, raspberry and Saskatoon varieties, and Amur maples. Trees in the Chinook-affected areas of Alberta are known to be small, with much less growth than trees in areas not affected by Chinooks. This is once again caused by the ‘off-and-on’ dormancy throughout winter.
Chinook winds are said to sometimes cause a sharp increase in the number of migraine headaches suffered by the locals. At least one study conducted by the department of clinical neurosciences at the University of Calgary supports that belief. They are popularly[clarification needed] believed[by whom?] to increase irritability and sleeplessness. In mid-winter over major centres such as Calgary, Chinooks can often override cold air in the city, trapping the pollutants in the cold air and causing inversion smog. At such times, it is possible for it to be cold at street level and much warmer at the tops of the skyscrapers and in higher terrain. In 1983, on the 45th floor [about 145 m (460 ft) above the street] of the Petro-Canada Center, carpenters worked shirtless in +12 °C, windy conditions (temperature reported to them by overhead crane operator), but were chagrined to find out the street temperature was still −20 °C as they left work at 3:30 that afternoon.
Loma, Montana, boasts having the most extreme recorded temperature change in a 24-hour period. On 15 January 1972, the temperature rose from −54 °F to 49 °F (−48 °C to 9 °C), a 103 °F (58 °C) change in temperature, a dramatic example of the regional Chinook wind in action.
The Black Hills of South Dakota are home to the world's fastest recorded rise in temperature. On 22 January 1943, at about 7:30 am MST, the temperature in Spearfish, South Dakota, was −4 °F (−20 °C). The Chinook kicked in, and two minutes later, the temperature was 45 °F (7 °C). The 49 °F (27 °C) rise set a world record, yet to be exceeded. By 9:00 am, the temperature had risen to 54 °F (12 °C). Suddenly, the Chinook died down and the temperature tumbled back to −4°F (−20 °C). The 58 °F (32 °C) drop took only 27 minutes.
The aforementioned 107 mph (172 km/h) wind in Alberta and other local wind records west of the 100th meridian on the Great Plains of the United States and Canada, as well as instances of the record high and low temperature for a given day of the year being set on the same date, are largely the result of these winds.
On rare occasions, Chinook winds generated on the eastern slope of the Rocky Mountains have reached as far east as Wisconsin.
Chinooks are generally called föhn winds by meteorologists and climatologists, and, regardless of name, can occur in most places on the leeward side of a nearby mountain range. They are called “Chinook winds” throughout most of inland western North America, particularly the Rocky Mountain region. Montana, in particular, has a significant amount of föhn winds across much of the state during the winter months, but particularly coming off the Rocky Mountain Front in the northern and west-central areas of the state.
One such wind occurs in the Cook Inlet region in Alaska as air moves over the Chugach Mountains between Prince William Sound and Portage Glacier. Anchorage residents often believe the warm winds which melt snow and leave their streets slushy and muddy are a midwinter gift from Hawaii, following a common mistake that the warm winds come from the same place as the similar winds near the coasts in southern British Columbia, Washington, and Oregon.