{"id":848,"date":"2024-11-08T11:00:59","date_gmt":"2024-11-08T18:00:59","guid":{"rendered":"https:\/\/blogs.ubc.ca\/michaelpidwirny\/?page_id=848"},"modified":"2025-10-18T09:34:58","modified_gmt":"2025-10-18T16:34:58","slug":"2024-25","status":"publish","type":"page","link":"https:\/\/blogs.ubc.ca\/michaelpidwirny\/2024-25\/","title":{"rendered":"2024\/25 Winter Forecast for Western Canada\u2019s Ski Resorts"},"content":{"rendered":"

by\u00a0MICHAEL PIDWIRNY<\/p>\n

Introduction<\/b><\/span><\/h4>\n

During the winter months of December, January, and February, the climate of the northwest USA and southern British Columbia is defined by cooling temperatures and increased precipitation. Temperatures cool mainly because of the Sun’s reduced heat energy. During these months, the intensity of the solar radiant energy declines because of lower Sun angles and a shortening of day length.<\/span> Figure 1<\/strong><\/span> describes the winter season’s average near-surface temperature (2 meters above ground level). Temperatures along the west coast are moderated by the stored heat energy found in the waters of the Pacific Ocean.<\/span><\/p>\n

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Figure 1<\/strong><\/span>. Average winter precipitation over the North American continent and the adjacent oceans from 1981-2010. Source: Climate Reanalyzer – https:\/\/climatereanalyzer.org<\/a>.<\/p><\/div>\n

Figure 2<\/strong><\/span> describes the typical patterns of winter precipitation in North America. High amounts of precipitation occur along much of the West Coast because of the interaction between mid-latitude cyclones and orographic uplift. During winter, mid-latitude cyclones often originate in the northeastern Pacific Ocean and then move in an easterly direction. Orographic enhancement of the quantity of precipitation falling from these storm systems occurs because of mountains running from Alaska to California. Central North America is relatively dry compared to the West Coast because most of the precipitable water held in the clouds of the mid-latitude cyclones previously precipitated out, and the cold continental air masses frequently found here retain little moisture.<\/span><\/p>\n

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Figure 2<\/strong><\/span>. Average winter precipitation over the North American continent\u00a0and the adjacent oceans for the period 1981-2010. Source: Climate Reanalyzer – https:\/\/climatereanalyzer.org<\/a>.<\/p><\/div>\n

Variation in year-to-year winter weather of the northwest USA and southern British Columbia is strongly influenced by several large-scale cyclic climate phenomena which modify large-scale atmospheric circulation and sea surface temperatures in the Pacific Ocean. Further, these climate factors significantly impact temperature and precipitation trends during the winter months over southern British Columbia and Washington state. Seesawing on a time scale of a few years are El Ni\u00f1o and La Ni\u00f1a events located along the tropical Pacific Ocean. El Ni\u00f1o<\/strong><\/a>\u00a0– usually brings warmer-than-average winters and below-average precipitation to this area of the Pacific Northwest. La Ni\u00f1a<\/strong><\/a>\u00a0– is often associated with cold winters with average to above-normal precipitation. Generally, the effects of significant El Ni\u00f1o and La Ni\u00f1a are limited to one or maybe two consecutive winter seasons. Operating on a much longer timescale of one to three decades is another cyclic climate factor of importance known as the Pacific Decadal Oscillation<\/strong><\/a>. The Pacific Decadal Oscillation alternates between a warm or a cold state, and these states seem to amplify the climatic effects of co-occurring El Ni\u00f1o and La Ni\u00f1a events, respectively.<\/span><\/p>\n

El Ni\u00f1o<\/strong><\/span><\/h4>\n

El Ni\u00f1o<\/strong><\/a>\u00a0is the name given to the cyclical development of warm ocean surface waters on the east side of the Pacific Ocean at the equator. This climate event usually occurs around Christmas and usually lasts for a few weeks (weak) to a few months (strong). El Ni\u00f1o is created by a reduction in the speed of the Trade Winds right along the equator, which results in a shift in atmospheric circulation and pressure patterns in this region of the planet (Figure 3<\/strong><\/span>). Sometimes, an extremely warm El Ni\u00f1o can develop and last for more than a year. Since 1935, significant El Ni\u00f1o events have formed in 1958, 1966, 1978, 1983, 1987, 1990, 1992, 1993, 1998, 2005, 2010, 2016, and 2024. Figure 4 <\/strong><\/span>shows the general global patterns of winter surface temperature warming and cooling associated with El Ni\u00f1o.<\/span><\/p>\n

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Figure 3<\/strong><\/span>. Cross-section along the Pacific Ocean at the equator during an El Ni\u00f1o event. Notice associated atmospheric circulation patterns and the direction of warm seawater pulse in the ocean.<\/p><\/div>\n

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Figure 4<\/strong>.<\/span><\/span> The December to February near-surface temperature anomaly is based on the average of twelve El Ni\u00f1o years relative to the 1981-2010 average.<\/p><\/div>\n

La Ni\u00f1a<\/strong><\/span><\/h4>\n

La Ni\u00f1a <\/strong><\/a>is the name given to the cyclical development of cold ocean surface waters on the east side of the Pacific Ocean at the equator. Like El Ni\u00f1o, a La Ni\u00f1a climate event usually occurs around Christmas and lasts typically for a few weeks (weak) to a few months (strong). La Ni\u00f1a is created by an increase in the speed of the Trade Winds along the equator, which results in a shift in atmospheric circulation and pressure patterns in this region of the planet (Figure 5<\/strong><\/span>). Sometimes, an extremely cold La Ni\u00f1a can develop and last for more than a year. Since 1935, significant La Ni\u00f1as have occurred in 1950, 1956, 1967, 1971, 1974, 1976, 1999, 2008, 2011, and 2021. Figure 6<\/strong><\/span> shows the general global patterns of winter surface temperature cooling and warming associated with La Ni\u00f1a.<\/span><\/p>\n

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Figure 5<\/strong><\/span>. Cross-section along the Pacific Ocean at the equator during a La Ni\u00f1a event. Notice associated atmospheric circulation patterns and the direction of cold seawater pulse in the ocean.<\/p><\/div>\n

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Figure 6<\/strong><\/span>. December to February near-surface temperature anomaly based on the average of ten La Ni\u00f1a years relative to the 1981-2010 normal average.<\/p><\/div>\n

Figure 7 <\/strong><\/span>shows the relative strength of El Ni\u00f1o and La Ni\u00f1a events from 1930 to March 2022, according to the Southern Oscillation Index (SOI)<\/strong><\/a>. In this figure, negative values indicate El Ni\u00f1o conditions, with lower values suggesting stronger events. High positive values indicate significant La Ni\u00f1a eve<\/span>nts.<\/p>\n

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Figure 7<\/strong><\/span>. Relative strength El Ni\u00f1o and La Ni\u00f1a events from January 1930 to March 2024. Red indicates the El Ni\u00f1o event, while blue identifies the La Ni\u00f1a event. Data Source: National Center for Atmospheric Research<\/a>.<\/p><\/div>\n

The Pacific Decadal Oscillation<\/span><\/strong><\/h4>\n

The Pacific Decadal Oscillation<\/strong><\/a> (PDO) is a cyclical ocean-atmosphere climate variability pattern in the North Pacific Ocean. The PDO is detected as a change in sea surface temperatures over the Pacific Ocean from 20 to 60\u00b0 North latitude. There are two phases that can last many years to several decades, as shown in\u00a0Figure 8<\/strong><\/span>. During the warm<\/strong> or positive phase<\/strong>, sea surface temperatures in the western North Pacific Ocean become cooler, while the eastern side of this ocean warms (Figure 9<\/strong><\/span>). The warm phase results in a zone of warm seawater hugging the west coast of North America from Alaska down to the Baja Peninsula. During the cold<\/strong> or negative phase<\/strong>, sea surface temperatures in the western North Pacific Ocean become warmer, while the eastern part of this ocean cools down (Figure 10<\/strong><\/span>). Significant reversals in the prevailing phase of the PDO have occurred around 1956, 1960, 1976, 1997, 2013, and 2019 (Figure 8<\/strong><\/span>).<\/span><\/p>\n

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Figure 8<\/strong><\/span>. Relative strength and phase of the monthly Pacific Decadal Oscillation (PDO) Index from January 1950 to September 2024. Moving average produced by loess smoothing. Values above zero indicate the warm or positive phase (red) of the PDO, while values below zero identify the cold or negative phase (blue). Data Source: Japan Meteorological Agency<\/a>.<\/p><\/div>\n

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Figure 9<\/strong><\/span>. Surface temperature effects of the warm (positive) phase of the Pacific Decadal Oscillation during the winter season (December, January, and February) for the North American continent and the Pacific Ocean. This map describes the average temperature anomaly of nine significant warm episode years to the 30-year average 1981-2010.<\/p><\/div>\n

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Figure 10<\/strong><\/span>. Surface temperature effects of the cold (negative) phase of the Pacific Decadal Oscillation during the winter season (December, January, and February) for the North American continent and the Pacific Ocean. This map describes the average temperature anomaly of fourteen significant cold episode years to the 30-year average 1981-2010.<\/p><\/div>\n

<\/h4>\n

Forecast Winter 2024\/25<\/span><\/strong><\/h4>\n

Weak La Ni\u00f1a conditions are now observed over the equatorial Pacific (Figure 11<\/strong><\/span>). Computer models suggest weak La Ni\u00f1a conditions will continue from January to March 2025.<\/span><\/p>\n

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Figure 11<\/strong><\/span>. Pacific Ocean sea surface temperature anomalies for November 6, 2024. In this image, black represents a temperature no different than the 1981-2010 thirty-year average. Red to yellow indicates an above-normal temperature anomaly. Blue to light blue indicates a below-normal temperature anomaly. Weak\u00a0La Ni\u00f1a<\/span> conditions are now observable along the equatorial Pacific. Also, an extensive area of cooler-than-average sea surface temperatures exists off the west coast of Canada. This pattern usually occurs when PDO is in its negative phase. (Image Source: https:\/\/earth.nullschool.net<\/a>).<\/span><\/p><\/div>\n

The Pacific Decadal Oscillation (PDO) index from January 2018 to September 20241 is shown in Figure 12<\/strong><\/span>\u00a0(and see web page<\/span>\u00a0Monthly PDO Index<\/a><\/strong>). From the summer of 2018 until fall 2019 the monthly PDO index rose from near zero to around +1.0. A sudden decline into negative territory occurred in October 2019, then a rebound to higher values in November and December, and mainly negative values from January 2020 to September 2024.\u00a0<\/span><\/p>\n

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Figure 12<\/strong><\/span>. Relative strength and phase of the monthly Pacific Decadal Oscillation (PDO) Index from January 2010 to September 2024. Values above zero indicate warm or positive phase, while values below zero identify cold or negative phase.<\/p><\/div>\n

In conclusion, current patterns associated with La Ni\u00f1a and the Pacific Decadal Oscillation suggest that the climate of the winter of 2024\/25 will be colder than normal, with higher than average precipitation for southern British Columbia and western Alberta.<\/span><\/p>\n

 <\/p>\n

Climate Prediction Center – North American Multi-Model Ensemble Long-Range Monthly Forecasts – November 2024<\/span><\/h4>\n

There is one more critical piece of information that can provide insight into what the winter season will be like in the Pacific Northwest USA and southern British Columbia in 2024\/25. National Oceanic and Atmospheric Administration’s<\/span> Climate Prediction Center<\/a> <\/strong>creates long-range seasonal forecasts based on the average of seven different General Circulation Model simulations. Figure 13<\/strong><\/span> describes the November surface mean temperature forecast for North America released in October 2024. This forecast suggests temperatures will be 0.5 to 2.0\u00b0C above-normal for British Columbia, Alberta, Washington state, eastern Oregon, Idaho, Montana, Utah, and Colorado.<\/span><\/p>\n

 <\/p>\n

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Figure 13<\/strong><\/span>. Climate Prediction Center – North American Multi-Model Ensemble temperature forecast for November 2024. October 2024 model run. Shown is the forecasted precipitation anomaly relative to the 1981-2010 thirty-year average.<\/p><\/div>\n

Figure\u00a0<\/strong>14<\/strong><\/span> describes the November precipitation forecast for North America from the Climate Prediction Center released in October 2024. This forecast suggests well above-normal precipitation for southern British Columbia and western Washington State. California, southern Oregon, Idaho, and southern Montana will see below-normal precipitation.<\/span><\/p>\n

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Figure 14<\/strong><\/span>. Climate Prediction Center – North American Multi-Model Ensemble precipitation forecast for November 2024. October 2024 model run. Shown is the forecasted precipitation anomaly relative to the 1981-2010 thirty-year average.<\/p><\/div>\n

<\/div>\n

Climate Prediction Center – North American Multi-Model Ensemble Long-Range Seasonal Forecasts – December \u00a02024\u00a0<\/span><\/h4>\n

Figures 15<\/strong><\/span>\u00a0and 16\u00a0<\/strong><\/span>describe December 2024 forecasts of surface mean temperature and precipition for North America released in November 2024. The December forecast suggests near-normal temperatures for southern British Columbia, western Alberta, Washington State, and Oregon (Figure 15<\/strong><\/span>). While Montana, Idaho, California, Utah, Arizona, New Mexico, and Colorado will see above-normal temperatures.<\/span><\/p>\n

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Figure 15<\/strong><\/span>. Climate Prediction Center – North American Multi-Model Ensemble surface temperature forecast for December 2024. November 2024 model run. The forecasted temperature anomaly is shown relative to the thirty-year average for 1981-2010.<\/p><\/div>\n

Above-normal precipitation is forecasted for December for most of British Columbia, Washington State, northern Idaho, and Oregon north (Figure 16<\/strong><\/span>). While California, Utah, Arizona, New Mexico, and Colorado will see below-normal precipitation.<\/span><\/p>\n

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Figure 16<\/strong><\/span>. Climate Prediction Center – North American Multi-Model Ensemble precipitation forecast for December 2024. November 2024 model run. The forecasted precipitation rate anomaly is shown relative to the 1981-2010 thirty-year average.<\/p><\/div>\n

 <\/p>\n

Climate Prediction Center – North American Multi-Model Ensemble Long-Range Seasonal Forecasts – January \u00a02025\u00a0<\/span><\/h4>\n

The January 2025 forecast suggests temperatures will be normal for southern British Columbia and western Alberta (Figure 17<\/strong><\/span>). Washington State, Montana, Oregon, California, Idaho, Wyoming, Utah, Nevada, New Mexico, and Colorado will see above-normal temperatures.<\/span><\/p>\n

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Figure 17<\/strong><\/span>. Climate Prediction Center – North American Multi-Model Ensemble surface temperature forecast for January 2025. December 2024 model run. Shown is the forecasted temperature anomaly relative to the 1981-2010 thirty-year average.<\/p><\/div>\n

Figure <\/strong><\/span>18\u00a0<\/strong><\/span>describes the January 2025 precipitation rate forecasts for North America, released in December 2024. The January forecast suggests precipitation will be above-normal for British Columbia, Alberta, Washington state, northern Oregon, northern Idaho, and western Montana. Below-normal precipitation will occur in California, Arizona, southern Nevada, southern Utah, and most of New Mexico.\u00a0<\/span><\/p>\n

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Figure 18<\/strong><\/span>. Climate Prediction Center – North American Multi-Model Ensemble precipitation forecast for January 2025. December 2024 model run. Shown is the forecasted precipitation rate anomaly relative to the 1981-2010 thirty-year average.<\/p><\/div>\n

<\/h3>\n

Climate Prediction Center – North American Multi-Model Ensemble Long-Range Seasonal Forecasts – February \u00a02025\u00a0<\/span><\/h4>\n

The February 2025 forecast suggests temperatures will be below-average for British Columbia, Alberta, Washington State, western Oregon, and northern Montana (Figure 18<\/strong><\/span>). Above-normal temperatures will be seen in southern California, south Idaho, southern Wyoming, Colorado, Nevada, Utah, Arizona, and New Mexico.<\/span><\/p>\n

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Figure <\/strong><\/span>19 <\/strong><\/span>describes North America’s February 2025 precipitation forecasts, released in December 2024. The February forecast suggests precipitation will be above-normal for southern Alberta, south-eastern British Columbia, Washington State, Oregon, Idaho, western Wyoming, western Colorado, and Montana. Below-normal precipitation will occur in southern California, southern Nevada, Arizona, and New Mexico. Elsewhere, precipitation conditions will be near normal.<\/span><\/p>\n

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Figure 19<\/strong><\/span>. Climate Prediction Center – North American Multi-Model Ensemble precipitation forecast for February 2025. December 2024 model run. Shown is the forecasted precipitation rate anomaly relative to the 1981-2010 thirty-year average.<\/p><\/div>\n

 <\/p>\n

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by\u00a0MICHAEL PIDWIRNY Introduction During the winter months of December, January, and February, the climate of the northwest USA and southern British Columbia is defined by cooling temperatures and increased precipitation. Temperatures cool mainly because of the Sun’s reduced heat energy. During these months, the intensity of the solar radiant energy declines because of lower Sun […]<\/p>\n","protected":false},"author":43164,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-848","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/blogs.ubc.ca\/michaelpidwirny\/wp-json\/wp\/v2\/pages\/848","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.ubc.ca\/michaelpidwirny\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/blogs.ubc.ca\/michaelpidwirny\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.ubc.ca\/michaelpidwirny\/wp-json\/wp\/v2\/users\/43164"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.ubc.ca\/michaelpidwirny\/wp-json\/wp\/v2\/comments?post=848"}],"version-history":[{"count":89,"href":"https:\/\/blogs.ubc.ca\/michaelpidwirny\/wp-json\/wp\/v2\/pages\/848\/revisions"}],"predecessor-version":[{"id":1034,"href":"https:\/\/blogs.ubc.ca\/michaelpidwirny\/wp-json\/wp\/v2\/pages\/848\/revisions\/1034"}],"wp:attachment":[{"href":"https:\/\/blogs.ubc.ca\/michaelpidwirny\/wp-json\/wp\/v2\/media?parent=848"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}