Average Weather in February in Watson Lake Canada
Daily low temperatures increase by 6°F, from -11°F to -5°F, rarely falling below -36°F or exceeding 17°F.
For reference, on July 29, the hottest day of the year, temperatures in Watson Lake typically range from 50°F to 71°F, while on December 31, the coldest day of the year, they range from -15°F to 2°F.
Average High and Low Temperature in February
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on February. The horizontal axis is the day, the vertical axis is the hour of the day, and the color is the average temperature for that hour and day.
Average Hourly Temperature in February
The month of February in Watson Lake experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 72% throughout the month.
The clearest day of the month is February 1, with clear, mostly clear, or partly cloudy conditions 29% of the time.
For reference, on November 28, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 74%, while on August 8, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 45%.
Cloud Cover Categories in February
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Watson Lake, the chance of a wet day over the course of February is decreasing, starting the month at 19% and ending it at 14%.
For reference, the year's highest daily chance of a wet day is 33% on October 9, and its lowest chance is 13% on March 2.
Over the course of February in Watson Lake, the chance of a day with only rain remains an essentially constant 0% throughout, the chance of a day with mixed snow and rain remains an essentially constant 1% throughout, and the chance of a day with only snow decreases from 19% to 12%.
Probability of Precipitation in February
We report snowfall in liquid-equivalent terms. The actual depth of new snowfall is typically between 5 and 10 times the liquid-equivalent amount, assuming the ground is frozen. As with rainfall, we consider the liquid-equivalent snowfall accumulated over a sliding 31-day period centered around each day.
The average sliding 31-day liquid-equivalent snowfall during February in Watson Lake is gradually decreasing, starting the month at 0.8 inches, when it rarely exceeds 1.4 inches or falls below 0.2 inches, and ending the month at 0.5 inches, when it rarely exceeds 1.0 inches or falls below 0.2 inches.
Average Monthly Liquid-Equivalent Snowfall in February
Over the course of February in Watson Lake, the length of the day is very rapidly increasing. From the start to the end of the month, the length of the day increases by 2 hours, 23 minutes, implying an average daily increase of 5 minutes, 19 seconds, and weekly increase of 37 minutes, 11 seconds.
The shortest day of the month is February 1, with 8 hours, 1 minute of daylight and the longest day is February 28, with 10 hours, 25 minutes of daylight.
Hours of Daylight and Twilight in February
The latest sunrise of the month in Watson Lake is 8:48 AM on February 1 and the earliest sunrise is 1 hour, 13 minutes earlier at 7:35 AM on February 28.
The earliest sunset is 4:49 PM on February 1 and the latest sunset is 1 hour, 11 minutes later at 6:00 PM on February 28.
Daylight saving time is observed in Watson Lake during 2018, but it neither starts nor ends during February, so the entire month is in standard time.
For reference, on June 21, the longest day of the year, the Sun rises at 4:09 AM and sets 18 hours, 54 minutes later, at 11:03 PM, while on December 21, the shortest day of the year, it rises at 9:37 AM and sets 5 hours, 51 minutes later, at 3:28 PM.
Sunrise & Sunset with Twilight and Daylight Saving Time in February
We base the humidity comfort level on the dew point, as it determines whether perspiration will evaporate from the skin, thereby cooling the body. Lower dew points feel drier and higher dew points feel more humid. Unlike temperature, which typically varies significantly between night and day, dew point tends to change more slowly, so while the temperature may drop at night, a muggy day is typically followed by a muggy night.
The chance that a given day will be muggy in Watson Lake is essentially constant during February, remaining around 0% throughout.
For reference, on July 18, the muggiest day of the year, there are muggy conditions 0% of the time, while on January 1, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in February
This section discusses the wide-area hourly average wind vector (speed and direction) at 10 meters above the ground. The wind experienced at any given location is highly dependent on local topography and other factors, and instantaneous wind speed and direction vary more widely than hourly averages.
The average hourly wind speed in Watson Lake is essentially constant during February, remaining within 0.1 miles per hour of 3.9 miles per hour throughout.
For reference, on March 16, the windiest day of the year, the daily average wind speed is 4.2 miles per hour, while on July 6, the calmest day of the year, the daily average wind speed is 3.6 miles per hour.
Average Wind Speed in February
Wind Direction in February
Definitions of the growing season vary throughout the world, but for the purposes of this report, we define it as the longest continuous period of non-freezing temperatures (≥ 32°F) in the year (the calendar year in the Northern Hemisphere, or from July 1 until June 30 in the Southern Hemisphere).
The growing season in Watson Lake typically lasts for 3.6 months (109 days), from around May 23 to around September 10, rarely starting before May 8 or after June 8, and rarely ending before August 25 or after September 26.
The month of February in Watson Lake is reliably fully outside of the growing season.
Time Spent in Various Temperature Bands and the Growing Season in February
Growing degree days are a measure of yearly heat accumulation used to predict plant and animal development, and defined as the integral of warmth above a base temperature, discarding any excess above a maximum temperature. In this report, we use a base of 50°F and a cap of 86°F.
The average accumulated growing degree days in Watson Lake are essentially constant during February, remaining around 0°F throughout.
Growing Degree Days in February
This section discusses the total daily incident shortwave solar energy reaching the surface of the ground over a wide area, taking full account of seasonal variations in the length of the day, the elevation of the Sun above the horizon, and absorption by clouds and other atmospheric constituents. Shortwave radiation includes visible light and ultraviolet radiation.
The average daily incident shortwave solar energy in Watson Lake is gradually increasing during February, rising by 1.0 kWh, from 0.7 kWh to 1.6 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in February
For the purposes of this report, the geographical coordinates of Watson Lake are 60.063 deg latitude, -128.709 deg longitude, and 2,290 ft elevation.
The topography within 2 miles of Watson Lake contains significant variations in elevation, with a maximum elevation change of 604 feet and an average elevation above sea level of 2,303 feet. Within 10 miles contains significant variations in elevation (1,834 feet). Within 50 miles contains very significant variations in elevation (5,203 feet).
The area within 2 miles of Watson Lake is covered by trees (84%), within 10 miles by trees (94%), and within 50 miles by trees (91%).
This report illustrates the typical weather in Watson Lake year round, based on a statistical analysis of historical hourly weather reports and model reconstructions from January 1, 1980 to December 31, 2016.
Temperature and Dew Point
There is only a single weather station, Watson Lake, in our network suitable to be used as a proxy for the historical temperature and dew point records of Watson Lake.
At a distance of 8 kilometers from Watson Lake, closer than our threshold of 150 kilometers, this station is deemed sufficiently nearby to be relied upon as our primary source for temperature and dew point records.
The station records are corrected for the elevation difference between the station and Watson Lake according to the International Standard Atmosphere , and by the relative change present in the MERRA-2 satellite-era reanalysis between the two locations.
Please note that the station records themselves may additionally have been back-filled using other nearby stations or the MERRA-2 reanalysis.
All data relating to the Sun's position (e.g., sunrise and sunset) are computed using astronomical formulas from the book, Astronomical Tables of the Sun, Moon and Planets , by Jean Meeus.
All other weather data, including cloud cover, precipitation, wind speed and direction, and solar flux, come from NASA's MERRA-2 Modern-Era Retrospective Analysis . This reanalysis combines a variety of wide-area measurements in a state-of-the-art global meteorological model to reconstruct the hourly history of weather throughout the world on a 50-kilometer grid.
Land Use data comes from the Global Land Cover SHARE database , published by the Food and Agriculture Organization of the United Nations.
Elevation data comes from the Shuttle Radar Topography Mission (SRTM) , published by NASA's Jet Propulsion Laboratory.
Names, locations, and time zones of places and some airports come from the GeoNames Geographical Database .
Time zones for aiports and weather stations are provided by AskGeo.com .
Maps are © Esri, with data from National Geographic, Esri, DeLorme, NAVTEQ, UNEP-WCMC, USGS, NASA, ESA, METI, NRCAN, GEBCO, NOAA, and iPC.
The information on this site is provided as is, without any assurances as to its accuracy or suitability for any purpose. Weather data is prone to errors, outages, and other defects. We assume no responsibility for any decisions made on the basis of the content presented on this site.
We draw particular cautious attention to our reliance on the MERRA-2 model-based reconstructions for a number of important data series. While having the tremendous advantages of temporal and spatial completeness, these reconstructions: (1) are based on computer models that may have model-based errors, (2) are coarsely sampled on a 50 km grid and are therefore unable to reconstruct the local variations of many microclimates, and (3) have particular difficulty with the weather in some coastal areas, especially small islands.
We further caution that our travel scores are only as good as the data that underpin them, that weather conditions at any given location and time are unpredictable and variable, and that the definition of the scores reflects a particular set of preferences that may not agree with those of any particular reader.