Average Weather at Creston Automatic Weather Reporting System Canada
At Creston Automatic Weather Reporting System, the summers are short, warm, dry, and partly cloudy and the winters are freezing and mostly cloudy. Over the course of the year, the temperature typically varies from 21°F to 85°F and is rarely below 3°F or above 94°F.
Based on the tourism score, the best time of year to visit Creston Automatic Weather Reporting System for warm-weather activities is from mid July to mid August.
The warm season lasts for 2.8 months, from June 17 to September 10, with an average daily high temperature above 74°F. The hottest day of the year is August 3, with an average high of 85°F and low of 59°F.
The cold season lasts for 3.5 months, from November 12 to February 26, with an average daily high temperature below 42°F. The coldest day of the year is January 1, with an average low of 21°F and high of 31°F.
Average High and Low Temperature
The figure below shows you a compact characterization of the entire year of hourly average temperatures. The horizontal axis is the day of the year, the vertical axis is the hour of the day, and the color is the average temperature for that hour and day.
Average Hourly Temperature
Salgótarján, Hungary (5,239 miles away) and Chiprovtsi, Bulgaria (5,597 miles) are the far-away foreign places with temperatures most similar to Creston Automatic Weather Reporting System (view comparison).
At Creston Automatic Weather Reporting System, the average percentage of the sky covered by clouds experiences significant seasonal variation over the course of the year.
The clearer part of the year at Creston Automatic Weather Reporting System begins around June 15 and lasts for 3.8 months, ending around October 8. On August 2, the clearest day of the year, the sky is clear, mostly clear, or partly cloudy 75% of the time, and overcast or mostly cloudy 25% of the time.
The cloudier part of the year begins around October 8 and lasts for 8.2 months, ending around June 15. On January 10, the cloudiest day of the year, the sky is overcast or mostly cloudy 74% of the time, and clear, mostly clear, or partly cloudy 26% of the time.
Cloud Cover Categories
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. The chance of wet days at Creston Automatic Weather Reporting System varies throughout the year.
The wetter season lasts 8.5 months, from October 18 to July 1, with a greater than 25% chance of a given day being a wet day. The chance of a wet day peaks at 37% on November 21.
The drier season lasts 3.5 months, from July 1 to October 18. The smallest chance of a wet day is 13% on August 2.
Among wet days, we distinguish between those that experience rain alone, snow alone, or a mixture of the two. Based on this categorization, the most common form of precipitation at Creston Automatic Weather Reporting System changes throughout the year.
Rain alone is the most common for 12 months, from January 3 to December 25. The highest chance of a day with rain alone is 36% on June 4.
Snow alone is the most common for 1.3 weeks, from December 25 to January 3. The highest chance of a day with snow alone is 13% on December 27.
Daily Chance of Precipitation
To show variation within the months and not just the monthly totals, we show the rainfall accumulated over a sliding 31-day period centered around each day of the year. Creston Automatic Weather Reporting System experiences some seasonal variation in monthly rainfall.
Rain falls throughout the year at Creston Automatic Weather Reporting System. The most rain falls during the 31 days centered around November 18, with an average total accumulation of 2.5 inches.
The least rain falls around August 7, with an average total accumulation of 0.7 inches.
Average Monthly Rainfall
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. Colder, drier snow tends to be on the higher end of that range and warmer, wetter snow on the lower end.
As with rainfall, we consider the snowfall accumulated over a sliding 31-day period centered around each day of the year. Creston Automatic Weather Reporting System experiences some seasonal variation in monthly liquid-equivalent snowfall.
The snowy period of the year lasts for 4.9 months, from October 28 to March 23, with a sliding 31-day liquid-equivalent snowfall of at least 0.1 inches. The most snow falls during the 31 days centered around December 28, with an average total liquid-equivalent accumulation of 0.8 inches.
The snowless period of the year lasts for 7.1 months, from March 23 to October 28. The least snow falls around July 24, with an average total liquid-equivalent accumulation of 0.0 inches.
Average Liquid-Equivalent Monthly Snowfall
The length of the day at Creston Automatic Weather Reporting System varies extremely over the course of the year. In 2017, the shortest day is December 21, with 8 hours, 13 minutes of daylight; the longest day is June 20, with 16 hours, 13 minutes of daylight.
Hours of Daylight and Twilight
The earliest sunrise is at 4:40 AM on June 16, and the latest sunrise is 3 hours, 60 minutes later at 8:40 AM on December 31. The earliest sunset is at 4:48 PM on December 11, and the latest sunset is 4 hours, 7 minutes later at 8:54 PM on June 24.
Daylight saving time (DST) is not observed at Creston Automatic Weather Reporting System during 2017.
Sunrise & Sunset with Twilight
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 perceived humidity level at Creston Automatic Weather Reporting System, as measured by the percentage of time in which the humidity comfort level is muggy, oppressive, or miserable, does not vary significantly over the course of the year, staying within 1% of 1% throughout.
Humidity Comfort Levels
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 at Creston Automatic Weather Reporting System does not vary significantly over the course of the year, remaining within 0.3 miles per hour of 3.6 miles per hour throughout.
Average Wind Speed
The predominant average hourly wind direction at Creston Automatic Weather Reporting System is from the west throughout the year.
Best Time of Year to Visit
To characterize how pleasant the weather is at Creston Automatic Weather Reporting System throughout the year, we compute two travel scores.
The tourism score favors clear, rainless days with perceived temperatures between 65°F and 80°F. Based on this score, the best time of year to visit Creston Automatic Weather Reporting System for general outdoor tourist activities is from mid July to mid August, with a peak score in the first week of August.
The beach/pool score favors clear, rainless days with perceived temperatures between 75°F and 90°F. Based on this score, the best time of year to visit Creston Automatic Weather Reporting System for hot-weather activities is from mid July to mid August, with a peak score in the first week of August.
For each hour between 8:00 AM and 9:00 PM of each day in the analysis period (1980 to 2016), independent scores are computed for perceived temperature, cloud cover, and total precipitation. Those scores are combined into a single hourly composite score, which is then aggregated into days, averaged over all the years in the analysis period, and smoothed.
Our cloud cover score is 10 for fully clear skies, falling linearly to 9 for mostly clear skies, and to 1 for fully overcast skies.
Our precipitation score, which is based on the three-hour precipitation centered on the hour in question, is 10 for no precipitation, falling linearly to 9 for trace precipitation, and to 0 for 0.04 inches of precipitation or more.
Our tourism temperature score is 0 for perceived temperatures below 50°F, rising linearly to 9 for 65°F, to 10 for 75°F, falling linearly to 9 for 80°F, and to 1 for 90°F or hotter.
Our beach/pool temperature score is 0 for perceived temperatures below 65°F, rising linearly to 9 for 75°F, to 10 for 82°F, falling linearly to 9 for 90°F, and to 1 for 100°F or hotter.
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 at Creston Automatic Weather Reporting System typically lasts for 6.0 months (182 days), from around April 17 to around October 16, rarely starting before March 26 or after May 12, and rarely ending before September 26 or after November 5.
Time Spent in Various Temperature Bands and the Growing Season
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.
Based on growing degree days alone, the first spring blooms at Creston Automatic Weather Reporting System should appear around May 1, only rarely appearing before April 20 or after May 13.
Growing Degree Days
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 experiences extreme seasonal variation over the course of the year.
The brighter period of the year lasts for 3.3 months, from May 11 to August 20, with an average daily incident shortwave energy per square meter above 6.0 kWh. The brightest day of the year is July 15, with an average of 7.3 kWh.
The darker period of the year lasts for 3.8 months, from October 24 to February 16, with an average daily incident shortwave energy per square meter below 2.2 kWh. The darkest day of the year is December 24, with an average of 1.0 kWh.
Average Daily Incident Shortwave Solar Energy
For the purposes of this report, the geographical coordinates of Creston Automatic Weather Reporting System are 49.083 deg latitude, -116.500 deg longitude, and 2,044 ft elevation.
The topography within 2 miles of Creston Automatic Weather Reporting System contains very significant variations in elevation, with a maximum elevation change of 1,693 feet and an average elevation above sea level of 2,023 feet. Within 10 miles contains very significant variations in elevation (5,364 feet). Within 50 miles also contains extreme variations in elevation (7,949 feet).
The area within 2 miles of Creston Automatic Weather Reporting System is covered by sparse vegetation (33%), trees (28%), cropland (14%), and shrubs (13%), within 10 miles by trees (66%) and sparse vegetation (13%), and within 50 miles by trees (76%) and shrubs (11%).
This report illustrates the typical weather at Creston Automatic Weather Reporting System, 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
Creston Automatic Weather Reporting System has a weather station that reported reliably enough during the analysis period that we have included it in our network. When available, historical temperature and dew point measurements are taken directly from this weather station. These records are obtained from NOAA's Integrated Surface Hourly data set, falling back on ICAO METAR records as required.
In the case of missing or erroneous measurements from this station, we fall back on records from nearby stations, adjusted according to typical seasonal and diurnal intra-station differences. For a given day of the year and hour of the day, the fallback station is selected to minimize the prediction error over the years for which there are measurements for both stations.
The stations on which we may fall back are Sandpoint Airport, Cranbrook/Canadian Rockies International Airport, Nelson Automatic Weather Reporting System, West Kootenay Regional Airport, Sparwood Automatic Weather Reporting System, Nakusp Automatic Weather Reporting System, Crowsnest, and Glacier Park International Airport.
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.