Average Weather in August in Manning Canada
In Manning, the month of August is characterized by falling daily high temperatures, with daily highs decreasing by 7°F, from 74°F to 68°F over the course of the month, and rarely exceeding 84°F or dropping below 57°F.
Daily low temperatures decrease by 7°F, from 49°F to 42°F, rarely falling below 34°F or exceeding 56°F.
For reference, on July 25, the hottest day of the year, temperatures in Manning typically range from 49°F to 75°F, while on January 12, the coldest day of the year, they range from -4°F to 12°F.
Average High and Low Temperature in August
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on August. 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 August
The month of August in Manning experiences gradually increasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy increasing from 47% to 52%. The lowest chance of overcast or mostly cloudy conditions is 46% on August 10.
The clearest day of the month is August 10, with clear, mostly clear, or partly cloudy conditions 54% of the time.
For reference, on February 26, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 72%, while on August 3, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 54%.
Cloud Cover Categories in August
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Manning, the chance of a wet day over the course of August is gradually decreasing, starting the month at 22% and ending it at 19%.
For reference, the year's highest daily chance of a wet day is 29% on June 22, and its lowest chance is 9% on February 14.
Probability of Precipitation in August
To show variation within the month and not just the monthly total, we show the rainfall accumulated over a sliding 31-day period centered around each day.
The average sliding 31-day rainfall during August in Manning is gradually decreasing, starting the month at 1.8 inches, when it rarely exceeds 3.7 inches or falls below 0.4 inches, and ending the month at 1.3 inches, when it rarely exceeds 2.8 inches or falls below 0.3 inches.
Average Monthly Rainfall in August
Over the course of August in Manning, the length of the day is very rapidly decreasing. From the start to the end of the month, the length of the day decreases by 2 hours, 14 minutes, implying an average daily decrease of 4 minutes, 29 seconds, and weekly decrease of 31 minutes, 22 seconds.
The shortest day of the month is August 31, with 13 hours, 57 minutes of daylight and the longest day is August 1, with 16 hours, 11 minutes of daylight.
Hours of Daylight and Twilight in August
The earliest sunrise of the month in Manning is 5:50 AM on August 1 and the latest sunrise is 1 hour, 1 minute later at 6:51 AM on August 31.
The latest sunset is 10:01 PM on August 1 and the earliest sunset is 1 hour, 13 minutes earlier at 8:48 PM on August 31.
Daylight saving time is observed in Manning during 2017, but it neither starts nor ends during August, so the entire month is in daylight saving time.
For reference, on June 21, the longest day of the year, the Sun rises at 4:56 AM and sets 17 hours, 52 minutes later, at 10:48 PM, while on December 21, the shortest day of the year, it rises at 9:26 AM and sets 6 hours, 44 minutes later, at 4:10 PM.
Sunrise & Sunset with Twilight in August
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 Manning is essentially constant during August, remaining around 0% throughout.
For reference, on July 27, the muggiest day of the year, there are muggy conditions 1% 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 August
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 Manning is essentially constant during August, remaining within 0.2 miles per hour of 3.9 miles per hour throughout.
For reference, on January 14, the windiest day of the year, the daily average wind speed is 5.5 miles per hour, while on August 1, the calmest day of the year, the daily average wind speed is 3.8 miles per hour.
The lowest daily average wind speed during August is 3.8 miles per hour on August 3.
Average Wind Speed in August
Wind Direction in August
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 Manning typically lasts for 3.5 months (108 days), from around May 23 to around September 7, rarely starting before May 5 or after June 9, and rarely ending before August 20 or after September 24.
The month of August in Manning is more likely than not fully within the growing season, with the chance that a given day is in the growing season rapidly decreasing from 100% to 71% over the course of the month.
Time Spent in Various Temperature Bands and the Growing Season in August
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 Manning is increasing during August, increasing by 286°F, from 847°F to 1,133°F, over the course of the month.
Growing Degree Days in August
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 Manning is decreasing during August, falling by 1.4 kWh, from 5.7 kWh to 4.3 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in August
For the purposes of this report, the geographical coordinates of Manning are 56.917 deg latitude, -117.619 deg longitude, and 1,565 ft elevation.
The topography within 2 miles of Manning contains only modest variations in elevation, with a maximum elevation change of 171 feet and an average elevation above sea level of 1,560 feet. Within 10 miles contains only modest variations in elevation (1,001 feet). Within 50 miles contains very significant variations in elevation (2,464 feet).
The area within 2 miles of Manning is covered by cropland (73%) and sparse vegetation (18%), within 10 miles by cropland (60%) and trees (29%), and within 50 miles by trees (75%) and cropland (12%).
This report illustrates the typical weather in Manning 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 are 2 weather stations near enough to contribute to our estimation of the temperature and dew point in Manning.
For each station, the records are corrected for the elevation difference between that station and Manning according to the International Standard Atmosphere , and by the relative change present in the MERRA-2 satellite-era reanalysis between the two locations.
The estimated value at Manning is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Manning and a given station.
The stations contributing to this reconstruction are: Manning AGDM (94%, 12 kilometers, northeast) and Peace River Airport (6%, 78 kilometers, south).
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.