Average Weather in July in High Level Canada
In High Level, the month of July is characterized by essentially constant daily high temperatures, with daily highs around 74°F throughout the month, rarely exceeding 84°F or dropping below 65°F. The highest daily average high temperature is 75°F on July 23.
Daily low temperatures are around 51°F, rarely falling below 43°F or exceeding 59°F. The highest daily average low temperature is 52°F on July 23.
For reference, on July 23, the hottest day of the year, temperatures in High Level typically range from 52°F to 75°F, while on January 15, the coldest day of the year, they range from -12°F to 5°F.
Average High and Low Temperature in July
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on July. 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 July
The month of July in High Level experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 51% throughout the month.
The clearest day of the month is July 31, with clear, mostly clear, or partly cloudy conditions 51% of the time.
For reference, on March 6, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 75%, while on August 10, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 52%.
Cloud Cover Categories in July
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In High Level, the chance of a wet day over the course of July is gradually decreasing, starting the month at 27% and ending it at 24%.
For reference, the year's highest daily chance of a wet day is 28% on July 4, and its lowest chance is 10% on February 18.
Probability of Precipitation in July
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 July in High Level is gradually decreasing, starting the month at 2.3 inches, when it rarely exceeds 4.2 inches or falls below 0.9 inches, and ending the month at 2.1 inches, when it rarely exceeds 3.7 inches or falls below 0.8 inches.
The highest average 31-day accumulation is 2.4 inches on July 13.
Average Monthly Rainfall in July
Over the course of July in High Level, the length of the day is rapidly decreasing. From the start to the end of the month, the length of the day decreases by 1 hour, 39 minutes, implying an average daily decrease of 3 minutes, 17 seconds, and weekly decrease of 23 minutes, 0 seconds.
The shortest day of the month is July 31, with 16 hours, 33 minutes of daylight and the longest day is July 1, with 18 hours, 12 minutes of daylight.
Hours of Daylight and Twilight in July
The earliest sunrise of the month in High Level is 4:46 AM on July 1 and the latest sunrise is 51 minutes later at 5:37 AM on July 31.
The latest sunset is 10:58 PM on July 1 and the earliest sunset is 47 minutes earlier at 10:10 PM on July 31.
Daylight saving time is observed in High Level during 2017, but it neither starts nor ends during July, so the entire month is in daylight saving time.
For reference, on June 21, the longest day of the year, the Sun rises at 4:40 AM and sets 18 hours, 21 minutes later, at 11:00 PM, while on December 21, the shortest day of the year, it rises at 9:37 AM and sets 6 hours, 19 minutes later, at 3:56 PM.
Sunrise & Sunset with Twilight in July
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 High Level is essentially constant during July, remaining around 0% throughout.
For reference, on July 26, the muggiest day of the year, there are muggy conditions 0% of the time, while on September 15, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in July
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 High Level is essentially constant during July, remaining within 0.1 miles per hour of 3.4 miles per hour throughout.
For reference, on January 30, the windiest day of the year, the daily average wind speed is 4.8 miles per hour, while on July 21, the calmest day of the year, the daily average wind speed is 3.3 miles per hour.
The lowest daily average wind speed during July is 3.3 miles per hour on July 21.
Average Wind Speed in July
Wind Direction in July
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 High Level typically lasts for 3.5 months (107 days), from around May 24 to around September 8, rarely starting before May 5 or after June 10, and rarely ending before August 18 or after September 26.
The month of July in High Level is reliably fully within the growing season.
Time Spent in Various Temperature Bands and the Growing Season in July
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 High Level is increasing during July, increasing by 385°F, from 495°F to 880°F, over the course of the month.
Growing Degree Days in July
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 High Level is gradually decreasing during July, falling by 0.7 kWh, from 6.1 kWh to 5.5 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in July
For the purposes of this report, the geographical coordinates of High Level are 58.517 deg latitude, -117.136 deg longitude, and 1,076 ft elevation.
The topography within 2 miles of High Level is essentially flat, with a maximum elevation change of 59 feet and an average elevation above sea level of 1,069 feet. Within 10 miles is essentially flat (236 feet). Within 50 miles contains only modest variations in elevation (2,346 feet).
The area within 2 miles of High Level is covered by trees (51%), cropland (24%), and sparse vegetation (20%), within 10 miles by trees (69%) and cropland (20%), and within 50 miles by trees (69%) and herbaceous vegetation (12%).
This report illustrates the typical weather in High Level 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 High Level.
For each station, the records are corrected for the elevation difference between that station and High Level 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 High Level is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between High Level and a given station.
The stations contributing to this reconstruction are: High Level Airport (93%, 12 kilometers, north) and Fort Vermilion (7%, 66 kilometers, east).
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.