Average Weather in August in Ashland Alabama, United States
Daily high temperatures decrease by 2°F, from 88°F to 86°F, rarely falling below 80°F or exceeding 94°F.
Daily low temperatures decrease by 2°F, from 70°F to 67°F, rarely falling below 62°F or exceeding 73°F.
For reference, on July 23, the hottest day of the year, temperatures in Ashland typically range from 70°F to 88°F, while on January 24, the coldest day of the year, they range from 35°F to 53°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 Ashland experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 38% throughout the month.
The clearest day of the month is August 12, with clear, mostly clear, or partly cloudy conditions 63% of the time.
For reference, on January 4, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 54%, while on October 11, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 67%.
Cloud Cover Categories in August
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Ashland, the chance of a wet day over the course of August is very rapidly decreasing, starting the month at 40% and ending it at 30%.
For reference, the year's highest daily chance of a wet day is 45% on July 9, and its lowest chance is 19% on October 16.
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 Ashland is essentially constant, remaining about 2.9 inches throughout, and rarely exceeding 5.6 inches or falling below 1.0 inches.
The lowest average 31-day accumulation is 2.8 inches on August 23.
Average Monthly Rainfall in August
Over the course of August in Ashland, the length of the day is decreasing. From the start to the end of the month, the length of the day decreases by 54 minutes, implying an average daily decrease of 1 minute, 47 seconds, and weekly decrease of 12 minutes, 31 seconds.
The shortest day of the month is August 31, with 12 hours, 53 minutes of daylight and the longest day is August 1, with 13 hours, 46 minutes of daylight.
Hours of Daylight and Twilight in August
The earliest sunrise of the month in Ashland is 5:56 AM on August 1 and the latest sunrise is 21 minutes later at 6:16 AM on August 31.
The latest sunset is 7:42 PM on August 1 and the earliest sunset is 33 minutes earlier at 7:09 PM on August 31.
Daylight saving time is observed in Ashland during 2018, 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 5:34 AM and sets 14 hours, 21 minutes later, at 7:55 PM, while on December 21, the shortest day of the year, it rises at 6:42 AM and sets 9 hours, 57 minutes later, at 4:40 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 Ashland is rapidly decreasing during August, falling from 90% to 76% over the course of the month.
For reference, on July 24, the muggiest day of the year, there are muggy conditions 93% of the time, while on January 23, 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 Ashland is essentially constant during August, remaining within 0.1 miles per hour of 3.2 miles per hour throughout.
For reference, on February 26, the windiest day of the year, the daily average wind speed is 5.1 miles per hour, while on August 5, the calmest day of the year, the daily average wind speed is 3.1 miles per hour.
The lowest daily average wind speed during August is 3.1 miles per hour on August 7.
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 Ashland typically lasts for 7.5 months (228 days), from around March 23 to around November 6, rarely starting before March 1 or after April 13, and rarely ending before October 17 or after November 26.
The month of August in Ashland is reliably fully within the growing season.
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 Ashland are rapidly increasing during August, increasing by 797°F, from 2,887°F to 3,685°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 Ashland is gradually decreasing during August, falling by 0.5 kWh, from 6.4 kWh to 5.8 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 Ashland are 33.274 deg latitude, -85.836 deg longitude, and 1,073 ft elevation.
The topography within 2 miles of Ashland contains only modest variations in elevation, with a maximum elevation change of 384 feet and an average elevation above sea level of 1,080 feet. Within 10 miles contains only modest variations in elevation (1,631 feet). Within 50 miles contains very significant variations in elevation (2,146 feet).
The area within 2 miles of Ashland is covered by cropland (69%) and trees (26%), within 10 miles by trees (80%) and cropland (19%), and within 50 miles by trees (78%) and cropland (14%).
This report illustrates the typical weather in Ashland 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 4 weather stations near enough to contribute to our estimation of the temperature and dew point in Ashland.
For each station, the records are corrected for the elevation difference between that station and Ashland 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 Ashland is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Ashland and a given station.
The stations contributing to this reconstruction are: Anniston Metropolitan Airport (41%, 35 kilometers, north); Thomas C Russell Field (34%, 42 kilometers, south); La Grange, Callaway Airport (14%, 77 kilometers, east); and Shelby County Airport (11%, 89 kilometers, west).
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.