Average Weather in Inverness Alabama, United States
In Inverness, the summers are long, hot, and oppressive; the winters are short and cold; and it is wet and partly cloudy year round. Over the course of the year, the temperature typically varies from 38°F to 91°F and is rarely below 25°F or above 97°F.
The hot season lasts for 4.1 months, from May 20 to September 22, with an average daily high temperature above 84°F. The hottest day of the year is July 22, with an average high of 91°F and low of 72°F.
The cool season lasts for 2.9 months, from November 30 to February 23, with an average daily high temperature below 65°F. The coldest day of the year is January 17, with an average low of 38°F and high of 58°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
In Inverness, the average percentage of the sky covered by clouds experiences mild seasonal variation over the course of the year.
The clearer part of the year in Inverness begins around August 21 and lasts for 3.4 months, ending around December 2. On October 8, the clearest day of the year, the sky is clear, mostly clear, or partly cloudy 66% of the time, and overcast or mostly cloudy 34% of the time.
The cloudier part of the year begins around December 2 and lasts for 8.6 months, ending around August 21. On January 3, the cloudiest day of the year, the sky is overcast or mostly cloudy 52% of the time, and clear, mostly clear, or partly cloudy 48% 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 in Inverness varies significantly throughout the year.
The wetter season lasts 3.0 months, from May 29 to August 30, with a greater than 33% chance of a given day being a wet day. The chance of a wet day peaks at 49% on July 17.
The drier season lasts 9.0 months, from August 30 to May 29. The smallest chance of a wet day is 17% on October 16.
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 throughout the year is rain alone, with a peak probability of 49% on July 17.
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. Inverness experiences significant seasonal variation in monthly rainfall.
Rain falls throughout the year in Inverness. The most rain falls during the 31 days centered around March 11, with an average total accumulation of 5.2 inches.
The least rain falls around October 17, with an average total accumulation of 2.6 inches.
Average Monthly Rainfall
The length of the day in Inverness varies significantly over the course of the year. In 2017, the shortest day is December 21, with 10 hours, 3 minutes of daylight; the longest day is June 20, with 14 hours, 15 minutes of daylight.
Hours of Daylight and Twilight
The earliest sunrise is at 5:36 AM on June 11, and the latest sunrise is 1 hour, 26 minutes later at 7:02 AM on November 4. The earliest sunset is at 4:38 PM on December 3, and the latest sunset is 3 hours, 15 minutes later at 7:53 PM on June 30.
Daylight saving time (DST) is observed in Inverness during 2017, starting in the spring on March 12, lasting 7.8 months, and ending in the fall on November 5.
Sunrise & Sunset with Twilight and Daylight Saving Time
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.
Inverness experiences extreme seasonal variation in the perceived humidity.
The muggier period of the year lasts for 5.0 months, from May 10 to October 10, during which time the comfort level is muggy, oppressive, or miserable at least 24% of the time. The muggiest day of the year is July 24, with muggy conditions 96% of the time.
The least muggy day of the year is January 23, when muggy conditions are essentially unheard of.
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 in Inverness experiences mild seasonal variation over the course of the year.
The windier part of the year lasts for 7.2 months, from October 7 to May 12, with average wind speeds of more than 3.9 miles per hour. The windiest day of the year is February 26, with an average hourly wind speed of 4.7 miles per hour.
The calmer time of year lasts for 4.8 months, from May 12 to October 7. The calmest day of the year is August 5, with an average hourly wind speed of 3.0 miles per hour.
Average Wind Speed
The predominant average hourly wind direction in Inverness varies throughout the year.
The wind is most often from the south for 3.7 months, from February 23 to June 13, with a peak percentage of 36% on April 18. The wind is most often from the east for 3.1 months, from August 14 to November 17, with a peak percentage of 46% on September 9. The wind is most often from the north for 3.2 months, from November 17 to February 23, with a peak percentage of 30% on January 1.
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 significant seasonal variation over the course of the year.
The brighter period of the year lasts for 3.9 months, from April 8 to August 6, with an average daily incident shortwave energy per square meter above 6.0 kWh. The brightest day of the year is May 20, with an average of 6.8 kWh.
The darker period of the year lasts for 2.6 months, from November 15 to February 3, with an average daily incident shortwave energy per square meter below 3.6 kWh. The darkest day of the year is December 23, with an average of 2.8 kWh.
Average Daily Incident Shortwave Solar Energy
For the purposes of this report, the geographical coordinates of Inverness are 32.015 deg latitude, -85.746 deg longitude, and 456 ft elevation.
The topography within 2 miles of Inverness contains only modest variations in elevation, with a maximum elevation change of 157 feet and an average elevation above sea level of 448 feet. Within 10 miles also contains only modest variations in elevation (351 feet). Within 50 miles contains only modest variations in elevation (771 feet).
The area within 2 miles of Inverness is covered by trees (87%) and cropland (13%), within 10 miles by trees (90%), and within 50 miles by trees (73%) and cropland (19%).
This report illustrates the typical weather in Inverness, 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 Inverness.
For each station, the records are corrected for the elevation difference between that station and Inverness 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 Inverness is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Inverness and a given station.
The stations contributing to this reconstruction are: Troy Municipal Airport (52%, 30 kilometers, southwest); Weedon Field (19%, 59 kilometers, east); Maxwell Air Force Base / Montgomery (15%, 70 kilometers, northwest); and Auburn-Opelika Robert G Pitts Airport (14%, 73 kilometers, northeast).
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.