Average Weather in April in Aragon Georgia, United States
Daily high temperatures increase by 7°F, from 69°F to 77°F, rarely falling below 57°F or exceeding 85°F.
Daily low temperatures increase by 7°F, from 48°F to 55°F, rarely falling below 36°F or exceeding 64°F.
For reference, on July 23, the hottest day of the year, temperatures in Aragon typically range from 71°F to 90°F, while on January 24, the coldest day of the year, they range from 34°F to 53°F.
Average High and Low Temperature in April
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on April. 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 April
The month of April in Aragon experiences gradually decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 47% to 41%.
The clearest day of the month is April 30, with clear, mostly clear, or partly cloudy conditions 59% of the time.
For reference, on January 3, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 55%, while on October 8, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 67%.
Cloud Cover Categories in April
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Aragon, the chance of a wet day over the course of April is essentially constant, remaining around 31% throughout.
For reference, the year's highest daily chance of a wet day is 44% on July 9, and its lowest chance is 20% on October 15.
Probability of Precipitation in April
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 April in Aragon is decreasing, starting the month at 4.2 inches, when it rarely exceeds 7.0 inches or falls below 1.7 inches, and ending the month at 3.7 inches, when it rarely exceeds 6.6 inches or falls below 1.2 inches.
Average Monthly Rainfall in April
Over the course of April in Aragon, the length of the day is increasing. From the start to the end of the month, the length of the day increases by 58 minutes, implying an average daily increase of 1 minute, 60 seconds, and weekly increase of 13 minutes, 57 seconds.
The shortest day of the month is April 1, with 12 hours, 34 minutes of daylight and the longest day is April 30, with 13 hours, 31 minutes of daylight.
Hours of Daylight and Twilight in April
The latest sunrise of the month in Aragon is 7:27 AM on April 1 and the earliest sunrise is 36 minutes earlier at 6:52 AM on April 30.
The earliest sunset is 8:01 PM on April 1 and the latest sunset is 22 minutes later at 8:23 PM on April 30.
Daylight saving time is observed in Aragon during 2018, but it neither starts nor ends during April, so the entire month is in daylight saving time.
For reference, on June 21, the longest day of the year, the Sun rises at 6:29 AM and sets 14 hours, 26 minutes later, at 8:54 PM, while on December 21, the shortest day of the year, it rises at 7:41 AM and sets 9 hours, 53 minutes later, at 5:34 PM.
Sunrise & Sunset with Twilight and Daylight Saving Time in April
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 Aragon is increasing during April, rising from 1% to 7% over the course of the month.
For reference, on July 24, the muggiest day of the year, there are muggy conditions 91% of the time, while on February 19, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in April
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 Aragon is gradually decreasing during April, decreasing from 5.0 miles per hour to 4.4 miles per hour over the course of the month.
For reference, on February 26, the windiest day of the year, the daily average wind speed is 5.2 miles per hour, while on August 4, the calmest day of the year, the daily average wind speed is 3.1 miles per hour.
Average Wind Speed in April
Wind Direction in April
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 Aragon typically lasts for 7.7 months (235 days), from around March 23 to around November 13, rarely starting before February 28 or after April 12, and rarely ending before October 25 or after December 4.
The month of April in Aragon is more likely than not fully within the growing season, with the chance that a given day is in the growing season rapidly increasing from 71% to 99% over the course of the month.
Time Spent in Various Temperature Bands and the Growing Season in April
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 Aragon are increasing during April, increasing by 350°F, from 354°F to 704°F, over the course of the month.
Growing Degree Days in April
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 Aragon is increasing during April, rising by 1.0 kWh, from 5.4 kWh to 6.4 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in April
For the purposes of this report, the geographical coordinates of Aragon are 34.046 deg latitude, -85.056 deg longitude, and 784 ft elevation.
The topography within 2 miles of Aragon contains only modest variations in elevation, with a maximum elevation change of 413 feet and an average elevation above sea level of 780 feet. Within 10 miles contains only modest variations in elevation (755 feet). Within 50 miles contains significant variations in elevation (1,854 feet).
The area within 2 miles of Aragon is covered by cropland (52%) and trees (41%), within 10 miles by trees (64%) and cropland (30%), and within 50 miles by trees (65%) and cropland (17%).
This report illustrates the typical weather in Aragon 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 Aragon.
For each station, the records are corrected for the elevation difference between that station and Aragon 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 Aragon is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Aragon and a given station.
The stations contributing to this reconstruction are: Paulding Northwest Atlanta Airport (34%, 18 kilometers, southeast); Cartersville Airport (42%, 21 kilometers, northeast); Richard B Russell Airport (19%, 35 kilometers, north); and Northeast Alabama Regional Airport (4.3%, 95 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.