Average Weather in May in Bells Texas, United States
Daily high temperatures increase by 8°F, from 78°F to 85°F, rarely falling below 69°F or exceeding 92°F.
Daily low temperatures increase by 8°F, from 58°F to 67°F, rarely falling below 48°F or exceeding 73°F.
For reference, on July 27, the hottest day of the year, temperatures in Bells typically range from 74°F to 95°F, while on January 7, the coldest day of the year, they range from 35°F to 53°F.
Average High and Low Temperature in May
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on May. 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 May
frigid 15°F freezing 32°F very cold 45°F cold 55°F cool 65°F comfortable 75°F warm 85°F hot 95°F sweltering
The month of May in Bells 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 highest chance of overcast or mostly cloudy conditions is 39% on May 14.
The clearest day of the month is May 7, with clear, mostly clear, or partly cloudy conditions 63% of the time.
For reference, on February 24, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 46%, while on October 5, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 73%.
Cloud Cover Categories in May
0% clear 20% mostly clear 40% partly cloudy 60% mostly cloudy 80% overcast 100%
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Bells, the chance of a wet day over the course of May is rapidly increasing, starting the month at 34% and ending it at 41%.
For reference, the year's highest daily chance of a wet day is 41% on May 22, and its lowest chance is 16% on January 1.
Probability of Precipitation in May
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 May in Bells is essentially constant, remaining about 4.6 inches throughout, and rarely exceeding 8.9 inches or falling below 1.5 inches.
The highest average 31-day accumulation is 4.8 inches on May 17.
Average Monthly Rainfall in May
Over the course of May in Bells, the length of the day is increasing. From the start to the end of the month, the length of the day increases by 42 minutes, implying an average daily increase of 1 minute, 24 seconds, and weekly increase of 9 minutes, 49 seconds.
The shortest day of the month is May 1, with 13 hours, 31 minutes of daylight and the longest day is May 31, with 14 hours, 13 minutes of daylight.
Hours of Daylight and Twilight in May
The latest sunrise of the month in Bells is 6:37 AM on May 1 and the earliest sunrise is 21 minutes earlier at 6:16 AM on May 31.
The earliest sunset is 8:08 PM on May 1 and the latest sunset is 22 minutes later at 8:30 PM on May 31.
Daylight saving time is observed in Bells during 2019, but it neither starts nor ends during May, so the entire month is in daylight saving time.
For reference, on June 21, the longest day of the year, the Sun rises at 6:15 AM and sets 14 hours, 23 minutes later, at 8:39 PM, while on December 22, the shortest day of the year, it rises at 7:26 AM and sets 9 hours, 55 minutes later, at 5:21 PM.
Sunrise & Sunset with Twilight in May
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 Bells is very rapidly increasing during May, rising from 21% to 59% over the course of the month.
For reference, on July 3, the muggiest day of the year, there are muggy conditions 87% of the time, while on January 20, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in May
dry 55°F comfortable 60°F humid 65°F muggy 70°F oppressive 75°F miserable
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 Bells is decreasing during May, decreasing from 10.9 miles per hour to 9.7 miles per hour over the course of the month.
For reference, on April 2, the windiest day of the year, the daily average wind speed is 11.8 miles per hour, while on August 19, the calmest day of the year, the daily average wind speed is 7.7 miles per hour.
Average Wind Speed in May
The hourly average wind direction in Bells throughout May is predominantly from the south, with a peak proportion of 62% on May 31.
Wind Direction in May
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 Bells typically lasts for 8.1 months (250 days), from around March 14 to around November 19, rarely starting before February 19 or after April 6, and rarely ending before October 31 or after December 8.
The month of May in Bells is reliably fully within the growing season.
Time Spent in Various Temperature Bands and the Growing Season in May
frigid 15°F freezing 32°F very cold 45°F cold 55°F cool 65°F comfortable 75°F warm 85°F hot 95°F sweltering
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 Bells are rapidly increasing during May, increasing by 626°F, from 836°F to 1,462°F, over the course of the month.
Growing Degree Days in May
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 Bells is essentially constant during May, remaining within 0.2 kWh of 6.5 kWh throughout.
Average Daily Incident Shortwave Solar Energy in May
For the purposes of this report, the geographical coordinates of Bells are 33.610 deg latitude, -96.411 deg longitude, and 666 ft elevation.
The topography within 2 miles of Bells contains only modest variations in elevation, with a maximum elevation change of 213 feet and an average elevation above sea level of 685 feet. Within 10 miles also contains only modest variations in elevation (371 feet). Within 50 miles contains only modest variations in elevation (643 feet).
The area within 2 miles of Bells is covered by grassland (73%) and cropland (20%), within 10 miles by grassland (49%) and cropland (42%), and within 50 miles by cropland (40%) and grassland (35%).
This report illustrates the typical weather in Bells 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 5 weather stations near enough to contribute to our estimation of the temperature and dew point in Bells.
For each station, the records are corrected for the elevation difference between that station and Bells 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 Bells is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Bells and a given station.
The stations contributing to this reconstruction are: North Texas Regional Airport (41%, 27 kilometers, northwest); Eaker Field (26%, 37 kilometers, north); McKinney Municipal Airport (16%, 50 kilometers, south); Majors Airport (10%, 68 kilometers, southeast); and Cox Field Airport (7%, 89 kilometers, east).
All data relating to the Sun's position (e.g., sunrise and sunset) are computed using astronomical formulas from the book, Astronomical Algorithms 2nd Edition , 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.