Average Weather on May 28 in Edwards Mississippi, United States
On May 28, the temperature in Edwards typically ranges from 66°F to 85°F and is rarely below 58°F or above 91°F.
For reference, on July 21, the hottest day of the year, temperatures in Edwards typically range from 72°F to 91°F, while on January 16, the coldest day of the year, they range from 37°F to 57°F.
The coolest time of the day is from 11:30 PM to 7:45 AM, with the coldest at 5:45 AM, at which time the temperature is below 70°F three days out of four, and below 73°F nine days out of ten.
The warmest time of the day is from 11:30 AM to 7:00 PM, with the hottest at 3:30 PM, at which time the temperature is above 81°F three days out of four, and above 76°F nine days out of ten.
The day has gained half its heat by 9:15 AM and lost it again by 8:15 PM.
Average Temperature on May 28
The figure below shows you a compact characterization of the range of temperatures experienced on May 28 throughout the historical record. The horizontal axis is the time of day and the colored stacked areas indicate the percentage of hours spent in various temperature bands.
Temperature Bands on May 28
Compared to May 28 (excluding 30 days before and after), September 14 has the most similar daily average high and low temperatures.
The average percentage of the sky covered by clouds in Edwards on May 28 varies over the course of the day.
The cloudiest time of day is around 12:30 AM, at which time the chance of overcast or mostly cloudy conditions is 47%.
The clearest time of day is around 10:30 AM, at which time the chance of clear, mostly clear, or partly cloudy conditions is 64%.
For reference, on January 3, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 51%, while on October 4, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 69%.
Cloud Cover Categories on May 28
0% clear 20% mostly clear 40% partly cloudy 60% mostly cloudy 80% overcast 100%
On average, there is a 36% chance that more than 0.04 inches of total precipitation will fall in Edwards throughout the day on May 28, all of which can be expected to be rain.
For reference, the year's highest daily chance of precipitation is 42% on July 7, and its lowest chance is 23% on October 8.
For those 36% of years with precipitation on May 28, the chart below shows when throughout the day that precipitation is more or less likely to occur, excluding hourly accumulations of less than 0.01 inches. If precipitation were equally likely throughout the day, all hours would report 4.2% (100% divided by 24 hours).
Precipitation is most likely between 1 PM and 2 PM, and least likely between 12 AM and 1 AM.
Hourly Share of Precipitation on May 28
In Edwards on Thursday, May 28, 2020, the Sun rises at 5:57 AM and sets 14 hours, 5 minutes later, at 8:02 PM. Solar noon is at 12:59 PM.
For reference, on June 20, the longest day of the year, the Sun rises at 5:55 AM and sets 14 hours, 16 minutes later, at 8:12 PM, while on December 21, the shortest day of the year, it rises at 6:59 AM and sets 10 hours, 2 minutes later, at 5:01 PM.
Civil twilight, the period before the Sun has risen or after the Sun has set during which time it is possible to engage in most outdoor activities without artificial lighting, begins and ends 28 minutes before sunrise and after sunset, at 5:29 AM and 8:30 PM respectively.
Nautical twilight, during which time it is possible to clearly discern the horizon (e.g., for navigational purposes), begins and ends 1 hour, 2 minutes before sunrise and after sunset, at 4:55 AM and 9:04 PM respectively.
Astronomical twilight, outside of which it is possible to make the most sensitive of astronomical observations, begins and ends 1 hour, 38 minutes before sunrise and after sunset, at 4:19 AM and 9:40 PM respectively.
Solar Elevation on May 28, 2020
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 of muggy, oppressive, or miserable conditions in Edwards on May 28 varies over the course of the day, with an average daily chance of 71%.
The muggiest time of day on May 28 is around 7:30 PM, with muggy conditions 82% of the time.
The least muggy time of day is around 6:30 AM, with muggy conditions 54% of the time.
For reference, on July 21, the muggiest day of the year, there are muggy conditions 98% of the time, while on January 16, the least muggy day of the year, there are muggy conditions 2% of the time.
Humidity Comfort Levels on May 28
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 Edwards on May 28 varies throughout the day, with a daily average of 5.5 miles per hour.
The windiest time of day is around 1:00 PM, with an average hourly wind speed of 6.5 miles per hour, mostly staying between 4.4 miles per hour and 8.4 miles per hour, and rarely falling below 2.7 miles per hour or exceeding 10.4 miles per hour.
The calmest time of day is around 7:30 PM, with an average hourly wind speed of 4.3 miles per hour, mostly staying between 3.3 miles per hour and 5.2 miles per hour, and rarely falling below 2.4 miles per hour or exceeding 6.7 miles per hour.
For reference, on February 25, the windiest day of the year, the daily average wind speed is 7.4 miles per hour, while on July 28, the calmest day of the year, the daily average wind speed is 4.5 miles per hour.
Wind Speed on May 28
Over the entire course of May 28 in Edwards, the hourly average wind direction, in order of prevalence, is from the south (49%), north (19%), east (17%), and west (16%).
Wind Direction on May 28
Shortwave Solar Power
This section discusses the incident shortwave solar power 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 peak incident shortwave solar power per square meter is 0.82 kilowatts at around 12:45 PM.
In contrast, the corresponding value on June 1, the brightest day of the year, is 0.82 kilowatts at around 11:45 AM. The corresponding value on December 24, the darkest day of the year, is 0.45 kilowatts at around 11:15 AM.
Shortwave Solar Power on May 28
For the purposes of this report, the geographical coordinates of Edwards are 32.330 deg latitude, -90.606 deg longitude, and 190 ft elevation.
The topography within 2 miles of Edwards contains only modest variations in elevation, with a maximum elevation change of 223 feet and an average elevation above sea level of 201 feet. Within 10 miles also contains only modest variations in elevation (308 feet). Within 50 miles contains only modest variations in elevation (581 feet).
The area within 2 miles of Edwards is covered by trees (48%), cropland (32%), and herbaceous vegetation (21%), within 10 miles by trees (43%) and cropland (35%), and within 50 miles by cropland (37%) and trees (36%).
This report illustrates the typical weather in Edwards, 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 Edwards.
For each station, the records are corrected for the elevation difference between that station and Edwards 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 Edwards is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Edwards and a given station.
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.