Average Weather in Al Bawīţī Egypt
In Al Bawīţī, the summers are long, hot, arid, and clear and the winters are cool, dry, and mostly clear. Over the course of the year, the temperature typically varies from 43°F to 96°F and is rarely below 38°F or above 103°F.
Based on the beach/pool score, the best time of year to visit Al Bawīţī for hot-weather activities is from mid May to mid October.
The hot season lasts for 4.5 months, from May 11 to September 28, with an average daily high temperature above 90°F. The hottest day of the year is July 25, with an average high of 96°F and low of 71°F.
The cool season lasts for 3.0 months, from November 30 to February 28, with an average daily high temperature below 70°F. The coldest day of the year is January 17, with an average low of 43°F and high of 64°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 Al Bawīţī, the average percentage of the sky covered by clouds experiences significant seasonal variation over the course of the year.
The clearer part of the year in Al Bawīţī begins around May 25 and lasts for 4.9 months, ending around October 21. On June 25, the clearest day of the year, the sky is clear, mostly clear, or partly cloudy 99% of the time, and overcast or mostly cloudy 1% of the time.
The cloudier part of the year begins around October 21 and lasts for 7.1 months, ending around May 25. On December 1, the cloudiest day of the year, the sky is overcast or mostly cloudy 26% of the time, and clear, mostly clear, or partly cloudy 74% of the time.
Cloud Cover Categories
Al Bawīţī does not experience significant seasonal variation in the frequency of wet days (i.e., those with greater than 0.04 inches of liquid or liquid-equivalent precipitation). The frequency ranges from 0% to 2%, with an average value of 1%.
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 2% on December 26.
Daily Chance of Precipitation
The sliding 31-day quantity of rainfall in Al Bawīţī does not vary significantly over the course of the year, staying within 0.0 inches of 0.0 inches throughout.
Average Monthly Rainfall
The length of the day in Al Bawīţī varies over the course of the year. In 2018, the shortest day is December 22, with 10 hours, 20 minutes of daylight; the longest day is June 21, with 13 hours, 57 minutes of daylight.
Hours of Daylight and Twilight
The earliest sunrise is at 5:06 AM on June 11, and the latest sunrise is 1 hour, 51 minutes later at 6:58 AM on January 12. The earliest sunset is at 5:07 PM on December 1, and the latest sunset is 1 hour, 58 minutes later at 7:05 PM on July 1.
Daylight saving time (DST) is not observed in Al Bawīţī during 2018.
Sunrise & Sunset with Twilight
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.
Al Bawīţī experiences some seasonal variation in the perceived humidity.
The muggier period of the year lasts for 3.5 months, from June 29 to October 13, during which time the comfort level is muggy, oppressive, or miserable at least 3% of the time. The muggiest day of the year is August 24, with muggy conditions 12% of the time.
The least muggy day of the year is December 28, 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 Al Bawīţī experiences mild seasonal variation over the course of the year.
The windier part of the year lasts for 6.4 months, from March 18 to September 30, with average wind speeds of more than 9.4 miles per hour. The windiest day of the year is June 30, with an average hourly wind speed of 10.5 miles per hour.
The calmer time of year lasts for 5.6 months, from September 30 to March 18. The calmest day of the year is December 21, with an average hourly wind speed of 8.2 miles per hour.
Average Wind Speed
The predominant average hourly wind direction in Al Bawīţī varies throughout the year.
The wind is most often from the west for 6.0 days, from February 2 to February 8, with a peak percentage of 38% on February 2. The wind is most often from the north for 12 months, from February 8 to February 2, with a peak percentage of 42% on January 1.
Best Time of Year to Visit
To characterize how pleasant the weather is in Al Bawīţī throughout the year, we compute two travel scores.
The tourism score favors clear, rainless days with perceived temperatures between 65°F and 80°F. Based on this score, the best times of year to visit Al Bawīţī for general outdoor tourist activities are from mid March to late April and from late September to late November, with a peak score in the third week of October.
The beach/pool score favors clear, rainless days with perceived temperatures between 75°F and 90°F. Based on this score, the best time of year to visit Al Bawīţī for hot-weather activities is from mid May to mid October, with a peak score in the second week of September.
For each hour between 8:00 AM and 9:00 PM of each day in the analysis period (1980 to 2016), independent scores are computed for perceived temperature, cloud cover, and total precipitation. Those scores are combined into a single hourly composite score, which is then aggregated into days, averaged over all the years in the analysis period, and smoothed.
Our cloud cover score is 10 for fully clear skies, falling linearly to 9 for mostly clear skies, and to 1 for fully overcast skies.
Our precipitation score, which is based on the three-hour precipitation centered on the hour in question, is 10 for no precipitation, falling linearly to 9 for trace precipitation, and to 0 for 0.04 inches of precipitation or more.
Our tourism temperature score is 0 for perceived temperatures below 50°F, rising linearly to 9 for 65°F, to 10 for 75°F, falling linearly to 9 for 80°F, and to 1 for 90°F or hotter.
Our beach/pool temperature score is 0 for perceived temperatures below 65°F, rising linearly to 9 for 75°F, to 10 for 82°F, falling linearly to 9 for 90°F, and to 1 for 100°F or hotter.
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).
Temperatures in Al Bawīţī are sufficiently warm year round that it is not entirely meaningful to discuss the growing season in these terms. We nevertheless include the chart below as an illustration of the distribution of temperatures experienced throughout the year.
Time Spent in Various Temperature Bands and the Growing Season
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.
Growing Degree Days
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 3.7 months, from May 4 to August 28, with an average daily incident shortwave energy per square meter above 7.6 kWh. The brightest day of the year is June 23, with an average of 8.6 kWh.
The darker period of the year lasts for 2.9 months, from November 8 to February 5, with an average daily incident shortwave energy per square meter below 4.7 kWh. The darkest day of the year is December 18, with an average of 3.8 kWh.
Average Daily Incident Shortwave Solar Energy
For the purposes of this report, the geographical coordinates of Al Bawīţī are 28.349 deg latitude, 28.866 deg longitude, and 433 ft elevation.
The topography within 2 miles of Al Bawīţī contains only modest variations in elevation, with a maximum elevation change of 279 feet and an average elevation above sea level of 414 feet. Within 10 miles contains only modest variations in elevation (702 feet). Within 50 miles contains significant variations in elevation (1,040 feet).
The area within 2 miles of Al Bawīţī is covered by bare soil (54%), cropland (32%), and artificial surfaces (14%), within 10 miles by bare soil (89%) and cropland (10%), and within 50 miles by bare soil (99%).
This report illustrates the typical weather in Al Bawīţī, 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 is only a single weather station, Minya, in our network suitable to be used as a proxy for the historical temperature and dew point records of Al Bawīţī.
At a distance of 186 kilometers from Al Bawīţī, further than our threshold of 150 kilometers, this station is deemed insufficiently nearby to be relied upon as our primary source for temperature and dew point records. Consequently, the station records are blended with interpolated values from NASA's MERRA-2 satellite-era reanalysis , and both are corrected for elevation differences according to the International Standard Atmosphere .
The weight assigned to the MERRA-2 value depends on the distance from Al Bawīţī to the nearest station, increasing from 0% at 150 kilometers to 100% at 200 kilometers. In this case, the MERRA-2 weight is 42%, making the weight assigned to the weather station 58%.
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.