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Summer Weather in Quwaysinā Egypt

Daily high temperatures are around 95°F, rarely falling below 86°F or exceeding 103°F. The highest daily average high temperature is 96°F on August 7.

Daily low temperatures increase by 5°F, from 68°F to 73°F, rarely falling below 64°F or exceeding 78°F. The highest daily average low temperature is 75°F on August 10.

For reference, on July 31, the hottest day of the year, temperatures in Quwaysinā typically range from 74°F to 96°F, while on January 21, the coldest day of the year, they range from 49°F to 67°F.

Average High and Low Temperature in the Summer in Quwaysinā

Average High and Low Temperature in the Summer in QuwaysināJunJulAug55°F55°F60°F60°F65°F65°F70°F70°F75°F75°F80°F80°F85°F85°F90°F90°F95°F95°F100°F100°F105°F105°FSpringFallJul 3196°FJul 3196°F74°F74°FJun 193°FJun 193°F68°F68°FAug 3195°FAug 3195°F73°F73°FJul 196°FJul 196°F73°F73°F
The daily average high (red line) and low (blue line) temperature, with 25th to 75th and 10th to 90th percentile bands. The thin dotted lines are the corresponding average perceived temperatures.

The figure below shows you a compact characterization of the hourly average summer temperatures. 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 the Summer in Quwaysinā

Average Hourly Temperature in the Summer in QuwaysināJunJulAug12 AM12 AM2 AM2 AM4 AM4 AM6 AM6 AM8 AM8 AM10 AM10 AM12 PM12 PM2 PM2 PM4 PM4 PM6 PM6 PM8 PM8 PM10 PM10 PM12 AM12 AMSpringFallcoolcomfortablewarmwarmwarmhotswelteringcomfortable
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 average hourly temperature, color coded into bands. The shaded overlays indicate night and civil twilight.

Alice, Texas, United States (7,207 miles away) is the far-away foreign place with temperatures most similar to Quwaysinā (view comparison).

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The summer in Quwaysinā experiences decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 9% to 0%. The lowest chance of overcast or mostly cloudy conditions is 0% on June 29.

The clearest day of the summer is June 29, with clear, mostly clear, or partly cloudy conditions 100% of the time.

For reference, on December 8, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 29%, while on June 29, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 100%.

Cloud Cover Categories in the Summer in Quwaysinā

Cloud Cover Categories in the Summer in QuwaysināJunJulAug0%100%10%90%20%80%30%70%40%60%50%50%60%40%70%30%80%20%90%10%100%0%SpringFallDec 871%Dec 871%Jun 191%Jun 191%Aug 31100%Aug 31100%Jul 1100%Jul 1100%Aug 199%Aug 199%clearovercastmostly clearpartly cloudy
0% clear 20% mostly clear 40% partly cloudy 60% mostly cloudy 80% overcast 100%
The percentage of time spent in each cloud cover band, categorized by the percentage of the sky covered by clouds.

Over the course of the summer in Quwaysinā, the length of the day is rapidly decreasing. From the start to the end of the season, the length of the day decreases by 1 hour, 12 minutes, implying an average daily decrease of 48 seconds, and weekly decrease of 5 minutes, 34 seconds.

The shortest day of the summer is August 31, with 12 hours, 48 minutes of daylight and the longest day is June 20, with 14 hours, 8 minutes of daylight.

Hours of Daylight and Twilight in the Summer in Quwaysinā

Hours of Daylight and Twilight in the Summer in QuwaysināJunJulAug0 hr24 hr4 hr20 hr8 hr16 hr12 hr12 hr16 hr8 hr20 hr4 hr24 hr0 hrSpringFallJun 2014 hr, 8 minJun 2014 hr, 8 minnightnightdaydayAug 3112 hr, 48 minAug 3112 hr, 48 minAug 113 hr, 36 minAug 113 hr, 36 min
The number of hours during which the Sun is visible (black line). From bottom (most yellow) to top (most gray), the color bands indicate: full daylight, twilight (civil, nautical, and astronomical), and full night.

The earliest sunrise of the summer in Quwaysinā is 5:52 AM on June 11 and the latest sunrise is 39 minutes later at 6:31 AM on August 31.

The latest sunset is 8:01 PM on June 29 and the earliest sunset is 43 minutes earlier at 7:19 PM on August 31.

Daylight saving time is observed in Quwaysinā during 2024, but it neither starts nor ends during the summer, so the entire season is in standard time.

For reference, on June 20, the longest day of the year, the Sun rises at 5:53 AM and sets 14 hours, 8 minutes later, at 8:00 PM, while on December 21, the shortest day of the year, it rises at 6:48 AM and sets 10 hours, 10 minutes later, at 4:58 PM.

Sunrise & Sunset with Twilight in the Summer in Quwaysinā

Sunrise & Sunset with Twilight in the Summer in QuwaysināJunJulAug2 AM4 AM6 AM8 AM10 AM12 PM2 PM4 PM6 PM8 PM10 PM12 AMSpringFall5:52 AM5:52 AMJun 117:58 PMJun 117:58 PM5:55 AM5:55 AMJun 298:01 PMJun 298:01 PM6:31 AM6:31 AMAug 317:19 PMAug 317:19 PM6:13 AM6:13 AMAug 17:49 PMAug 17:49 PMSolarMidnightSolarMidnightSolarNoonSunriseSunset
The solar day in the summer. From bottom to top, the black lines are the previous solar midnight, sunrise, solar noon, sunset, and the next solar midnight. The day, twilights (civil, nautical, and astronomical), and night are indicated by the color bands from yellow to gray.

The figure below presents a compact representation of the sun's elevation (the angle of the sun above the horizon) and azimuth (its compass bearing) for every hour of every day in the reporting period. The horizontal axis is the day of the year and the vertical axis is the hour of the day. For a given day and hour of that day, the background color indicates the azimuth of the sun at that moment. The black isolines are contours of constant solar elevation.

Solar Elevation and Azimuth in the Summer in Quwaysinā

Solar Elevation and Azimuth in the Summer in QuwaysināJunJulAug12 AM12 AM2 AM2 AM4 AM4 AM6 AM6 AM8 AM8 AM10 AM10 AM12 PM12 PM2 PM2 PM4 PM4 PM6 PM6 PM8 PM8 PM10 PM10 PM12 AM12 AMSpringFall001020203030405050606070800010102030304040506060707080
northeastsouthwest
Solar elevation and azimuth in the the summer of 2024. The black lines are lines of constant solar elevation (the angle of the sun above the horizon, in degrees). The background color fills indicate the azimuth (the compass bearing) of the sun. The lightly tinted areas at the boundaries of the cardinal compass points indicate the implied intermediate directions (northeast, southeast, southwest, and northwest).

The figure below presents a compact representation of key lunar data for the summer of 2024. The horizontal axis is the day, the vertical axis is the hour of the day, and the colored areas indicate when the moon is above the horizon. The vertical gray bars (new Moons) and blue bars (full Moons) indicate key Moon phases. The label associated with each bar indicates the date and time that the phase is obtained, and the companion time labels indicate the rise and set times of the Moon for the nearest time interval in which the moon is above the horizon.

Moon Rise, Set & Phases in the Summer in Quwaysinā

Moon Rise, Set & Phases in the Summer in QuwaysināJunJulAug12 AM12 AM4 AM4 AM8 AM8 AM12 PM12 PM4 PM4 PM8 PM8 PM12 AM12 AMSpringFallMay 86:23 AMMay 86:23 AMMay 234:54 PMMay 234:54 PMJun 63:38 PMJun 63:38 PMJun 224:09 AMJun 224:09 AMJul 61:58 AMJul 61:58 AMJul 211:18 PMJul 211:18 PMAug 42:14 PMAug 42:14 PMAug 199:26 PMAug 199:26 PMSep 34:56 AMSep 34:56 AMSep 185:35 AMSep 185:35 AM5:58 AM5:58 AM8:17 PM8:17 PM7:59 PM7:59 PM6:10 AM6:10 AM8:14 PM8:14 PM7:51 PM7:51 PM5:47 AM5:47 AM6:00 AM6:00 AM8:51 PM8:51 PM8:23 PM8:23 PM6:52 AM6:52 AM8:07 PM8:07 PM7:38 PM7:38 PM6:52 AM6:52 AM6:39 AM6:39 AM7:36 PM7:36 PM6:42 PM6:42 PM6:48 AM6:48 AM
The time in which the moon is above the horizon (light blue area), with new moons (dark gray lines) and full moons (blue lines) indicated. The shaded overlays indicate night and civil 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.

The chance that a given day will be muggy in Quwaysinā is very rapidly increasing during the summer, rising from 11% to 62% over the course of the season.

The highest chance of a muggy day during the summer is 70% on August 15.

For reference, on August 15, the muggiest day of the year, there are muggy conditions 70% of the time, while on December 22, the least muggy day of the year, there are muggy conditions 0% of the time.

Humidity Comfort Levels in the Summer in Quwaysinā

Humidity Comfort Levels in the Summer in QuwaysināJunJulAug0%0%10%10%20%20%30%30%40%40%50%50%60%60%70%70%80%80%90%90%100%100%SpringFallAug 1570%Aug 1570%Jun 111%Jun 111%Aug 3162%Aug 3162%Jul 146%Jul 146%Aug 168%Aug 168%oppressiveoppressivemuggymuggyhumidhumiddrydrycomfortablecomfortablemiserablemiserable
dry 55°F comfortable 60°F humid 65°F muggy 70°F oppressive 75°F miserable
The percentage of time spent at various humidity comfort levels, categorized by dew point.

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 Quwaysinā is decreasing during the summer, decreasing from 9.4 miles per hour to 8.3 miles per hour over the course of the season.

For reference, on June 10, the windiest day of the year, the daily average wind speed is 9.6 miles per hour, while on December 17, the calmest day of the year, the daily average wind speed is 7.9 miles per hour.

The highest daily average wind speed during the summer is 9.6 miles per hour on June 10.

Average Wind Speed in the Summer in Quwaysinā

Average Wind Speed in the Summer in QuwaysināJunJulAug0 mph0 mph2 mph2 mph4 mph4 mph6 mph6 mph8 mph8 mph10 mph10 mph12 mph12 mph14 mph14 mph16 mph16 mphSpringFallJun 109.6 mphJun 109.6 mphAug 318.3 mphAug 318.3 mphJul 19.4 mphJul 19.4 mphAug 18.6 mphAug 18.6 mph
The average of mean hourly wind speeds (dark gray line), with 25th to 75th and 10th to 90th percentile bands.

The hourly average wind direction in Quwaysinā throughout the summer is predominantly from the north, with a peak proportion of 80% on August 31.

Wind Direction in the Summer in Quwaysinā

Wind Direction in the Summer in QuwaysināJunJulAug0%100%20%80%40%60%60%40%80%20%100%0%SpringFallnortheastwest
northeastsouthwest
The percentage of hours in which the mean wind direction is from each of the four cardinal wind directions, excluding hours in which the mean wind speed is less than 1.0 mph. The lightly tinted areas at the boundaries are the percentage of hours spent in the implied intermediate directions (northeast, southeast, southwest, and northwest).

Quwaysinā is located near a large body of water (e.g., ocean, sea, or large lake). This section reports on the wide-area average surface temperature of that water.

The average surface water temperature in Quwaysinā is rapidly increasing during the summer, rising by 8°F, from 73°F to 82°F, over the course of the season.

The highest average surface water temperature during the summer is 82°F on August 21.

Average Water Temperature in the Summer in Quwaysinā

Average Water Temperature in the Summer in QuwaysināJunJulAug65°F65°F70°F70°F75°F75°F80°F80°F85°F85°FSpringFallAug 2182°FAug 2182°FJun 173°FJun 173°FJul 178°FJul 178°FAug 181°FAug 181°F
The daily average water temperature (purple line), with 25th to 75th and 10th to 90th percentile bands.

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 Quwaysinā 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 in the Summer in Quwaysinā

Time Spent in Various Temperature Bands and the Growing Season in the Summer in QuwaysināJunJulAug0%100%10%90%20%80%30%70%40%60%50%50%60%40%70%30%80%20%90%10%100%0%SpringFall100%Jul 17100%Jul 17coolcomfortablewarmhotsweltering
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 percentage of time spent in various temperature bands. The black line is the percentage chance that a given day is within 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.

The average accumulated growing degree days in Quwaysinā are very rapidly increasing during the summer, increasing by 2,824°F, from 2,378°F to 5,202°F, over the course of the season.

Growing Degree Days in the Summer in Quwaysinā

Growing Degree Days in the Summer in QuwaysināJunJulAug2,500°F2,500°F3,000°F3,000°F3,500°F3,500°F4,000°F4,000°F4,500°F4,500°F5,000°F5,000°FSpringFallJun 12,378°FJun 12,378°FAug 315,202°FAug 315,202°FJul 13,278°FJul 13,278°FAug 14,255°FAug 14,255°F
The average growing degree days accumulated over the course of the summer, with 25th to 75th and 10th to 90th percentile bands.

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 Quwaysinā is gradually decreasing during the summer, falling by 0.9 kWh, from 8.1 kWh to 7.2 kWh, over the course of the season.

The highest average daily incident shortwave solar energy during the summer is 8.5 kWh on June 25.

Average Daily Incident Shortwave Solar Energy in the Summer in Quwaysinā

Average Daily Incident Shortwave Solar Energy in the Summer in QuwaysināJunJulAug0 kWh0 kWh1 kWh1 kWh2 kWh2 kWh3 kWh3 kWh4 kWh4 kWh5 kWh5 kWh6 kWh6 kWh7 kWh7 kWh8 kWh8 kWh9 kWh9 kWhSpringFallJun 258.5 kWhJun 258.5 kWhJun 18.1 kWhJun 18.1 kWhAug 317.2 kWhAug 317.2 kWhAug 18.0 kWhAug 18.0 kWh
The average daily shortwave solar energy reaching the ground per square meter (orange line), with 25th to 75th and 10th to 90th percentile bands.

For the purposes of this report, the geographical coordinates of Quwaysinā are 30.565 deg latitude, 31.158 deg longitude, and 49 ft elevation.

The topography within 2 miles of Quwaysinā is essentially flat, with a maximum elevation change of 43 feet and an average elevation above sea level of 37 feet. Within 10 miles is essentially flat (121 feet). Within 50 miles contains only modest variations in elevation (1,634 feet).

The area within 2 miles of Quwaysinā is covered by cropland (87%) and artificial surfaces (13%), within 10 miles by cropland (92%), and within 50 miles by cropland (67%) and bare soil (27%).

This report illustrates the typical weather in Quwaysinā, 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 3 weather stations near enough to contribute to our estimation of the temperature and dew point in Quwaysinā.

For each station, the records are corrected for the elevation difference between that station and Quwaysinā 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 Quwaysinā is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Quwaysinā and a given station.

The stations contributing to this reconstruction are:

To get a sense of how much these sources agree with each other, you can view a comparison of Quwaysinā and the stations that contribute to our estimates of its temperature history and climate. Please note that each source's contribution is adjusted for elevation and the relative change present in the MERRA-2 data.

Other Data

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 airports and weather stations are provided by AskGeo.com .

Maps are © OpenStreetMap contributors.

Disclaimer

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.

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