Average Weather in March in Tabuk Saudi Arabia
Daily high temperatures increase by 8°F, from 72°F to 80°F, rarely falling below 62°F or exceeding 89°F.
Daily low temperatures increase by 7°F, from 47°F to 54°F, rarely falling below 40°F or exceeding 61°F.
For reference, on August 6, the hottest day of the year, temperatures in Tabuk typically range from 76°F to 102°F, while on January 16, the coldest day of the year, they range from 40°F to 64°F.
Average High and Low Temperature in March
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 temperatures for the quarter of the year centered on March. 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 March
The average hourly temperature, color coded into bands: 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 shaded overlays indicate night and civil twilight.
Sky Valley, California, United States (7,791 miles away) and Marana, Arizona, United States (7,740 miles) are the far-away foreign places with temperatures most similar to Tabuk (view comparison).
The month of March in Tabuk experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 20% throughout the month. The lowest chance of overcast or mostly cloudy conditions is 18% on March 28.
The clearest day of the month is March 28, with clear, mostly clear, or partly cloudy conditions 82% of the time.
For reference, on December 19, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 27%, while on September 8, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 99%.
Cloud Cover Categories in March
The percentage of time spent in each cloud cover band, categorized by the percentage of the sky covered by clouds: clear < 20% < mostly clear < 40% < partly cloudy < 60% < mostly cloudy < 80% < overcast.
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Tabuk, the chance of a wet day over the course of March is essentially constant, remaining around 1% throughout.
For reference, the year's highest daily chance of a wet day is 2% on January 29, and its lowest chance is 0% on July 1.
Probability of Precipitation in March
The percentage of days in which various types of precipitation are observed, excluding trace quantities: rain alone, snow alone, and mixed (both rain and snow fell in the same day).
Over the course of March in Tabuk, the length of the day is increasing. From the start to the end of the month, the length of the day increases by 51 minutes, implying an average daily increase of 1 minute, 42 seconds, and weekly increase of 11 minutes, 54 seconds.
The shortest day of the month is March 1, with 11 hours, 35 minutes of daylight and the longest day is March 31, with 12 hours, 26 minutes of daylight.
Hours of Daylight and Twilight in March
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 latest sunrise of the month in Tabuk is 6:58 AM on March 1 and the earliest sunrise is 34 minutes earlier at 6:25 AM on March 31.
The earliest sunset is 6:33 PM on March 1 and the latest sunset is 17 minutes later at 6:50 PM on March 31.
Daylight saving time is not observed in Tabuk during 2018.
For reference, on June 21, the longest day of the year, the Sun rises at 5:36 AM and sets 13 hours, 57 minutes later, at 7:34 PM, while on December 21, the shortest day of the year, it rises at 7:21 AM and sets 10 hours, 20 minutes later, at 5:41 PM.
Sunrise & Sunset with Twilight in March
The solar day over the course of March. 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.
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 Tabuk is essentially constant during March, remaining around 0% throughout.
For reference, on August 18, the muggiest day of the year, there are muggy conditions 0% of the time, while on January 1, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in March
The percentage of time spent at various humidity comfort levels, categorized by dew point: 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 Tabuk is essentially constant during March, remaining within 0.1 miles per hour of 8.9 miles per hour throughout.
For reference, on March 11, the windiest day of the year, the daily average wind speed is 9.0 miles per hour, while on October 13, the calmest day of the year, the daily average wind speed is 7.2 miles per hour.
The highest daily average wind speed during March is 9.0 miles per hour on March 15.
Average Wind Speed in March
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 Tabuk throughout March is predominantly from the west
, with a peak proportion of 36%
on March 1
Wind Direction in March
The percentage of hours in which the mean wind direction is from each of the four cardinal wind directions (north, east, south, and west), excluding hours in which the mean wind speed is less than 1 mph. The lightly tinted areas at the boundaries are the percentage of hours spent in the implied intermediate directions (northeast, southeast, southwest, and northwest).
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).
While it does not do so every year, freezing temperatures are seen in Tabuk over some winters. The day least likely to be in the growing season is January 16, with a 63% chance.
Time Spent in Various Temperature Bands and the Growing Season in March
The percentage of time spent in various temperature bands: 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 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 Tabuk are increasing during March, increasing by 402°F, from 370°F to 772°F, over the course of the month.
Growing Degree Days in March
The average growing degree days accumulated over the course of March, 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 Tabuk is increasing during March, rising by 1.2 kWh, from 5.9 kWh to 7.1 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in March
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 Tabuk are 28.400 deg latitude, 36.572 deg longitude, and 2,503 ft elevation.
The topography within 2 miles of Tabuk contains only modest variations in elevation, with a maximum elevation change of 125 feet and an average elevation above sea level of 2,508 feet. Within 10 miles also contains only modest variations in elevation (397 feet). Within 50 miles contains only modest variations in elevation (4,373 feet).
The area within 2 miles of Tabuk is covered by artificial surfaces (93%), within 10 miles by bare soil (75%) and cropland (16%), and within 50 miles by bare soil (93%).
This report illustrates the typical weather in Tabuk 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 is only a single weather station, Tabuk Regional Airport, in our network suitable to be used as a proxy for the historical temperature and dew point records of Tabuk.
At a distance of 6 kilometers from Tabuk, closer than our threshold of 150 kilometers, this station is deemed sufficiently nearby to be relied upon as our primary source for temperature and dew point records.
The station records are corrected for the elevation difference between the station and Tabuk according to the International Standard Atmosphere , and by the relative change present in the MERRA-2 satellite-era reanalysis between the two locations.
Please note that the station records themselves may additionally have been back-filled using other nearby stations or the MERRA-2 reanalysis.
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.