Summer Weather in Sharbulag MongoliaDaily high temperatures are around 77°F, rarely falling below 62°F or exceeding 91°F. The highest daily average high temperature is 81°F on July 14. Daily low temperatures are around 57°F, rarely falling below 43°F or exceeding 68°F. The highest daily average low temperature is 62°F on July 15. For reference, on July 14, the hottest day of the year, temperatures in Sharbulag typically range from 62°F to 81°F, while on January 18, the coldest day of the year, they range from -7°F to 10°F. 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. Saskatoon, Saskatchewan, Canada (5,371 miles away) and Headingley, Manitoba, Canada (5,595 miles) are the far-away foreign places with temperatures most similar to Sharbulag (view comparison). CloudsThe summer in Sharbulag experiences gradually decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 40% to 33%. The highest chance of overcast or mostly cloudy conditions is 43% on June 30. The lowest chance of overcast or mostly cloudy conditions is 32% on August 28. The clearest day of the summer is August 28, with clear, mostly clear, or partly cloudy conditions 68% of the time. For reference, on December 16, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 47%, while on August 28, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 68%. PrecipitationA wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Sharbulag, the chance of a wet day over the course of the summer is essentially constant, remaining around 13% throughout. For reference, the year's highest daily chance of a wet day is 18% on July 16, and its lowest chance is 0% on January 16. RainfallTo show variation within the season and not just the monthly totals, we show the rainfall accumulated over a sliding 31-day period centered around each day. The average sliding 31-day rainfall during the summer in Sharbulag is essentially constant, remaining about 0.6 inches throughout, and rarely exceeding 1.5 inches. The highest average 31-day accumulation is 0.8 inches on July 18. Average Monthly Rainfall in the Summer in Sharbulag
The average rainfall (solid line) accumulated over the course of a sliding 31-day period centered on the day in question, with 25th to 75th and 10th to 90th percentile bands. The thin dotted line is the corresponding average snowfall.
SunOver the course of the summer in Sharbulag, the length of the day is very rapidly decreasing. From the start to the end of the season, the length of the day decreases by 2 hours, 23 minutes, implying an average daily decrease of 1 minute, 34 seconds, and weekly decrease of 11 minutes, 1 second. The shortest day of the summer is August 31, with 13 hours, 30 minutes of daylight and the longest day is June 21, with 16 hours, 11 minutes of daylight. The earliest sunrise of the summer in Sharbulag is 4:43 AM on June 16 and the latest sunrise is 1 hour, 19 minutes later at 6:02 AM on August 31. The latest sunset is 8:55 PM on June 26 and the earliest sunset is 1 hour, 23 minutes earlier at 7:32 PM on August 31. Daylight saving time is not observed in Sharbulag during 2026. For reference, on June 21, the longest day of the year, the Sun rises at 4:44 AM and sets 16 hours, 11 minutes later, at 8:54 PM, while on December 21, the shortest day of the year, it rises at 8:37 AM and sets 8 hours, 15 minutes later, at 4:53 PM. Sunrise & Sunset with Twilight in the Summer in Sharbulag
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 Sharbulag
northeastsouthwest
Solar elevation and azimuth in the the summer of 2026. 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).
MoonThe figure below presents a compact representation of key lunar data for the summer of 2026. 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. HumidityWe 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 Sharbulag is essentially constant during the summer, remaining around 0% throughout. WindThis 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 Sharbulag is decreasing during the summer, decreasing from 9.5 miles per hour to 7.8 miles per hour over the course of the season. For reference, on May 8, the windiest day of the year, the daily average wind speed is 10.0 miles per hour, while on January 22, the calmest day of the year, the daily average wind speed is 4.7 miles per hour. The hourly average wind direction in Sharbulag throughout the summer is predominantly from the north, with a peak proportion of 60% on July 5. Wind Direction in the Summer in Sharbulag
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).
Growing SeasonDefinitions 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 Sharbulag typically lasts for 5.2 months (156 days), from around April 29 to around October 2, rarely starting before April 13 or after May 15, and rarely ending before September 16 or after October 18. The summer in Sharbulag is reliably fully within the growing season. Time Spent in Various Temperature Bands and the Growing Season in the Summer in Sharbulag
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 Sharbulag are very rapidly increasing during the summer, increasing by 1,689°F, from 383°F to 2,072°F, over the course of the season. Solar EnergyThis 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 Sharbulag is rapidly decreasing during the summer, falling by 1.8 kWh, from 7.4 kWh to 5.6 kWh, over the course of the season. The highest average daily incident shortwave solar energy during the summer is 7.4 kWh on June 3. TopographyFor the purposes of this report, the geographical coordinates of Sharbulag are 48.817 deg latitude, 93.100 deg longitude, and 3,432 ft elevation. The topography within 2 miles of Sharbulag contains only modest variations in elevation, with a maximum elevation change of 157 feet and an average elevation above sea level of 3,458 feet. Within 10 miles contains only modest variations in elevation (673 feet). Within 50 miles contains significant variations in elevation (5,138 feet). The area within 2 miles of Sharbulag is covered by bare soil (100%), within 10 miles by bare soil (100%), and within 50 miles by bare soil (89%). Data SourcesThis report illustrates the typical weather in Sharbulag, based on a statistical analysis of historical hourly weather reports and model reconstructions from January 1, 1980 to December 31, 2016. Sharbulag is further than 200 kilometers from the nearest reliable weather station, so the weather-related data on this page were taken entirely from NASA's MERRA-2 satellite-era reanalysis . 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. The temperature and dew point estimates are corrected for the difference between the reference elevation of the MERRA-2 grid cell and the elevation of Sharbulag, according to the International Standard Atmosphere . 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. 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. DisclaimerThe 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. Please review our full terms contained on our Terms of Service page. |