Spring Weather in Korla ChinaDaily high temperatures increase by 40°F, from 47°F to 87°F, rarely falling below 38°F or exceeding 96°F. Daily low temperatures increase by 35°F, from 27°F to 62°F, rarely falling below 20°F or exceeding 69°F. For reference, on July 24, the hottest day of the year, temperatures in Korla typically range from 71°F to 96°F, while on January 11, the coldest day of the year, they range from 13°F to 29°F. The figure below shows you a compact characterization of the hourly average spring 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. Loma, Colorado, United States (6,772 miles away) and Lincoln, Nebraska, United States (6,737 miles) are the far-away foreign places with temperatures most similar to Korla (view comparison). CloudsThe spring in Korla experiences gradually decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 48% to 41%. The highest chance of overcast or mostly cloudy conditions is 51% on March 23. The clearest day of the spring is May 30, with clear, mostly clear, or partly cloudy conditions 59% of the time. For reference, on March 23, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 51%, while on August 11, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 83%. PrecipitationA wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Korla, the chance of a wet day over the course of the spring is increasing, starting the season at 0% and ending it at 6%. For reference, the year's highest daily chance of a wet day is 9% on July 9, and its lowest chance is 0% on January 6. 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 spring in Korla is gradually increasing, starting the season at 0.0 inches, when it rarely exceeds 0.0 inches or falls below -0.0 inches, and ending the season at 0.4 inches, when it rarely exceeds 0.9 inches. Average Monthly Rainfall in the Spring in Korla
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 spring in Korla, the length of the day is very rapidly increasing. From the start to the end of the season, the length of the day increases by 3 hours, 44 minutes, implying an average daily increase of 2 minutes, 28 seconds, and weekly increase of 17 minutes, 16 seconds. The shortest day of the spring is March 1, with 11 hours, 15 minutes of daylight and the longest day is May 31, with 14 hours, 59 minutes of daylight. The latest sunrise of the spring in Korla is 6:50 AM on March 1 and the earliest sunrise is 2 hours, 7 minutes earlier at 4:43 AM on May 31. The earliest sunset is 6:05 PM on March 1 and the latest sunset is 1 hour, 37 minutes later at 7:42 PM on May 31. Daylight saving time is not observed in Korla during 2026. For reference, on June 21, the longest day of the year, the Sun rises at 4:40 AM and sets 15 hours, 13 minutes later, at 7:53 PM, while on December 21, the shortest day of the year, it rises at 7:39 AM and sets 9 hours, 9 minutes later, at 4:47 PM. Sunrise & Sunset with Twilight in the Spring in Korla
The solar day in the spring. 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 Spring in Korla
northeastsouthwest
Solar elevation and azimuth in the the spring 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 spring 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 Korla is essentially constant during the spring, 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 Korla is rapidly increasing during the spring, increasing from 5.9 miles per hour to 8.2 miles per hour over the course of the season. For reference, on May 11, the windiest day of the year, the daily average wind speed is 8.4 miles per hour, while on January 1, the calmest day of the year, the daily average wind speed is 3.9 miles per hour. The highest daily average wind speed during the spring is 8.4 miles per hour on May 14. The hourly average wind direction in Korla throughout the spring is predominantly from the east, with a peak proportion of 39% on March 27. Wind Direction in the Spring in Korla
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 Korla typically lasts for 7.2 months (221 days), from around March 28 to around November 5, rarely starting before March 11 or after April 18, and rarely ending before October 19 or after November 21. During the spring in Korla, the chance that a given day is within the growing season is very rapidly increasing rising from 1% to 100% over the course of the season. Time Spent in Various Temperature Bands and the Growing Season in the Spring in Korla
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 Korla are very rapidly increasing during the spring, increasing by 1,021°F, from 3°F to 1,023°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 Korla is very rapidly increasing during the spring, rising by 3.1 kWh, from 4.0 kWh to 7.1 kWh, over the course of the season. TopographyFor the purposes of this report, the geographical coordinates of Korla are 41.761 deg latitude, 86.152 deg longitude, and 3,100 ft elevation. The topography within 2 miles of Korla contains only modest variations in elevation, with a maximum elevation change of 335 feet and an average elevation above sea level of 3,116 feet. Within 10 miles contains only modest variations in elevation (3,668 feet). Within 50 miles also contains extreme variations in elevation (9,285 feet). The area within 2 miles of Korla is covered by artificial surfaces (65%) and cropland (30%), within 10 miles by bare soil (52%) and cropland (23%), and within 50 miles by grassland (41%) and bare soil (35%). Data SourcesThis report illustrates the typical weather in Korla, based on a statistical analysis of historical hourly weather reports and model reconstructions from January 1, 1980 to December 31, 2016. Korla 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 Korla, 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. |