Average Weather in Oltinko‘l Uzbekistan
In Oltinko‘l, the summers are hot, arid, and mostly clear and the winters are freezing, dry, windy, and partly cloudy. Over the course of the year, the temperature typically varies from 16°F to 95°F and is rarely below -2°F or above 103°F.
Based on the beach/pool score, the best time of year to visit Oltinko‘l for hot-weather activities is from early June to late August.
The hot season lasts for 3.9 months, from May 16 to September 12, with an average daily high temperature above 82°F. The hottest day of the year is July 20, with an average high of 95°F and low of 70°F.
The cold season lasts for 3.4 months, from November 22 to March 2, with an average daily high temperature below 43°F. The coldest day of the year is January 19, with an average low of 16°F and high of 31°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 Oltinko‘l, 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 Oltinko‘l begins around May 19 and lasts for 4.9 months, ending around October 17. On August 4, the clearest day of the year, the sky is clear, mostly clear, or partly cloudy 94% of the time, and overcast or mostly cloudy 6% of the time.
The cloudier part of the year begins around October 17 and lasts for 7.1 months, ending around May 19. On January 15, the cloudiest day of the year, the sky is overcast or mostly cloudy 54% of the time, and clear, mostly clear, or partly cloudy 46% of the time.
Cloud Cover Categories
Oltinko‘l 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 5%, with an average value of 2%.
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 in Oltinko‘l changes throughout the year.
Rain alone is the most common for 10.0 months, from February 14 to December 15. The highest chance of a day with rain alone is 5% on March 31.
Snow alone is the most common for 2.0 months, from December 15 to February 14. The highest chance of a day with snow alone is 1% on January 16.
Daily Chance of Precipitation
The sliding 31-day quantity of rainfall in Oltinko‘l does not vary significantly over the course of the year, staying within 0.1 inches of 0.1 inches throughout.
Average Monthly Rainfall
The length of the day in Oltinko‘l varies significantly over the course of the year. In 2018, the shortest day is December 22, with 8 hours, 60 minutes of daylight; the longest day is June 21, with 15 hours, 22 minutes of daylight.
Hours of Daylight and Twilight
The earliest sunrise is at 5:24 AM on June 15, and the latest sunrise is 3 hours, 12 minutes later at 8:35 AM on January 3. The earliest sunset is at 5:29 PM on December 8, and the latest sunset is 3 hours, 19 minutes later at 8:47 PM on June 27.
Daylight saving time (DST) is not observed in Oltinko‘l 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.
The perceived humidity level in Oltinko‘l, as measured by the percentage of time in which the humidity comfort level is muggy, oppressive, or miserable, does not vary significantly over the course of the year, staying within 4% of 4% throughout.
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 Oltinko‘l experiences mild seasonal variation over the course of the year.
The windier part of the year lasts for 4.3 months, from January 30 to June 9, with average wind speeds of more than 10.2 miles per hour. The windiest day of the year is March 21, with an average hourly wind speed of 11.5 miles per hour.
The calmer time of year lasts for 7.7 months, from June 9 to January 30. The calmest day of the year is October 18, with an average hourly wind speed of 8.8 miles per hour.
Average Wind Speed
The predominant average hourly wind direction in Oltinko‘l varies throughout the year.
The wind is most often from the north for 2.7 months, from June 3 to August 24, with a peak percentage of 51% on July 23. The wind is most often from the east for 9.3 months, from August 24 to June 3, with a peak percentage of 35% on January 1.
Best Time of Year to Visit
To characterize how pleasant the weather is in Oltinko‘l 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 Oltinko‘l for general outdoor tourist activities are from mid May to early June and from mid August to late September, with a peak score in the first week of September.
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 Oltinko‘l for hot-weather activities is from early June to late August, with a peak score in the first week of August.
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).
The growing season in Oltinko‘l typically lasts for 6.7 months (204 days), from around March 30 to around October 19, rarely starting before March 13 or after April 17, and rarely ending before October 3 or after November 5.
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.
Based on growing degree days alone, the first spring blooms in Oltinko‘l should appear around April 4, only rarely appearing before March 24 or after April 15.
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 extreme seasonal variation over the course of the year.
The brighter period of the year lasts for 3.5 months, from May 9 to August 23, with an average daily incident shortwave energy per square meter above 6.6 kWh. The brightest day of the year is June 25, with an average of 7.9 kWh.
The darker period of the year lasts for 3.5 months, from October 31 to February 13, with an average daily incident shortwave energy per square meter below 2.9 kWh. The darkest day of the year is December 24, with an average of 1.7 kWh.
Average Daily Incident Shortwave Solar Energy
For the purposes of this report, the geographical coordinates of Oltinko‘l are 43.069 deg latitude, 58.904 deg longitude, and 197 ft elevation.
The topography within 2 miles of Oltinko‘l is essentially flat, with a maximum elevation change of 30 feet and an average elevation above sea level of 196 feet. Within 10 miles is essentially flat (190 feet). Within 50 miles contains only modest variations in elevation (610 feet).
The area within 2 miles of Oltinko‘l is covered by cropland (89%) and bare soil (11%), within 10 miles by cropland (75%) and bare soil (25%), and within 50 miles by bare soil (63%) and cropland (35%).
This report illustrates the typical weather in Oltinko‘l, 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, Nukus / Karakalpakstan, in our network suitable to be used as a proxy for the historical temperature and dew point records of Oltinko‘l.
At a distance of 88 kilometers from Oltinko‘l, 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 Oltinko‘l 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.