Average Weather in June in Qarnābād Iran
Daily high temperatures increase by 4°F, from 86°F to 90°F, rarely falling below 77°F or exceeding 97°F.
Daily low temperatures increase by 7°F, from 62°F to 70°F, rarely falling below 56°F or exceeding 74°F.
For reference, on July 31, the hottest day of the year, temperatures in Qarnābād typically range from 72°F to 92°F, while on January 23, the coldest day of the year, they range from 34°F to 52°F.
Average High and Low Temperature in June
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on June. 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 June
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 month of June in Qarnābād experiences decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 13% to 3%.
The clearest day of the month is June 30, with clear, mostly clear, or partly cloudy conditions 97% of the time.
For reference, on March 15, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 43%, while on August 11, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 99%.
Cloud Cover Categories in June
0% clear 20% mostly clear 40% partly cloudy 60% mostly cloudy 80% overcast 100%
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Qarnābād, the chance of a wet day over the course of June is gradually decreasing, starting the month at 5% and ending it at 3%.
For reference, the year's highest daily chance of a wet day is 14% on March 1, and its lowest chance is 3% on June 30.
Probability of Precipitation in June
To show variation within the month and not just the monthly total, we show the rainfall accumulated over a sliding 31-day period centered around each day.
The average sliding 31-day rainfall during June in Qarnābād is essentially constant, remaining about 0.2 inches throughout, and rarely exceeding 0.7 inches or falling below -0.0 inches.
The lowest average 31-day accumulation is 0.2 inches on June 26.
Average Monthly Rainfall in June
Over the course of June in Qarnābād, the length of the day is essentially constant. The shortest day of the month is June 1, with 14 hours, 31 minutes of daylight and the longest day is June 21, with 14 hours, 41 minutes of daylight.
Hours of Daylight and Twilight in June
The earliest sunrise of the month in Qarnābād is 5:31 AM on June 14 and the latest sunrise is 4 minutes later at 5:35 AM on June 30.
The earliest sunset is 8:05 PM on June 1 and the latest sunset is 10 minutes later at 8:14 PM on June 28.
Daylight saving time is observed in Qarnābād during 2018, but it neither starts nor ends during June, so the entire month is in daylight saving time.
For reference, on June 21, the longest day of the year, the Sun rises at 5:32 AM and sets 14 hours, 41 minutes later, at 8:14 PM, while on December 21, the shortest day of the year, it rises at 7:00 AM and sets 9 hours, 38 minutes later, at 4:38 PM.
Sunrise & Sunset with Twilight in June
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 Qarnābād is very rapidly increasing during June, rising from 4% to 31% over the course of the month.
For reference, on July 26, the muggiest day of the year, there are muggy conditions 53% of the time, while on November 22, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in June
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 Qarnābād is essentially constant during June, remaining within 0.1 miles per hour of 6.3 miles per hour throughout.
For reference, on June 27, the windiest day of the year, the daily average wind speed is 6.4 miles per hour, while on November 7, the calmest day of the year, the daily average wind speed is 4.8 miles per hour.
The highest daily average wind speed during June is 6.4 miles per hour on June 27.
Average Wind Speed in June
Wind Direction in June
Qarnābād 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 Qarnābād is increasing during June, rising by 6°F, from 73°F to 79°F, over the course of the month.
Average Water Temperature in June
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 Qarnābād typically lasts for 8.8 months (268 days), from around March 18 to around December 11, rarely starting before February 21 or after April 8, and rarely ending before November 19 or after January 3.
The month of June in Qarnābād is reliably fully within the growing season.
Time Spent in Various Temperature Bands and the Growing Season in June
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
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 Qarnābād are rapidly increasing during June, increasing by 758°F, from 1,094°F to 1,852°F, over the course of the month.
Growing Degree Days in June
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 Qarnābād is essentially constant during June, remaining within 0.1 kWh of 8.0 kWh throughout.
The highest average daily incident shortwave solar energy during June is 8.1 kWh on June 21.
Average Daily Incident Shortwave Solar Energy in June
For the purposes of this report, the geographical coordinates of Qarnābād are 36.822 deg latitude, 54.592 deg longitude, and 814 ft elevation.
The topography within 2 miles of Qarnābād contains very significant variations in elevation, with a maximum elevation change of 1,398 feet and an average elevation above sea level of 898 feet. Within 10 miles contains very significant variations in elevation (9,114 feet). Within 50 miles also contains extreme variations in elevation (12,894 feet).
The area within 2 miles of Qarnābād is covered by cropland (52%), shrubs (27%), and trees (12%), within 10 miles by trees (49%) and cropland (38%), and within 50 miles by shrubs (32%) and trees (21%).
This report illustrates the typical weather in Qarnābād 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 are 3 weather stations near enough to contribute to our estimation of the temperature and dew point in Qarnābād.
For each station, the records are corrected for the elevation difference between that station and Qarnābād 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 Qarnābād is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Qarnābād and a given station.
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.