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Winter Weather in Pāsārgād Iran

Daily high temperatures are around 54°F, rarely falling below 42°F or exceeding 66°F. The lowest daily average high temperature is 50°F on January 17.

Daily low temperatures are around 32°F, rarely falling below 23°F or exceeding 42°F. The lowest daily average low temperature is 29°F on January 12.

For reference, on July 10, the hottest day of the year, temperatures in Pāsārgād typically range from 67°F to 94°F, while on January 12, the coldest day of the year, they range from 29°F to 50°F.

Average High and Low Temperature in the Winter in Pāsārgād

Average High and Low Temperature in the Winter in PāsārgādDecJanFeb20°F20°F25°F25°F30°F30°F35°F35°F40°F40°F45°F45°F50°F50°F55°F55°F60°F60°F65°F65°F70°F70°F75°F75°FFallSpringJan 1750°FJan 1750°F30°F30°FDec 157°FDec 157°F34°F34°FFeb 2858°FFeb 2858°F35°F35°FJan 151°FJan 151°F30°F30°FFeb 151°FFeb 151°F30°F30°F
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 winter 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.

Average Hourly Temperature in the Winter in Pāsārgād

Average Hourly Temperature in the Winter in PāsārgādDecJanFeb12 AM12 AM2 AM2 AM4 AM4 AM6 AM6 AM8 AM8 AM10 AM10 AM12 PM12 PM2 PM2 PM4 PM4 PM6 PM6 PM8 PM8 PM10 PM10 PM12 AM12 AMFallSpringfreezingvery coldvery coldcoldcoldcoldcoolcool
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 average hourly temperature, color coded into bands. The shaded overlays indicate night and civil twilight.

Toquerville, United States (7,703 miles away); Belen, United States (7,777 miles); and Clarendon, United States (7,638 miles) are the far-away foreign places with temperatures most similar to Pāsārgād (view comparison).

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The winter in Pāsārgād experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 30% throughout the season.

The clearest day of the winter is January 31, with clear, mostly clear, or partly cloudy conditions 74% of the time.

For reference, on April 15, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 35%, while on September 14, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 98%.

Cloud Cover Categories in the Winter in Pāsārgād

Cloud Cover Categories in the Winter in PāsārgādDecJanFeb0%100%10%90%20%80%30%70%40%60%50%50%60%40%70%30%80%20%90%10%100%0%FallSpringDec 167%Dec 167%Feb 2871%Feb 2871%Jan 168%Jan 168%Feb 174%Feb 174%clearmostly clearpartly cloudyovercastmostly cloudy
0% clear 20% mostly clear 40% partly cloudy 60% mostly cloudy 80% overcast 100%
The percentage of time spent in each cloud cover band, categorized by the percentage of the sky covered by clouds.

A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Pāsārgād, the chance of a wet day over the course of the winter is essentially constant, remaining around 13% throughout.

For reference, the year's highest daily chance of a wet day is 15% on January 21, and its lowest chance is 0% on September 9.

Over the course of the winter in Pāsārgād, the chance of a day with only rain remains an essentially constant 10% throughout, the chance of a day with mixed snow and rain remains an essentially constant 1% throughout, and the chance of a day with only snow remains an essentially constant 0% throughout.

Probability of Precipitation in the Winter in Pāsārgād

Probability of Precipitation in the Winter in PāsārgādDecJanFeb0%0%2%2%4%4%6%6%8%8%10%10%12%12%14%14%16%16%FallSpringJan 2115%Jan 2115%Dec 111%Dec 111%Feb 2811%Feb 2811%Jan 112%Jan 112%mixedrainsnow
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).

Rainfall

To 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 winter in Pāsārgād is essentially constant, remaining about 0.9 inches throughout, and rarely exceeding 2.9 inches.

The highest average 31-day accumulation is 1.1 inches on January 18.

Average Monthly Rainfall in the Winter in Pāsārgād

Average Monthly Rainfall in the Winter in PāsārgādDecJanFeb0.0 in0.0 in0.5 in0.5 in1.0 in1.0 in1.5 in1.5 in2.0 in2.0 in2.5 in2.5 in3.0 in3.0 inFallSpringJan 171.1 inJan 171.1 inDec 10.9 inDec 10.9 inFeb 280.8 inFeb 280.8 inJan 11.0 inJan 11.0 inFeb 11.0 inFeb 11.0 in
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.

Snowfall

As with rainfall, we consider the snowfall accumulated over a sliding 31-day period centered around each day.

The average sliding 31-day snowfall during the winter in Pāsārgād is essentially constant, remaining about 0.7 inches throughout, and rarely exceeding 3.1 inches or falling below -0.0 inches.

The highest average 31-day accumulation is 1.2 inches on January 17.

Average Monthly Snowfall in the Winter in Pāsārgād

Average Monthly Snowfall in the Winter in PāsārgādDecJanFeb0.0 in0.0 in0.5 in0.5 in1.0 in1.0 in1.5 in1.5 in2.0 in2.0 in2.5 in2.5 in3.0 in3.0 inFallSpringJan 171.2 inJan 171.2 inDec 10.2 inDec 10.2 inFeb 280.1 inFeb 280.1 inJan 10.8 inJan 10.8 inFeb 10.8 inFeb 10.8 in
The average snowfall (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 rainfall.

Over the course of the winter in Pāsārgād, the length of the day is rapidly increasing. From the start to the end of the season, the length of the day increases by 1 hour, 11 minutes, implying an average daily increase of 48 seconds, and weekly increase of 5 minutes, 33 seconds.

The shortest day of the winter is December 21, with 10 hours, 12 minutes of daylight and the longest day is February 28, with 11 hours, 31 minutes of daylight.

Hours of Daylight and Twilight in the Winter in Pāsārgād

Hours of Daylight and Twilight in the Winter in PāsārgādDecJanFeb0 hr24 hr4 hr20 hr8 hr16 hr12 hr12 hr16 hr8 hr20 hr4 hr24 hr0 hrFallSpringDec 2110 hr, 12 minDec 2110 hr, 12 minnightnightdaydayFeb 2811 hr, 31 minFeb 2811 hr, 31 minFeb 110 hr, 46 minFeb 110 hr, 46 min
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 winter in Pāsārgād is 6:54 AM on January 10 and the earliest sunrise is 30 minutes earlier at 6:24 AM on February 28.

The earliest sunset is 4:56 PM on December 3 and the latest sunset is 59 minutes later at 5:55 PM on February 28.

Daylight saving time is not observed in Pāsārgād during 2024.

For reference, on June 20, the longest day of the year, the Sun rises at 4:56 AM and sets 14 hours, 6 minutes later, at 7:01 PM, while on December 21, the shortest day of the year, it rises at 6:49 AM and sets 10 hours, 12 minutes later, at 5:01 PM.

Sunrise & Sunset with Twilight in the Winter in Pāsārgād

Sunrise & Sunset with Twilight in the Winter in PāsārgādDecJanFeb12 AM2 AM4 AM6 AM8 AM10 AM12 PM2 PM4 PM6 PM8 PM10 PM12 AMFallSpring6:24 AM6:24 AMFeb 285:55 PMFeb 285:55 PM6:37 AM6:37 AMDec 34:56 PMDec 34:56 PM6:54 AM6:54 AMJan 105:15 PMJan 105:15 PM6:47 AM6:47 AMFeb 15:34 PMFeb 15:34 PMSolarMidnightSolarMidnightSolarNoonSunriseSunset
The solar day in the winter. 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 Winter in Pāsārgād

Solar Elevation and Azimuth in the Winter in PāsārgādDecJanFeb12 AM12 AM2 AM2 AM4 AM4 AM6 AM6 AM8 AM8 AM10 AM10 AM12 PM12 PM2 PM2 PM4 PM4 PM6 PM6 PM8 PM8 PM10 PM10 PM12 AM12 AMFallSpring001020203030500010102030304040
northeastsouthwest
Solar elevation and azimuth in the the winter of 2024. 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).

The figure below presents a compact representation of key lunar data for the winter of 2024. 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.

Moon Rise, Set & Phases in the Winter in Pāsārgād

Moon Rise, Set & Phases in the Winter in PāsārgādDecJanFeb12 AM12 AM4 AM4 AM8 AM8 AM12 PM12 PM4 PM4 PM8 PM8 PM12 AM12 AMFallSpringNov 14:18 PMNov 14:18 PMNov 1612:59 AMNov 1612:59 AMDec 19:52 AMDec 19:52 AMDec 1512:32 PMDec 1512:32 PMDec 311:58 AMDec 311:58 AMJan 141:58 AMJan 141:58 AMJan 294:07 PMJan 294:07 PMFeb 125:24 PMFeb 125:24 PMFeb 284:15 AMFeb 284:15 AMMar 1410:25 AMMar 1410:25 AMMar 292:28 PMMar 292:28 PM5:55 AM5:55 AM4:26 PM4:26 PM6:50 AM6:50 AM4:48 PM4:48 PM4:49 PM4:49 PM7:53 AM7:53 AM5:28 PM5:28 PM4:39 PM4:39 PM7:25 AM7:25 AM6:52 AM6:52 AM5:25 PM5:25 PM5:36 PM5:36 PM7:11 AM7:11 AM6:37 AM6:37 AM5:23 PM5:23 PM6:08 AM6:08 AM5:37 AM5:37 AM
The time in which the moon is above the horizon (light blue area), with new moons (dark gray lines) and full moons (blue lines) indicated. The shaded overlays indicate night and civil 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 chance that a given day will be muggy in Pāsārgād is essentially constant during the winter, remaining around 0% throughout.

For reference, on June 12, 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 the Winter in Pāsārgād

Humidity Comfort Levels in the Winter in PāsārgādDecJanFeb0%0%10%10%20%20%30%30%40%40%50%50%60%60%70%70%80%80%90%90%100%100%FallSpringJan 150%Jan 150%Dec 10%Dec 10%Feb 280%Feb 280%Jan 10%Jan 10%Feb 10%Feb 10%drydry
dry 55°F comfortable 60°F humid 65°F muggy 70°F oppressive 75°F miserable
The percentage of time spent at various humidity comfort levels, categorized by dew point.

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 Pāsārgād is increasing during the winter, increasing from 6.7 miles per hour to 8.6 miles per hour over the course of the season.

For reference, on March 4, the windiest day of the year, the daily average wind speed is 8.8 miles per hour, while on October 18, the calmest day of the year, the daily average wind speed is 5.7 miles per hour.

Average Wind Speed in the Winter in Pāsārgād

Average Wind Speed in the Winter in PāsārgādDecJanFeb0 mph0 mph2 mph2 mph4 mph4 mph6 mph6 mph8 mph8 mph10 mph10 mph12 mph12 mph14 mph14 mph16 mph16 mphFallSpringDec 16.7 mphDec 16.7 mphFeb 288.6 mphFeb 288.6 mphJan 17.2 mphJan 17.2 mphFeb 18.2 mphFeb 18.2 mph
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 Pāsārgād throughout the winter is predominantly from the west, with a peak proportion of 56% on February 28.

Wind Direction in the Winter in Pāsārgād

Wind Direction in the Winter in PāsārgādDecJanFeb0%100%20%80%40%60%60%40%80%20%100%0%FallSpringwestnorthsoutheast
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).

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 Pāsārgād typically lasts for 8.1 months (249 days), from around March 16 to around November 20, rarely starting before February 25 or after April 4, and rarely ending before November 2 or after December 8.

The winter in Pāsārgād is more likely than not fully outside of the growing season, with the chance that a given day is in the growing season reaching a low of 0% on January 15.

Time Spent in Various Temperature Bands and the Growing Season in the Winter in Pāsārgād

Time Spent in Various Temperature Bands and the Growing Season in the Winter in PāsārgādDecJanFeb0%100%10%90%20%80%30%70%40%60%50%50%60%40%70%30%80%20%90%10%100%0%FallSpringDec 123%Dec 123%Feb 2815%Feb 2815%Jan 10%Jan 10%Feb 10%Feb 10%50%Nov 2050%Nov 2090%Nov 290%Nov 2freezingvery coldcoldcoolcomfortable
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 Pāsārgād are very rapidly decreasing during the winter, decreasing by 4,939°F, from 4,990°F to 51°F, over the course of the season.

Growing Degree Days in the Winter in Pāsārgād

Growing Degree Days in the Winter in PāsārgādDecJanFeb0°F0°F1,000°F1,000°F2,000°F2,000°F3,000°F3,000°F4,000°F4,000°F5,000°F5,000°FFallSpringDec 14,990°FDec 14,990°FFeb 2851°FFeb 2851°F
The average growing degree days accumulated over the course of the winter, 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 Pāsārgād is rapidly increasing during the winter, rising by 1.6 kWh, from 3.9 kWh to 5.5 kWh, over the course of the season.

The lowest average daily incident shortwave solar energy during the winter is 3.7 kWh on December 25.

Average Daily Incident Shortwave Solar Energy in the Winter in Pāsārgād

Average Daily Incident Shortwave Solar Energy in the Winter in PāsārgādDecJanFeb0 kWh0 kWh1 kWh1 kWh2 kWh2 kWh3 kWh3 kWh4 kWh4 kWh5 kWh5 kWh6 kWh6 kWh7 kWh7 kWh8 kWh8 kWhFallSpringDec 253.7 kWhDec 253.7 kWhDec 13.9 kWhDec 13.9 kWhFeb 285.5 kWhFeb 285.5 kWhFeb 14.6 kWhFeb 14.6 kWh
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 Pāsārgād are 30.202 deg latitude, 53.180 deg longitude, and 6,073 ft elevation.

The topography within 2 miles of Pāsārgād contains only modest variations in elevation, with a maximum elevation change of 387 feet and an average elevation above sea level of 6,082 feet. Within 10 miles contains only modest variations in elevation (2,477 feet). Within 50 miles contains large variations in elevation (8,071 feet).

The area within 2 miles of Pāsārgād is covered by shrubs (41%) and cropland (39%), within 10 miles by shrubs (50%) and sparse vegetation (32%), and within 50 miles by shrubs (52%) and sparse vegetation (21%).

This report illustrates the typical weather in Pāsārgād, 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 2 weather stations near enough to contribute to our estimation of the temperature and dew point in Pāsārgād.

For each station, the records are corrected for the elevation difference between that station and Pāsārgād 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 Pāsārgād is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Pāsārgād and a given station.

The stations contributing to this reconstruction are:

To get a sense of how much these sources agree with each other, you can view a comparison of Pāsārgād and the stations that contribute to our estimates of its temperature history and climate. Please note that each source's contribution is adjusted for elevation and the relative change present in the MERRA-2 data.

Other Data

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.

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 airports and weather stations are provided by AskGeo.com .

Maps are © OpenStreetMap contributors.

Disclaimer

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.

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