Average Weather in March in Imām Şāḩib Afghanistan
Daily high temperatures increase by 11°F, from 60°F to 71°F, rarely falling below 43°F or exceeding 84°F.
Daily low temperatures increase by 10°F, from 40°F to 50°F, rarely falling below 31°F or exceeding 58°F.
For reference, on July 11, the hottest day of the year, temperatures in Imām Şāḩib typically range from 73°F to 102°F, while on January 11, the coldest day of the year, they range from 33°F to 50°F.
Average High and Low Temperature in March
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on March. 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 March
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 March in Imām Şāḩib experiences gradually decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 58% to 52%. The highest chance of overcast or mostly cloudy conditions is 58% on March 4.
The clearest day of the month is March 31, with clear, mostly clear, or partly cloudy conditions 48% of the time.
For reference, on March 2, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 58%, while on August 14, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 100%.
Cloud Cover Categories in March
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 Imām Şāḩib, the chance of a wet day over the course of March is essentially constant, remaining around 23% throughout.
For reference, the year's highest daily chance of a wet day is 24% on March 18, and its lowest chance is 0% on August 25.
Over the course of March in Imām Şāḩib, the chance of a day with only rain increases from 19% to 21%, 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 March
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 March in Imām Şāḩib is essentially constant, remaining about 1.3 inches throughout, and rarely exceeding 2.5 inches or falling below 0.4 inches.
The highest average 31-day accumulation is 1.4 inches on March 18.
Average Monthly Rainfall in March
We report snowfall in liquid-equivalent terms. The actual depth of new snowfall is typically between 5 and 10 times the liquid-equivalent amount, assuming the ground is frozen. As with rainfall, we consider the liquid-equivalent snowfall accumulated over a sliding 31-day period centered around each day.
The average sliding 31-day liquid-equivalent snowfall during March in Imām Şāḩib is essentially constant, remaining about 0.1 inches throughout, and rarely exceeding 0.3 inches or falling below -0.0 inches.
Average Monthly Liquid-Equivalent Snowfall in March
Over the course of March in Imām Şāḩib, the length of the day is rapidly increasing. From the start to the end of the month, the length of the day increases by 1 hour, 12 minutes, implying an average daily increase of 2 minutes, 23 seconds, and weekly increase of 16 minutes, 42 seconds.
The shortest day of the month is March 1, with 11 hours, 23 minutes of daylight and the longest day is March 31, with 12 hours, 35 minutes of daylight.
Hours of Daylight and Twilight in March
The latest sunrise of the month in Imām Şāḩib is 6:25 AM on March 1 and the earliest sunrise is 44 minutes earlier at 5:41 AM on March 31.
The earliest sunset is 5:48 PM on March 1 and the latest sunset is 28 minutes later at 6:16 PM on March 31.
Daylight saving time is not observed in Imām Şāḩib during 2020.
For reference, on June 20, the longest day of the year, the Sun rises at 4:34 AM and sets 14 hours, 43 minutes later, at 7:17 PM, while on December 21, the shortest day of the year, it rises at 7:04 AM and sets 9 hours, 36 minutes later, at 4:40 PM.
Sunrise & Sunset with Twilight in March
The figure below presents a compact representation of key lunar data for March 2020. 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 March
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 Imām Şāḩib is essentially constant during March, remaining around 0% throughout.
For reference, on May 12, the muggiest day of the year, there are muggy conditions 2% of the time, while on November 3, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in March
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 Imām Şāḩib is essentially constant during March, remaining within 0.1 miles per hour of 4.3 miles per hour throughout.
For reference, on July 8, the windiest day of the year, the daily average wind speed is 6.2 miles per hour, while on December 21, the calmest day of the year, the daily average wind speed is 3.5 miles per hour.
Average Wind Speed in March
The wind direction in Imām Şāḩib during March is predominantly out of the east from March 1 to March 19 and the west from March 19 to March 31.
Wind Direction in March
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 Imām Şāḩib typically lasts for 8.8 months (270 days), from around March 1 to around November 26, rarely starting before February 9 or after March 24, and rarely ending before November 3 or after December 22.
The month of March in Imām Şāḩib is more likely than not fully within the growing season, with the chance that a given day is in the growing season rapidly increasing from 51% to 96% over the course of the month.
Time Spent in Various Temperature Bands and the Growing Season in March
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 Imām Şāḩib are increasing during March, increasing by 223°F, from 119°F to 342°F, over the course of the month.
Growing Degree Days in March
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 Imām Şāḩib is increasing during March, rising by 1.4 kWh, from 3.9 kWh to 5.3 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in March
For the purposes of this report, the geographical coordinates of Imām Şāḩib are 37.189 deg latitude, 68.936 deg longitude, and 1,175 ft elevation.
The topography within 2 miles of Imām Şāḩib is essentially flat, with a maximum elevation change of 72 feet and an average elevation above sea level of 1,167 feet. Within 10 miles is essentially flat (3,146 feet). Within 50 miles contains large variations in elevation (5,587 feet).
The area within 2 miles of Imām Şāḩib is covered by cropland (84%) and artificial surfaces (14%), within 10 miles by cropland (59%) and grassland (13%), and within 50 miles by cropland (47%) and bare soil (21%).
This report illustrates the typical weather in Imām Şāḩib, 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 Imām Şāḩib.
For each station, the records are corrected for the elevation difference between that station and Imām Şāḩib 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 Imām Şāḩib is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Imām Şāḩib 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 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 © 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.