Average Weather in April in Ashley North Dakota, United States
Daily high temperatures increase by 14°F, from 47°F to 61°F, rarely falling below 31°F or exceeding 76°F.
Daily low temperatures increase by 10°F, from 27°F to 37°F, rarely falling below 15°F or exceeding 49°F.
For reference, on July 24, the hottest day of the year, temperatures in Ashley typically range from 59°F to 82°F, while on January 15, the coldest day of the year, they range from 5°F to 21°F.
Average High and Low Temperature in April
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on April. 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 April
The month of April in Ashley experiences gradually decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 55% to 50%.
The clearest day of the month is April 30, with clear, mostly clear, or partly cloudy conditions 50% of the time.
For reference, on January 11, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 60%, while on July 24, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 75%.
Cloud Cover Categories in April
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 Ashley, the chance of a wet day over the course of April is very rapidly increasing, starting the month at 12% and ending it at 22%.
For reference, the year's highest daily chance of a wet day is 37% on June 7, and its lowest chance is 4% on January 30.
Over the course of April in Ashley, the chance of a day with only rain increases from 7% to 21%, the chance of a day with mixed snow and rain remains an essentially constant 2% throughout, and the chance of a day with only snow decreases from 3% to 1%.
Probability of Precipitation in April
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 April in Ashley is rapidly increasing, starting the month at 0.7 inches, when it rarely exceeds 1.8 inches, and ending the month at 1.9 inches, when it rarely exceeds 3.7 inches or falls below 0.5 inches.
Average Monthly Rainfall in April
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 April in Ashley is essentially constant, remaining about 0.2 inches throughout, and rarely exceeding 0.9 inches or falling below -0.0 inches.
Average Monthly Liquid-Equivalent Snowfall in April
Over the course of April in Ashley, 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, 30 minutes, implying an average daily increase of 3 minutes, 5 seconds, and weekly increase of 21 minutes, 38 seconds.
The shortest day of the month is April 1, with 12 hours, 50 minutes of daylight and the longest day is April 30, with 14 hours, 19 minutes of daylight.
Hours of Daylight and Twilight in April
The latest sunrise of the month in Ashley is 7:16 AM on April 1 and the earliest sunrise is 51 minutes earlier at 6:25 AM on April 30.
The earliest sunset is 8:06 PM on April 1 and the latest sunset is 38 minutes later at 8:44 PM on April 30.
Daylight saving time is observed in Ashley during 2021, but it neither starts nor ends during April, so the entire month is in daylight saving time.
For reference, on June 21, the longest day of the year, the Sun rises at 5:46 AM and sets 15 hours, 46 minutes later, at 9:32 PM, while on December 21, the shortest day of the year, it rises at 8:16 AM and sets 8 hours, 38 minutes later, at 4:54 PM.
Sunrise & Sunset with Twilight and Daylight Saving Time in April
The figure below presents a compact representation of key lunar data for April 2021. 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 April
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 Ashley is essentially constant during April, remaining around 0% throughout.
For reference, on July 18, the muggiest day of the year, there are muggy conditions 21% 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 April
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 Ashley is essentially constant during April, remaining within 0.2 miles per hour of 12.8 miles per hour throughout.
For reference, on April 1, the windiest day of the year, the daily average wind speed is 13.0 miles per hour, while on July 31, the calmest day of the year, the daily average wind speed is 9.7 miles per hour.
The highest daily average wind speed during April is 13.0 miles per hour on April 1.
Average Wind Speed in April
The hourly average wind direction in Ashley throughout April is predominantly from the north, with a peak proportion of 35% on April 11.
Wind Direction in April
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 Ashley typically lasts for 4.6 months (143 days), from around May 9 to around September 29, rarely starting before April 22 or after May 26, and rarely ending before September 12 or after October 16.
The month of April in Ashley is more likely than not fully outside of the growing season, with the chance that a given day is in the growing season rapidly increasing from 0% to 24% over the course of the month.
Time Spent in Various Temperature Bands and the Growing Season in April
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 Ashley are gradually increasing during April, increasing by 72°F, from 14°F to 86°F, over the course of the month.
Growing Degree Days in April
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 Ashley is increasing during April, rising by 1.2 kWh, from 4.8 kWh to 6.0 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in April
For the purposes of this report, the geographical coordinates of Ashley are 46.034 deg latitude, -99.371 deg longitude, and 2,014 ft elevation.
The topography within 2 miles of Ashley contains only modest variations in elevation, with a maximum elevation change of 167 feet and an average elevation above sea level of 2,010 feet. Within 10 miles also contains only modest variations in elevation (322 feet). Within 50 miles contains only modest variations in elevation (955 feet).
The area within 2 miles of Ashley is covered by cropland (75%) and grassland (21%), within 10 miles by grassland (55%) and cropland (36%), and within 50 miles by grassland (49%) and cropland (49%).
This report illustrates the typical weather in Ashley, 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 5 weather stations near enough to contribute to our estimation of the temperature and dew point in Ashley.
For each station, the records are corrected for the elevation difference between that station and Ashley 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 Ashley is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Ashley and a given station.
The stations contributing to this reconstruction are: Ashley Municipal Airport (33%, 70 kilometers, west); Mobridge Municipal Airport (20%, 97 kilometers, southwest); Aberdeen Regional Airport (19%, 99 kilometers, southeast); Jamestown Municipal Airport (16%, 113 kilometers, northeast); and Gwinner-Roger Melroe Field Airport (12%, 135 kilometers, east).
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.