Average Weather in March in Maryville Missouri, United States
Daily high temperatures increase by 13°F, from 46°F to 59°F, rarely falling below 30°F or exceeding 75°F.
Daily low temperatures increase by 11°F, from 27°F to 38°F, rarely falling below 12°F or exceeding 52°F.
For reference, on July 20, the hottest day of the year, temperatures in Maryville typically range from 67°F to 87°F, while on January 15, the coldest day of the year, they range from 18°F to 35°F.
Average High and Low Temperature in March
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 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
The average hourly temperature, color coded into bands: 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 shaded overlays indicate night and civil twilight.
Bishkek, Kyrgyzstan (6,657 miles away) and Seongnam-si, South Korea (6,448 miles) are the far-away foreign places with temperatures most similar to Maryville (view comparison).
The month of March in Maryville experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 50% throughout the month.
The clearest day of the month is March 29, with clear, mostly clear, or partly cloudy conditions 52% of the time.
For reference, on February 12, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 52%, while on August 26, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 72%.
Cloud Cover Categories in March
The percentage of time spent in each cloud cover band, categorized by the percentage of the sky covered by clouds: clear < 20% < mostly clear < 40% < partly cloudy < 60% < mostly cloudy < 80% < overcast.
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Maryville, the chance of a wet day over the course of March is very rapidly increasing, starting the month at 15% and ending it at 24%.
For reference, the year's highest daily chance of a wet day is 44% on June 7, and its lowest chance is 8% on January 12.
Over the course of March in Maryville, the chance of a day with only rain increases from 10% to 23%, 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 decreases from 3% to 1%.
Probability of Precipitation in March
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).
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 Maryville is rapidly increasing, starting the month at 1.0 inches, when it rarely exceeds 2.2 inches or falls below 0.1 inches, and ending the month at 2.3 inches, when it rarely exceeds 3.7 inches or falls below 0.9 inches.
Average Monthly Rainfall in March
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 liquid-equivalent snowfall.
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 Maryville is essentially constant, remaining about 0.1 inches throughout, and rarely exceeding 0.5 inches or falling below -0.0 inches.
Average Monthly Liquid-Equivalent Snowfall in March
The average liquid-equivalent 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 March in Maryville, 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, 20 minutes, implying an average daily increase of 2 minutes, 40 seconds, and weekly increase of 18 minutes, 43 seconds.
The shortest day of the month is March 1, with 11 hours, 18 minutes of daylight and the longest day is March 31, with 12 hours, 38 minutes of daylight.
Hours of Daylight and Twilight in March
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 earliest sunrise of the month in Maryville is 6:39 AM on March 10 and the latest sunrise is 58 minutes later at 7:37 AM on March 11.
The earliest sunset is 6:11 PM on March 1 and the latest sunset is 1 hour, 32 minutes later at 7:43 PM on March 31.
Daylight saving time (DST) starts at 3:00 AM on March 11, 2018, shifting sunrise and sunset to be an hour later.
For reference, on June 21, the longest day of the year, the Sun rises at 5:49 AM and sets 15 hours, 3 minutes later, at 8:52 PM, while on December 21, the shortest day of the year, it rises at 7:38 AM and sets 9 hours, 18 minutes later, at 4:56 PM.
Sunrise & Sunset with Twilight and Daylight Saving Time in March
The solar day over the course of March. 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 transitions to and from daylight saving time are indicated by the 'DST' labels.
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 Maryville is essentially constant during March, remaining around 0% throughout.
For reference, on July 22, the muggiest day of the year, there are muggy conditions 64% of the time, while on November 18, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in March
The percentage of time spent at various humidity comfort levels, categorized by dew point: 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 Maryville is gradually increasing during March, increasing from 12.0 miles per hour to 12.7 miles per hour over the course of the month.
For reference, on April 1, the windiest day of the year, the daily average wind speed is 12.7 miles per hour, while on August 7, the calmest day of the year, the daily average wind speed is 8.1 miles per hour.
Average Wind Speed in March
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 Maryville throughout March is predominantly from the north
, with a peak proportion of 36%
on March 8
Wind Direction in March
The percentage of hours in which the mean wind direction is from each of the four cardinal wind directions (north, east, south, and west), excluding hours in which the mean wind speed is less than 1 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 Maryville typically lasts for 5.9 months (179 days), from around April 16 to around October 12, rarely starting before March 30 or after May 4, and rarely ending before September 24 or after October 31.
The month of March in Maryville is more likely than not fully outside of the growing season, with the chance that a given day is in the growing season increasing from 0% to 11% over the course of the month.
Time Spent in Various Temperature Bands and the Growing Season in March
The percentage of time spent in various temperature bands: 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 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 Maryville are gradually increasing during March, increasing by 69°F, from 17°F to 87°F, over the course of the month.
Growing Degree Days in March
The average growing degree days accumulated over the course of March, 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 Maryville is increasing during March, rising by 1.2 kWh, from 3.8 kWh to 5.0 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in March
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 Maryville are 40.346 deg latitude, -94.872 deg longitude, and 1,083 ft elevation.
The topography within 2 miles of Maryville contains only modest variations in elevation, with a maximum elevation change of 194 feet and an average elevation above sea level of 1,081 feet. Within 10 miles also contains only modest variations in elevation (295 feet). Within 50 miles contains only modest variations in elevation (591 feet).
The area within 2 miles of Maryville is covered by cropland (67%) and artificial surfaces (33%), within 10 miles by cropland (95%), and within 50 miles by cropland (92%).
This report illustrates the typical weather in Maryville 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 5 weather stations near enough to contribute to our estimation of the temperature and dew point in Maryville.
For each station, the records are corrected for the elevation difference between that station and Maryville 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 Maryville is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Maryville and a given station.
The stations contributing to this reconstruction are: Schenck Field Airport (38%, 44 kilometers, north); Rosecrans Memorial Airport (21%, 64 kilometers, south); Brenner Field (20%, 68 kilometers, southwest); Lamoni Municipal Airport (13%, 88 kilometers, east); and Chillicothe, Chillicothe Agri-Science Center (8%, 125 kilometers, southeast).
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.