Summer Weather in Kansas City Missouri, United States
Daily high temperatures increase by 5°F, from 81°F to 86°F, rarely falling below 71°F or exceeding 99°F. The highest daily average high temperature is 90°F on July 21.
Daily low temperatures increase by 5°F, from 63°F to 68°F, rarely falling below 55°F or exceeding 81°F. The highest daily average low temperature is 73°F on July 22.
For reference, on July 21, the hottest day of the year, temperatures in Kansas City typically range from 73°F to 90°F, while on January 6, the coldest day of the year, they range from 24°F to 40°F.
Average High and Low Temperature in the Summer in Kansas City
The figure below shows you a compact characterization of the hourly average summer 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 Summer in Kansas City
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
Lintong, China (7,145 miles away); Zhu Cheng City, China (6,822 miles); and Gwangju, South Korea (6,671 miles) are the far-away foreign places with temperatures most similar to Kansas City (view comparison).
The summer in Kansas City experiences rapidly decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 43% to 29%. The lowest chance of overcast or mostly cloudy conditions is 28% on August 26.
The clearest day of the summer is August 26, with clear, mostly clear, or partly cloudy conditions 72% 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 the Summer in Kansas City
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 Kansas City, the chance of a wet day over the course of the summer is very rapidly decreasing, starting the season at 43% and ending it at 31%.
For reference, the year's highest daily chance of a wet day is 45% on June 8, and its lowest chance is 10% on January 12.
Probability of Precipitation in the Summer in Kansas City
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 summer in Kansas City is rapidly decreasing, starting the season at 5.0 inches, when it rarely exceeds 8.1 inches or falls below 2.1 inches, and ending the season at 3.9 inches, when it rarely exceeds 7.1 inches or falls below 1.4 inches.
The highest average 31-day accumulation is 5.0 inches on June 2. The lowest average 31-day accumulation is 3.4 inches on August 1.
Average Monthly Rainfall in the Summer in Kansas City
Over the course of the summer in Kansas City, the length of the day is rapidly decreasing. From the start to the end of the season, the length of the day decreases by 1 hour, 41 minutes, implying an average daily decrease of 1 minute, 7 seconds, and weekly decrease of 7 minutes, 47 seconds.
The shortest day of the summer is August 31, with 13 hours, 3 minutes of daylight and the longest day is June 21, with 14 hours, 55 minutes of daylight.
Hours of Daylight and Twilight in the Summer in Kansas City
The earliest sunrise of the summer in Kansas City is 5:51 AM on June 14 and the latest sunrise is 55 minutes later at 6:46 AM on August 31.
The latest sunset is 8:48 PM on June 27 and the earliest sunset is 59 minutes earlier at 7:49 PM on August 31.
Daylight saving time is observed in Kansas City during 2021, but it neither starts nor ends during the summer, so the entire season is in daylight saving time.
For reference, on June 21, the longest day of the year, the Sun rises at 5:52 AM and sets 14 hours, 55 minutes later, at 8:47 PM, while on December 21, the shortest day of the year, it rises at 7:34 AM and sets 9 hours, 25 minutes later, at 4:59 PM.
Sunrise & Sunset with Twilight in the Summer in Kansas City
The figure below presents a compact representation of key lunar data for the summer of 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 the Summer in Kansas City
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 Kansas City is very rapidly increasing during the summer, rising from 24% to 46% over the course of the season.
The highest chance of a muggy day during the summer is 67% on July 23.
For reference, on July 23, the muggiest day of the year, there are muggy conditions 67% of the time, while on December 2, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in the Summer in Kansas City
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 Kansas City is decreasing during the summer, decreasing from 9.8 miles per hour to 8.7 miles per hour over the course of the season.
For reference, on April 1, the windiest day of the year, the daily average wind speed is 12.6 miles per hour, while on August 7, the calmest day of the year, the daily average wind speed is 7.9 miles per hour.
The lowest daily average wind speed during the summer is 7.9 miles per hour on August 7.
Average Wind Speed in the Summer in Kansas City
The hourly average wind direction in Kansas City throughout the summer is predominantly from the south, with a peak proportion of 54% on June 26.
Wind Direction in the Summer in Kansas City
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 Kansas City typically lasts for 7.0 months (214 days), from around April 3 to around November 2, rarely starting before March 13 or after April 21, and rarely ending before October 15 or after November 20.
The summer in Kansas City is reliably fully within the growing season.
Time Spent in Various Temperature Bands and the Growing Season in the Summer in Kansas City
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 Kansas City are very rapidly increasing during the summer, increasing by 2,497°F, from 969°F to 3,467°F, over the course of the season.
Growing Degree Days in the Summer in Kansas City
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 Kansas City is gradually decreasing during the summer, falling by 0.8 kWh, from 6.6 kWh to 5.8 kWh, over the course of the season.
The highest average daily incident shortwave solar energy during the summer is 7.0 kWh on July 9.
Average Daily Incident Shortwave Solar Energy in the Summer in Kansas City
For the purposes of this report, the geographical coordinates of Kansas City are 39.100 deg latitude, -94.579 deg longitude, and 899 ft elevation.
The topography within 2 miles of Kansas City contains only modest variations in elevation, with a maximum elevation change of 285 feet and an average elevation above sea level of 830 feet. Within 10 miles also contains only modest variations in elevation (377 feet). Within 50 miles contains only modest variations in elevation (531 feet).
The area within 2 miles of Kansas City is covered by artificial surfaces (100%), within 10 miles by artificial surfaces (82%) and trees (12%), and within 50 miles by cropland (72%) and trees (14%).
This report illustrates the typical weather in Kansas City, 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 Kansas City.
For each station, the records are corrected for the elevation difference between that station and Kansas City 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 Kansas City is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Kansas City 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 Kansas City 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.
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.