Average Weather in August in Lake City Iowa, United States
Daily high temperatures decrease by 3°F, from 83°F to 80°F, rarely falling below 71°F or exceeding 91°F.
Daily low temperatures decrease by 5°F, from 64°F to 60°F, rarely falling below 50°F or exceeding 73°F.
For reference, on July 5, the hottest day of the year, temperatures in Lake City typically range from 65°F to 85°F, while on January 20, the coldest day of the year, they range from 13°F to 29°F.
Average High and Low Temperature in August
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on August. 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 August
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
Almaty, Kazakhstan (6,512 miles away); Yinchuan, China (6,712 miles); and Kujang-ŭp, North Korea (6,221 miles) are the far-away foreign places with temperatures most similar to Lake City (view comparison).
The month of August in Lake City experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 29% throughout the month.
The clearest day of the month is August 1, with clear, mostly clear, or partly cloudy conditions 72% of the time.
For reference, on December 29, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 54%, while on July 28, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 72%.
Cloud Cover Categories in August
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 Lake City, the chance of a wet day over the course of August is decreasing, starting the month at 36% and ending it at 31%.
For reference, the year's highest daily chance of a wet day is 44% on June 7, and its lowest chance is 7% on January 11.
Probability of Precipitation in August
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 August in Lake City is gradually decreasing, starting the month at 3.5 inches, when it rarely exceeds 6.0 inches or falls below 1.2 inches, and ending the month at 3.2 inches, when it rarely exceeds 5.7 inches or falls below 1.3 inches.
Average Monthly Rainfall in August
Over the course of August in Lake City, the length of the day is rapidly decreasing. From the start to the end of the month, the length of the day decreases by 1 hour, 15 minutes, implying an average daily decrease of 2 minutes, 30 seconds, and weekly decrease of 17 minutes, 30 seconds.
The shortest day of the month is August 31, with 13 hours, 12 minutes of daylight and the longest day is August 1, with 14 hours, 27 minutes of daylight.
Hours of Daylight and Twilight in August
The earliest sunrise of the month in Lake City is 6:11 AM on August 1 and the latest sunrise is 31 minutes later at 6:42 AM on August 31.
The latest sunset is 8:38 PM on August 1 and the earliest sunset is 44 minutes earlier at 7:54 PM on August 31.
Daylight saving time is observed in Lake City during 2019, but it neither starts nor ends during August, so the entire month is in daylight saving time.
For reference, on June 21, the longest day of the year, the Sun rises at 5:42 AM and sets 15 hours, 16 minutes later, at 8:58 PM, while on December 22, the shortest day of the year, it rises at 7:44 AM and sets 9 hours, 5 minutes later, at 4:50 PM.
Sunrise & Sunset with Twilight in August
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 Lake City is rapidly decreasing during August, falling from 49% to 31% over the course of the month.
For reference, on July 21, the muggiest day of the year, there are muggy conditions 51% 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 August
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 Lake City is gradually increasing during August, increasing from 8.4 miles per hour to 9.3 miles per hour over the course of the month.
For reference, on April 12, the windiest day of the year, the daily average wind speed is 13.3 miles per hour, while on August 3, the calmest day of the year, the daily average wind speed is 8.3 miles per hour.
The lowest daily average wind speed during August is 8.3 miles per hour on August 3.
Average Wind Speed in August
Wind Direction in August
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 Lake City typically lasts for 5.5 months (167 days), from around April 22 to around October 6, rarely starting before April 4 or after May 11, and rarely ending before September 19 or after October 25.
The month of August in Lake City is reliably fully within the growing season.
Time Spent in Various Temperature Bands and the Growing Season in August
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 Lake City are rapidly increasing during August, increasing by 637°F, from 1,942°F to 2,579°F, over the course of the month.
Growing Degree Days in August
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 Lake City is gradually decreasing during August, falling by 1.0 kWh, from 6.7 kWh to 5.7 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in August
For the purposes of this report, the geographical coordinates of Lake City are 42.267 deg latitude, -94.734 deg longitude, and 1,188 ft elevation.
The topography within 2 miles of Lake City contains only modest variations in elevation, with a maximum elevation change of 121 feet and an average elevation above sea level of 1,199 feet. Within 10 miles also contains only modest variations in elevation (240 feet). Within 50 miles contains only modest variations in elevation (712 feet).
The area within 2 miles of Lake City is covered by cropland (98%), within 10 miles by cropland (100%), and within 50 miles by cropland (97%).
This report illustrates the typical weather in Lake City 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 3 weather stations near enough to contribute to our estimation of the temperature and dew point in Lake City.
For each station, the records are corrected for the elevation difference between that station and Lake 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 Lake City is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Lake City and a given station.
The stations contributing to this reconstruction are: Arthur N Neu Airport (62%, 25 kilometers, south); Fort Dodge Municipal Airport (19%, 55 kilometers, northeast); and Storm Lake Municipal Airport (19%, 56 kilometers, northwest).
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.