Average Weather in August in Kettleman City California, United States
In Kettleman City, the month of August is characterized by gradually falling daily high temperatures, with daily highs decreasing by 3°F, from 99°F to 96°F over the course of the month, and rarely exceeding 105°F or dropping below 89°F.
Daily low temperatures decrease by 3°F, from 64°F to 61°F, rarely falling below 55°F or exceeding 71°F.
For reference, on July 19, the hottest day of the year, temperatures in Kettleman City typically range from 65°F to 99°F, while on December 25, the coldest day of the year, they range from 37°F to 57°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
The month of August in Kettleman City experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 9% throughout the month. The lowest chance of overcast or mostly cloudy conditions is 8% on August 8.
The clearest day of the month is August 8, with clear, mostly clear, or partly cloudy conditions 92% of the time.
For reference, on December 29, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 47%, while on August 8, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 92%.
Cloud Cover Categories in August
Over the course of August in Kettleman City, the length of the day is decreasing. From the start to the end of the month, the length of the day decreases by 60 minutes, implying an average daily decrease of 1 minute, 59 seconds, and weekly decrease of 13 minutes, 56 seconds.
The shortest day of the month is August 31, with 12 hours, 57 minutes of daylight and the longest day is August 1, with 13 hours, 57 minutes of daylight.
Hours of Daylight and Twilight in August
The earliest sunrise of the month in Kettleman City is 6:07 AM on August 1 and the latest sunrise is 24 minutes later at 6:31 AM on August 31.
The latest sunset is 8:04 PM on August 1 and the earliest sunset is 36 minutes earlier at 7:28 PM on August 31.
Daylight saving time is observed in Kettleman City during 2017, 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 5:43 AM and sets 14 hours, 37 minutes later, at 8:20 PM, while on December 21, the shortest day of the year, it rises at 7:06 AM and sets 9 hours, 43 minutes later, at 4:49 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 Kettleman City is essentially constant during August, remaining around 0% throughout.
For reference, on July 20, the muggiest day of the year, there are muggy conditions 1% of the time, while on November 24, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in August
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 Kettleman City is essentially constant during August, remaining within 0.2 miles per hour of 7.0 miles per hour throughout.
For reference, on May 30, the windiest day of the year, the daily average wind speed is 8.7 miles per hour, while on January 7, the calmest day of the year, the daily average wind speed is 5.3 miles per hour.
Average Wind Speed in August
Wind Direction 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 Kettleman City is gradually decreasing during August, falling by 1.0 kWh, from 8.0 kWh to 7.1 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 Kettleman City are 36.008 deg latitude, -119.962 deg longitude, and 256 ft elevation.
The topography within 2 miles of Kettleman City contains only modest variations in elevation, with a maximum elevation change of 476 feet and an average elevation above sea level of 294 feet. Within 10 miles contains only modest variations in elevation (1,148 feet). Within 50 miles contains very significant variations in elevation (5,069 feet).
The area within 2 miles of Kettleman City is covered by cropland (74%) and grassland (19%), within 10 miles by cropland (60%) and grassland (31%), and within 50 miles by cropland (52%) and grassland (35%).
This report illustrates the typical weather in Kettleman 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 4 weather stations near enough to contribute to our estimation of the temperature and dew point in Kettleman City.
For each station, the records are corrected for the elevation difference between that station and Kettleman 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 Kettleman City is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Kettleman City and a given station.
The stations contributing to this reconstruction are: Lemoore Naval Air Station (Reeves Field) (44%, 36 kilometers, north); Hanford Municipal Airport (31%, 46 kilometers, northeast); Paso Robles Municipal Airport (15%, 71 kilometers, southwest); and Meadows Field (9%, 104 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.