Average Weather in June in Tahoma California, United States
Daily high temperatures increase by 10°F, from 66°F to 76°F, rarely falling below 53°F or exceeding 83°F.
Daily low temperatures increase by 5°F, from 37°F to 42°F, rarely falling below 29°F or exceeding 50°F.
For reference, on August 3, the hottest day of the year, temperatures in Tahoma typically range from 45°F to 80°F, while on December 31, the coldest day of the year, they range from 19°F to 40°F.
Average High and Low Temperature in June
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on June. 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 June
The month of June in Tahoma experiences rapidly decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 31% to 16%.
The clearest day of the month is June 30, with clear, mostly clear, or partly cloudy conditions 84% of the time.
For reference, on March 2, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 55%, while on July 29, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 89%.
Cloud Cover Categories in June
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Tahoma, the chance of a wet day over the course of June is rapidly decreasing, starting the month at 11% and ending it at 3%.
For reference, the year's highest daily chance of a wet day is 34% on February 23, and its lowest chance is 2% on July 19.
Over the course of June in Tahoma, the chance of a day with only rain decreases from 9% to 3%, 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 remains an essentially constant 0% throughout.
Probability of Precipitation in June
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 June in Tahoma is gradually decreasing, starting the month at 0.6 inches, when it rarely exceeds 1.8 inches, and ending the month at 0.2 inches, when it rarely exceeds 0.8 inches or falls below -0.0 inches.
Average Monthly Rainfall in June
Over the course of June in Tahoma, the length of the day is essentially constant. The shortest day of the month is June 1, with 14 hours, 44 minutes of daylight and the longest day is June 20, with 14 hours, 55 minutes of daylight.
Hours of Daylight and Twilight in June
The earliest sunrise of the month in Tahoma is 5:34 AM on June 14 and the latest sunrise is 4 minutes later at 5:37 AM on June 30.
The earliest sunset is 8:20 PM on June 1 and the latest sunset is 10 minutes later at 8:30 PM on June 28.
Daylight saving time is observed in Tahoma during 2018, but it neither starts nor ends during June, so the entire month is in daylight saving time.
For reference, on June 21, the longest day of the year, the Sun rises at 5:34 AM and sets 14 hours, 55 minutes later, at 8:29 PM, while on December 21, the shortest day of the year, it rises at 7:16 AM and sets 9 hours, 25 minutes later, at 4:41 PM.
Sunrise & Sunset with Twilight in June
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 Tahoma is essentially constant during June, remaining around 0% throughout.
Humidity Comfort Levels in June
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 Tahoma is essentially constant during June, remaining within 0.2 miles per hour of 5.9 miles per hour throughout.
For reference, on March 18, the windiest day of the year, the daily average wind speed is 6.9 miles per hour, while on August 6, the calmest day of the year, the daily average wind speed is 5.1 miles per hour.
Average Wind Speed in June
Wind Direction in June
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 Tahoma typically lasts for 2.9 months (89 days), from around June 15 to around September 12, rarely starting before May 20, or ending after October 8.
During June in Tahoma, the chance that a given day is within the growing season is very rapidly increasing rising from 23% to 76% over the course of the month.
Time Spent in Various Temperature Bands and the Growing Season in June
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 Tahoma are increasing during June, increasing by 255°F, from 197°F to 452°F, over the course of the month.
Growing Degree Days in June
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 Tahoma is gradually increasing during June, rising by 0.6 kWh, from 8.1 kWh to 8.7 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in June
For the purposes of this report, the geographical coordinates of Tahoma are 39.067 deg latitude, -120.128 deg longitude, and 6,230 ft elevation.
The topography within 2 miles of Tahoma contains significant variations in elevation, with a maximum elevation change of 614 feet and an average elevation above sea level of 6,306 feet. Within 10 miles contains significant variations in elevation (4,360 feet). Within 50 miles also contains extreme variations in elevation (10,302 feet).
The area within 2 miles of Tahoma is covered by water (51%) and trees (49%), within 10 miles by water (46%) and trees (38%), and within 50 miles by trees (46%) and shrubs (45%).
This report illustrates the typical weather in Tahoma 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 Tahoma.
For each station, the records are corrected for the elevation difference between that station and Tahoma 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 Tahoma is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Tahoma and a given station.
The stations contributing to this reconstruction are: Lake Tahoe Airport (46%, 22 kilometers, southeast); Truckee Tahoe Airport (30%, 28 kilometers, north); Carson Airport (11%, 36 kilometers, east); Blue Canyon-Nyack Airport (10%, 55 kilometers, northwest); and Placerville Airport (3.3%, 67 kilometers, southwest).
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.