Climate and Average Weather Year Round in Boulder Colorado, United States
In Boulder, the summers are warm; the winters are very cold, snowy, and windy; and it is partly cloudy year round. Over the course of the year, the temperature typically varies from 22°F to 87°F and is rarely below 6°F or above 95°F.
Based on the tourism score, the best time of year to visit Boulder for warm-weather activities is from mid June to early September.
Average Temperature in Boulder
The hot season lasts for 3.1 months, from June 8 to September 13, with an average daily high temperature above 78°F. The hottest month of the year in Boulder is July, with an average high of 86°F and low of 60°F.
The cold season lasts for 3.5 months, from November 18 to March 3, with an average daily high temperature below 51°F. The coldest month of the year in Boulder is December, with an average low of 23°F and high of 43°F.
The figure below shows you a compact characterization of the entire year of hourly average temperatures. The horizontal axis is the day of the year, the vertical axis is the hour of the day, and the color is the average temperature for that hour and day.
Ankara, Turkey (6,323 miles away) is the far-away foreign place with temperatures most similar to Boulder (view comparison).
In Boulder, the average percentage of the sky covered by clouds experiences significant seasonal variation over the course of the year.
The clearer part of the year in Boulder begins around June 3 and lasts for 5.0 months, ending around November 2.
The clearest month of the year in Boulder is September, during which on average the sky is clear, mostly clear, or partly cloudy 73% of the time.
The cloudier part of the year begins around November 2 and lasts for 7.0 months, ending around June 3.
The cloudiest month of the year in Boulder is March, during which on average the sky is overcast or mostly cloudy 47% of the time.
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. The chance of wet days in Boulder varies throughout the year.
The wetter season lasts 5.2 months, from March 28 to September 3, with a greater than 19% chance of a given day being a wet day. The month with the most wet days in Boulder is May, with an average of 8.5 days with at least 0.04 inches of precipitation.
The drier season lasts 6.8 months, from September 3 to March 28. The month with the fewest wet days in Boulder is January, with an average of 2.8 days with at least 0.04 inches of precipitation.
Among wet days, we distinguish between those that experience rain alone, snow alone, or a mixture of the two. Based on this categorization, the most common form of precipitation in Boulder changes throughout the year.
Rain alone is the most common for 9.3 months, from February 18 to November 28. The month with the most days of rain alone in Boulder is July, with an average of 8.2 days.
Snow alone is the most common for 2.7 months, from November 28 to February 18. The month with the most days of snow alone in Boulder is December, with an average of 1.4 days.
To show variation within the months and not just the monthly totals, we show the rainfall accumulated over a sliding 31-day period centered around each day of the year. Boulder experiences some seasonal variation in monthly rainfall.
The rainy period of the year lasts for 8.0 months, from March 5 to November 5, with a sliding 31-day rainfall of at least 0.5 inches. The month with the most rain in Boulder is May, with an average rainfall of 1.9 inches.
The rainless period of the year lasts for 4.0 months, from November 5 to March 5. The month with the least rain in Boulder is January, with an average rainfall of 0.1 inches.
As with rainfall, we consider the snowfall accumulated over a sliding 31-day period centered around each day of the year. Boulder experiences some seasonal variation in monthly snowfall.
The snowy period of the year lasts for 6.7 months, from October 10 to May 2, with a sliding 31-day snowfall of at least 1.0 inches. The month with the most snow in Boulder is December, with an average snowfall of 2.8 inches.
The snowless period of the year lasts for 5.3 months, from May 2 to October 10. The least snow falls around July 19, with an average total accumulation of 0.0 inches.
The length of the day in Boulder varies significantly over the course of the year. In 2023, the shortest day is December 21, with 9 hours, 20 minutes of daylight; the longest day is June 21, with 15 hours, 1 minute of daylight.
The earliest sunrise is at 5:31 AM on June 14, and the latest sunrise is 2 hours, 2 minutes later at 7:33 AM on November 4. The earliest sunset is at 4:35 PM on December 7, and the latest sunset is 3 hours, 59 minutes later at 8:34 PM on June 27.
Daylight saving time (DST) is observed in Boulder during 2023, starting in the spring on March 12, lasting 7.8 months, and ending in the fall on November 5.
The figure below presents a compact representation of the sun's elevation (the angle of the sun above the horizon) and azimuth (its compass bearing) for every hour of every day in the reporting period. The horizontal axis is the day of the year and the vertical axis is the hour of the day. For a given day and hour of that day, the background color indicates the azimuth of the sun at that moment. The black isolines are contours of constant solar elevation.
The figure below presents a compact representation of key lunar data for 2023. 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.
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 perceived humidity level in Boulder, as measured by the percentage of time in which the humidity comfort level is muggy, oppressive, or miserable, does not vary significantly over the course of the year, remaining a virtually constant 0% throughout.
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 Boulder experiences significant seasonal variation over the course of the year.
The windier part of the year lasts for 5.2 months, from November 11 to April 18, with average wind speeds of more than 8.0 miles per hour. The windiest month of the year in Boulder is January, with an average hourly wind speed of 9.9 miles per hour.
The calmer time of year lasts for 6.8 months, from April 18 to November 11. The calmest month of the year in Boulder is August, with an average hourly wind speed of 5.9 miles per hour.
The predominant average hourly wind direction in Boulder is from the west throughout the year.
Best Time of Year to Visit
To characterize how pleasant the weather is in Boulder throughout the year, we compute two travel scores.
The tourism score favors clear, rainless days with perceived temperatures between 65°F and 80°F. Based on this score, the best time of year to visit Boulder for general outdoor tourist activities is from mid June to early September, with a peak score in the first week of July.
Tourism Score in Boulder
The beach/pool score favors clear, rainless days with perceived temperatures between 75°F and 90°F. Based on this score, the best time of year to visit Boulder for hot-weather activities is from late June to early August, with a peak score in the second week of July.
Beach/Pool Score in Boulder
For each hour between 8:00 AM and 9:00 PM of each day in the analysis period (1980 to 2016), independent scores are computed for perceived temperature, cloud cover, and total precipitation. Those scores are combined into a single hourly composite score, which is then aggregated into days, averaged over all the years in the analysis period, and smoothed.
Our cloud cover score is 10 for fully clear skies, falling linearly to 9 for mostly clear skies, and to 1 for fully overcast skies.
Our precipitation score, which is based on the three-hour precipitation centered on the hour in question, is 10 for no precipitation, falling linearly to 9 for trace precipitation, and to 0 for 0.04 inches of precipitation or more.
Our tourism temperature score is 0 for perceived temperatures below 50°F, rising linearly to 9 for 65°F, to 10 for 75°F, falling linearly to 9 for 80°F, and to 1 for 90°F or hotter.
Our beach/pool temperature score is 0 for perceived temperatures below 65°F, rising linearly to 9 for 75°F, to 10 for 82°F, falling linearly to 9 for 90°F, and to 1 for 100°F or hotter.
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 Boulder typically lasts for 5.2 months (158 days), from around May 3 to around October 8, rarely starting before April 11 or after May 21, and rarely ending before September 17 or after October 28.
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.
Based on growing degree days alone, the first spring blooms in Boulder should appear around March 28, only rarely appearing before March 11 or after April 22.
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 experiences extreme seasonal variation over the course of the year.
The brighter period of the year lasts for 2.8 months, from May 10 to August 3, with an average daily incident shortwave energy per square meter above 6.8 kWh. The brightest month of the year in Boulder is June, with an average of 7.8 kWh.
The darker period of the year lasts for 3.2 months, from November 3 to February 9, with an average daily incident shortwave energy per square meter below 3.5 kWh. The darkest month of the year in Boulder is December, with an average of 2.5 kWh.
For the purposes of this report, the geographical coordinates of Boulder are 40.015 deg latitude, -105.271 deg longitude, and 5,328 ft elevation.
The topography within 2 miles of Boulder contains very significant variations in elevation, with a maximum elevation change of 1,627 feet and an average elevation above sea level of 5,464 feet. Within 10 miles contains very significant variations in elevation (4,131 feet). Within 50 miles also contains extreme variations in elevation (9,718 feet).
The area within 2 miles of Boulder is covered by artificial surfaces (70%) and shrubs (25%), within 10 miles by trees (33%) and shrubs (25%), and within 50 miles by trees (39%) and grassland (19%).
This report illustrates the typical weather in Boulder, 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 Boulder.
For each station, the records are corrected for the elevation difference between that station and Boulder 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 Boulder is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Boulder 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 Boulder 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 © OpenStreetMap contributors.
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.
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