Average Weather in March in Big Bear Lake California, United States
In Big Bear Lake, the month of March is characterized by rising daily high temperatures, with daily highs increasing by 6°F, from 50°F to 56°F over the course of the month, and rarely exceeding 67°F or dropping below 39°F.
Daily low temperatures increase by 4°F, from 28°F to 32°F, rarely falling below 20°F or exceeding 39°F.
For reference, on July 27, the hottest day of the year, temperatures in Big Bear Lake typically range from 54°F to 81°F, while on December 25, the coldest day of the year, they range from 22°F to 43°F.
Average High and Low Temperature in March
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on March. 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 March
The month of March in Big Bear Lake experiences decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 44% to 32%.
The clearest day of the month is March 30, with clear, mostly clear, or partly cloudy conditions 68% of the time.
For reference, on February 21, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 46%, while on September 7, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 89%.
Cloud Cover Categories in March
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Big Bear Lake, the chance of a wet day over the course of March is rapidly decreasing, starting the month at 14% and ending it at 7%.
For reference, the year's highest daily chance of a wet day is 15% on February 21, and its lowest chance is 1% on June 14.
Over the course of March in Big Bear Lake, the chance of a day with only rain decreases from 7% to 4%, the chance of a day with mixed snow and rain decreases from 5% to 3%, and the chance of a day with only snow remains an essentially constant 1% throughout.
Probability of Precipitation in March
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 March in Big Bear Lake is decreasing, starting the month at 0.9 inches, when it rarely exceeds 2.7 inches, and ending the month at 0.3 inches, when it rarely exceeds 0.9 inches.
Average Monthly Rainfall in March
We report snowfall in liquid-equivalent terms. The actual depth of new snowfall is typically between 5 and 10 times the liquid-equivalent amount, assuming the ground is frozen. As with rainfall, we consider the liquid-equivalent snowfall accumulated over a sliding 31-day period centered around each day.
The average sliding 31-day liquid-equivalent snowfall during March in Big Bear Lake is essentially constant, remaining about 0.2 inches throughout, and rarely exceeding 0.9 inches or falling below -0.0 inches.
Average Monthly Liquid-Equivalent Snowfall in March
Over the course of March in Big Bear Lake, the length of the day is rapidly increasing. From the start to the end of the month, the length of the day increases by 1 hour, 4 minutes, implying an average daily increase of 2 minutes, 8 seconds, and weekly increase of 14 minutes, 59 seconds.
The shortest day of the month is March 1, with 11 hours, 28 minutes of daylight and the longest day is March 31, with 12 hours, 32 minutes of daylight.
Hours of Daylight and Twilight in March
The earliest sunrise of the month in Big Bear Lake is 6:03 AM on March 11 and the latest sunrise is 59 minutes later at 7:01 AM on March 12.
The earliest sunset is 5:44 PM on March 1 and the latest sunset is 1 hour, 24 minutes later at 7:08 PM on March 31.
Daylight saving time (DST) starts at 3:00 AM on March 12, 2017, shifting sunrise and sunset to be an hour later.
For reference, on June 21, the longest day of the year, the Sun rises at 5:36 AM and sets 14 hours, 27 minutes later, at 8:02 PM, while on December 21, the shortest day of the year, it rises at 6:49 AM and sets 9 hours, 52 minutes later, at 4:42 PM.
Sunrise & Sunset with Twilight and Daylight Saving Time in March
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 Big Bear Lake is essentially constant during March, remaining around 0% throughout.
For reference, on August 10, the muggiest day of the year, there are muggy conditions 0% 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 March
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 Big Bear Lake is gradually increasing during March, increasing from 7.7 miles per hour to 8.3 miles per hour over the course of the month.
For reference, on April 26, the windiest day of the year, the daily average wind speed is 8.7 miles per hour, while on September 8, the calmest day of the year, the daily average wind speed is 6.2 miles per hour.
Average Wind Speed in March
Wind Direction in March
Big Bear Lake is located near a large body of water (e.g., ocean, sea, or large lake). This section reports on the wide-area average surface temperature of that water.
The average surface water temperature in Big Bear Lake is essentially constant during March, remaining around 59°F throughout.
Average Water Temperature in March
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 Big Bear Lake is rapidly increasing during March, rising by 1.7 kWh, from 5.0 kWh to 6.6 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in March
For the purposes of this report, the geographical coordinates of Big Bear Lake are 34.244 deg latitude, -116.911 deg longitude, and 6,988 ft elevation.
The topography within 2 miles of Big Bear Lake contains very significant variations in elevation, with a maximum elevation change of 1,421 feet and an average elevation above sea level of 7,001 feet. Within 10 miles contains very significant variations in elevation (7,831 feet). Within 50 miles also contains extreme variations in elevation (11,447 feet).
The area within 2 miles of Big Bear Lake is covered by trees (63%), shrubs (18%), and water (18%), within 10 miles by trees (52%) and shrubs (45%), and within 50 miles by shrubs (79%).
This report illustrates the typical weather in Big Bear Lake 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 Big Bear Lake.
For each station, the records are corrected for the elevation difference between that station and Big Bear Lake 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 Big Bear Lake is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Big Bear Lake and a given station.
The stations contributing to this reconstruction are: San Bernardino International Airport (18%, 34 kilometers, southwest); Southern California Logistics Airport (27%, 57 kilometers, northwest); Palm Springs International Airport (14%, 60 kilometers, southeast); Twenty-Nine Palms, Marine Corps Air-Ground Combat Center (21%, 69 kilometers, east); and Barstow Daggett County Airport (20%, 69 kilometers, north).
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.