Average Weather in February in London United Kingdom
Daily high temperatures increase by 2°F, from 47°F to 49°F, rarely falling below 38°F or exceeding 56°F.
Daily low temperatures are around 39°F, rarely falling below 31°F or exceeding 47°F. The lowest daily average low temperature is 39°F on February 7.
For reference, on August 1, the hottest day of the year, temperatures in London typically range from 60°F to 74°F, while on February 7, the coldest day of the year, they range from 39°F to 47°F.
Average High and Low Temperature in February
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on February. 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 February
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
The month of February in London experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 66% throughout the month.
The clearest day of the month is February 26, with clear, mostly clear, or partly cloudy conditions 36% of the time.
For reference, on December 27, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 74%, while on July 15, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 58%.
Cloud Cover Categories in February
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 London, the chance of a wet day over the course of February is rapidly decreasing, starting the month at 27% and ending it at 21%.
For reference, the year's highest daily chance of a wet day is 32% on December 30, and its lowest chance is 20% on April 28.
Probability of Precipitation in February
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 February in London is gradually decreasing, starting the month at 1.6 inches, when it rarely exceeds 3.4 inches or falls below 0.4 inches, and ending the month at 1.3 inches, when it rarely exceeds 2.4 inches or falls below 0.4 inches.
Average Monthly Rainfall in February
Over the course of February in London, 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, 40 minutes, implying an average daily increase of 3 minutes, 42 seconds, and weekly increase of 25 minutes, 51 seconds.
The shortest day of the month is February 1, with 9 hours, 10 minutes of daylight and the longest day is February 28, with 10 hours, 50 minutes of daylight.
Hours of Daylight and Twilight in February
The latest sunrise of the month in London is 7:39 AM on February 1 and the earliest sunrise is 51 minutes earlier at 6:48 AM on February 28.
The earliest sunset is 4:49 PM on February 1 and the latest sunset is 49 minutes later at 5:38 PM on February 28.
Daylight saving time is observed in London during 2019, but it neither starts nor ends during February, so the entire month is in standard time.
For reference, on June 21, the longest day of the year, the Sun rises at 4:43 AM and sets 16 hours, 38 minutes later, at 9:21 PM, while on December 22, the shortest day of the year, it rises at 8:04 AM and sets 7 hours, 50 minutes later, at 3:53 PM.
Sunrise & Sunset with Twilight and Daylight Saving Time in February
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 London is essentially constant during February, remaining around 0% throughout.
For reference, on August 11, 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 February
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 London is essentially constant during February, remaining within 0.2 miles per hour of 12.6 miles per hour throughout.
For reference, on January 3, 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 9.6 miles per hour.
Average Wind Speed in February
The hourly average wind direction in London throughout February is predominantly from the west, with a peak proportion of 37% on February 1.
Wind Direction in February
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 London typically lasts for 9.8 months (297 days), from around February 22 to around December 16, rarely starting after March 27, or ending before November 14.
During February in London, the chance that a given day is within the growing season is rapidly increasing rising from 20% to 60% over the course of the month.
Time Spent in Various Temperature Bands and the Growing Season in February
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
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 London are essentially constant during February, remaining within 6°F of 22°F throughout.
Growing Degree Days in February
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 London is increasing during February, rising by 1.0 kWh, from 1.2 kWh to 2.2 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in February
For the purposes of this report, the geographical coordinates of London are 51.509 deg latitude, -0.126 deg longitude, and 66 ft elevation.
The topography within 2 miles of London contains only modest variations in elevation, with a maximum elevation change of 164 feet and an average elevation above sea level of 70 feet. Within 10 miles contains only modest variations in elevation (492 feet). Within 50 miles contains significant variations in elevation (1,027 feet).
The area within 2 miles of London is covered by artificial surfaces (96%), within 10 miles by artificial surfaces (97%), and within 50 miles by cropland (40%) and grassland (26%).
This report illustrates the typical weather in London 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 2 weather stations near enough to contribute to our estimation of the temperature and dew point in London.
For each station, the records are corrected for the elevation difference between that station and London 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 London is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between London and a given station.
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.