Average Weather in August in Londres Argentina
Daily high temperatures increase by 5°F, from 74°F to 79°F, rarely falling below 62°F or exceeding 91°F.
Daily low temperatures increase by 3°F, from 48°F to 51°F, rarely falling below 39°F or exceeding 58°F.
For reference, on December 24, the hottest day of the year, temperatures in Londres typically range from 67°F to 90°F, while on July 17, the coldest day of the year, they range from 47°F to 73°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
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
Zephyrhills North, Florida, United States (3,997 miles away); Windhoek, Namibia (5,180 miles); and Biloela, Australia (8,059 miles) are the far-away foreign places with temperatures most similar to Londres (view comparison).
The month of August in Londres experiences gradually decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 19% to 14%.
The clearest day of the month is August 31, with clear, mostly clear, or partly cloudy conditions 86% of the time.
For reference, on June 11, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 30%, while on September 27, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 87%.
Cloud Cover Categories in August
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 Londres, the chance of a wet day over the course of August is essentially constant, remaining around 2% throughout.
For reference, the year's highest daily chance of a wet day is 33% on January 2, and its lowest chance is 1% on August 8.
Probability of Precipitation in August
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 August in Londres is essentially constant, remaining about 0.1 inches throughout, and rarely exceeding 0.6 inches or falling below -0.0 inches.
The lowest average 31-day accumulation is 0.1 inches on August 19.
Average Monthly Rainfall in August
Over the course of August in Londres, the length of the day is increasing. From the start to the end of the month, the length of the day increases by 42 minutes, implying an average daily increase of 1 minute, 24 seconds, and weekly increase of 9 minutes, 45 seconds.
The shortest day of the month is August 1, with 10 hours, 50 minutes of daylight and the longest day is August 31, with 11 hours, 32 minutes of daylight.
Hours of Daylight and Twilight in August
The latest sunrise of the month in Londres is 8:09 AM on August 1 and the earliest sunrise is 27 minutes earlier at 7:42 AM on August 31.
The earliest sunset is 7:00 PM on August 1 and the latest sunset is 15 minutes later at 7:14 PM on August 31.
Daylight saving time is not observed in Londres during 2021.
For reference, on December 21, the longest day of the year, the Sun rises at 6:29 AM and sets 13 hours, 54 minutes later, at 8:23 PM, while on June 21, the shortest day of the year, it rises at 8:18 AM and sets 10 hours, 23 minutes later, at 6:42 PM.
Sunrise & Sunset with Twilight in August
The figure below presents a compact representation of key lunar data for August 2021. 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. The label associated with each bar indicates the date and time that the phase is obtained, and the companion time labels indicate the rise and set times of the Moon for the nearest time interval in which the moon is above the horizon.
Moon Rise, Set & Phases 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 Londres is essentially constant during August, remaining around 0% throughout.
For reference, on February 4, the muggiest day of the year, there are muggy conditions 1% of the time, while on April 22, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in August
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 Londres is gradually increasing during August, increasing from 5.5 miles per hour to 6.2 miles per hour over the course of the month.
For reference, on November 22, the windiest day of the year, the daily average wind speed is 8.1 miles per hour, while on June 14, the calmest day of the year, the daily average wind speed is 4.8 miles per hour.
Average Wind Speed in August
The hourly average wind direction in Londres throughout August is predominantly from the east, with a peak proportion of 35% on August 31.
Wind Direction in August
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).
While it does not do so every year, freezing temperatures are seen in Londres over some winters. The day least likely to be in the growing season is July 16, with a 78% chance.
Time Spent in Various Temperature Bands and the Growing Season in August
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 Londres are increasing during August, increasing by 348°F, from 274°F to 622°F, over the course of the month.
Growing Degree Days 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 Londres is increasing during August, rising by 1.2 kWh, from 4.9 kWh to 6.1 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 Londres are -27.714 deg latitude, -67.133 deg longitude, and 4,009 ft elevation.
The topography within 2 miles of Londres contains very significant variations in elevation, with a maximum elevation change of 1,476 feet and an average elevation above sea level of 4,058 feet. Within 10 miles contains very significant variations in elevation (6,562 feet). Within 50 miles also contains extreme variations in elevation (13,655 feet).
The area within 2 miles of Londres is covered by shrubs (56%), cropland (18%), grassland (14%), and trees (12%), within 10 miles by shrubs (65%) and trees (14%), and within 50 miles by bare soil (44%) and sparse vegetation (18%).
This report illustrates the typical weather in Londres, based on a statistical analysis of historical hourly weather reports and model reconstructions from January 1, 1980 to December 31, 2016.
Londres is further than 200 kilometers from the nearest reliable weather station, so the weather-related data on this page were taken entirely from NASA's MERRA-2 satellite-era reanalysis . 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.
The temperature and dew point estimates are corrected for the difference between the reference elevation of the MERRA-2 grid cell and the elevation of Londres, according to the International Standard Atmosphere .
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.
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 © 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.