Average Weather in November in Quepos Costa Rica
In Quepos, the month of November is characterized by essentially constant daily high temperatures, with daily highs around 88°F throughout the month, rarely exceeding 92°F or dropping below 84°F.
Daily low temperatures are around 78°F, rarely falling below 76°F or exceeding 81°F.
For reference, on March 18, the hottest day of the year, temperatures in Quepos typically range from 80°F to 92°F, while on October 2, the coldest day of the year, they range from 78°F to 88°F.
Average High and Low Temperature in November
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on November. 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 November
The month of November in Quepos experiences very rapidly decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 87% to 62%.
The clearest day of the month is November 30, with clear, mostly clear, or partly cloudy conditions 38% of the time.
For reference, on May 28, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 95%, while on January 1, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 63%.
Cloud Cover Categories in November
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Quepos, the chance of a wet day over the course of November is very rapidly decreasing, starting the month at 50% and ending it at 34%.
For reference, the year's highest daily chance of a wet day is 56% on October 7, and its lowest chance is 8% on March 16.
Probability of Precipitation in November
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 November in Quepos is very rapidly decreasing, starting the month at 6.5 inches, when it rarely exceeds 11.9 inches or falls below 2.3 inches, and ending the month at 3.8 inches, when it rarely exceeds 7.7 inches or falls below 0.9 inches.
Average Monthly Rainfall in November
Over the course of November in Quepos, the length of the day is essentially constant. The shortest day of the month is November 30, with 11 hours, 37 minutes of daylight and the longest day is November 1, with 11 hours, 47 minutes of daylight.
Hours of Daylight and Twilight in November
The earliest sunrise of the month in Quepos is 5:26 AM on November 1 and the latest sunrise is 10 minutes later at 5:36 AM on November 30.
The earliest sunset is 5:12 PM on November 15 and the latest sunset is 1 minute, 57 seconds later at 5:13 PM on November 30.
Daylight saving time is not observed in Quepos during 2017.
For reference, on June 21, the longest day of the year, the Sun rises at 5:18 AM and sets 12 hours, 41 minutes later, at 5:58 PM, while on December 21, the shortest day of the year, it rises at 5:47 AM and sets 11 hours, 35 minutes later, at 5:22 PM.
Sunrise & Sunset with Twilight in November
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 Quepos is decreasing during November, falling from 98% to 88% over the course of the month.
For reference, on June 3, the muggiest day of the year, there are muggy conditions 99% of the time, while on February 10, the least muggy day of the year, there are muggy conditions 50% of the time.
Humidity Comfort Levels in November
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 Quepos is decreasing during November, decreasing from 5.8 miles per hour to 4.6 miles per hour over the course of the month.
For reference, on October 10, the windiest day of the year, the daily average wind speed is 6.4 miles per hour, while on January 19, the calmest day of the year, the daily average wind speed is 3.3 miles per hour.
Average Wind Speed in November
Wind Direction in November
Quepos 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 Quepos is essentially constant during November, remaining around 82°F throughout.
The lowest average surface water temperature during November is 82°F on November 12.
Average Water Temperature in November
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).
Temperatures in Quepos are sufficiently warm year round that it is not entirely meaningful to discuss the growing season in these terms. We nevertheless include the chart below as an illustration of the distribution of temperatures experienced throughout the year.
Time Spent in Various Temperature Bands and the Growing Season in November
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 Quepos is very rapidly increasing during November, increasing by 929°F, from 9,972°F to 10,901°F, over the course of the month.
Growing Degree Days in November
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 Quepos is gradually increasing during November, rising by 0.8 kWh, from 3.7 kWh to 4.5 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in November
For the purposes of this report, the geographical coordinates of Quepos are 9.417 deg latitude, -84.167 deg longitude, and 20 ft elevation.
The topography within 2 miles of Quepos contains significant variations in elevation, with a maximum elevation change of 643 feet and an average elevation above sea level of 115 feet. Within 10 miles contains significant variations in elevation (2,802 feet). Within 50 miles contains large variations in elevation (12,490 feet).
The area within 2 miles of Quepos is covered by water (49%) and trees (29%), within 10 miles by water (53%) and trees (25%), and within 50 miles by water (55%) and trees (24%).
This report illustrates the typical weather in Quepos 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 is only a single weather station, Juan Santamaría International Airport, in our network suitable to be used as a proxy for the historical temperature and dew point records of Quepos.
At a distance of 64 kilometers from Quepos, closer than our threshold of 150 kilometers, this station is deemed sufficiently nearby to be relied upon as our primary source for temperature and dew point records.
The station records are corrected for the elevation difference between the station and Quepos according to the International Standard Atmosphere , and by the relative change present in the MERRA-2 satellite-era reanalysis between the two locations.
Please note that the station records themselves may additionally have been back-filled using other nearby stations or the MERRA-2 reanalysis.
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.