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Winter Weather in El Cantón de San Pablo Colombia

Daily high temperatures are around 86°F, rarely falling below 82°F or exceeding 91°F. The highest daily average high temperature is 87°F on February 27.

Daily low temperatures are around 75°F, rarely falling below 73°F or exceeding 78°F. The highest daily average low temperature is 75°F on January 19.

For reference, on February 6, the hottest day of the year, temperatures in El Cantón de San Pablo typically range from 75°F to 87°F, while on October 28, the coldest day of the year, they range from 74°F to 85°F.

Average High and Low Temperature in the Winter in El Cantón de San Pablo

Average High and Low Temperature in the Winter in El Cantón de San PabloDecJanFeb72°F72°F74°F74°F76°F76°F78°F78°F80°F80°F82°F82°F84°F84°F86°F86°F88°F88°F90°F90°F92°F92°F94°F94°F96°F96°FFallSpringFeb 687°FFeb 687°F75°F75°FDec 185°FDec 185°F75°F75°FFeb 2887°FFeb 2887°F75°F75°FJan 186°FJan 186°F75°F75°F
The daily average high (red line) and low (blue line) temperature, with 25th to 75th and 10th to 90th percentile bands. The thin dotted lines are the corresponding average perceived temperatures.

The figure below shows you a compact characterization of the hourly average winter temperatures. 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 the Winter in El Cantón de San Pablo

Average Hourly Temperature in the Winter in El Cantón de San PabloDecJanFeb12 AM12 AM2 AM2 AM4 AM4 AM6 AM6 AM8 AM8 AM10 AM10 AM12 PM12 PM2 PM2 PM4 PM4 PM6 PM6 PM8 PM8 PM10 PM10 PM12 AM12 AMFallSpringwarmhot
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 average hourly temperature, color coded into bands. The shaded overlays indicate night and civil twilight.

Padang, Indonesia (12,086 miles away); Kijang, Indonesia (12,009 miles); and Tulagi, Solomon Islands (8,542 miles) are the far-away foreign places with temperatures most similar to El Cantón de San Pablo (view comparison).

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The winter in El Cantón de San Pablo experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 81% throughout the season. The lowest chance of overcast or mostly cloudy conditions is 77% on January 12.

The clearest day of the winter is January 12, with clear, mostly clear, or partly cloudy conditions 23% of the time.

For reference, on May 7, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 94%, while on January 12, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 23%.

Cloud Cover Categories in the Winter in El Cantón de San Pablo

Cloud Cover Categories in the Winter in El Cantón de San PabloDecJanFeb0%100%10%90%20%80%30%70%40%60%50%50%60%40%70%30%80%20%90%10%100%0%FallSpringMay 76%May 76%Dec 117%Dec 117%Feb 2816%Feb 2816%Jan 122%Jan 122%Feb 119%Feb 119%partly cloudymostly cloudyovercastmostly clear
0% clear 20% mostly clear 40% partly cloudy 60% mostly cloudy 80% overcast 100%
The percentage of time spent in each cloud cover band, categorized by the percentage of the sky covered by clouds.

A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In El Cantón de San Pablo, the chance of a wet day over the course of the winter is very rapidly decreasing, starting the season at 84% and ending it at 68%.

For reference, the year's highest daily chance of a wet day is 87% on November 7, and its lowest chance is 67% on February 10.

Probability of Precipitation in the Winter in El Cantón de San Pablo

Probability of Precipitation in the Winter in El Cantón de San PabloDecJanFeb0%0%10%10%20%20%30%30%40%40%50%50%60%60%70%70%80%80%90%90%FallSpringFeb 567%Feb 567%Dec 184%Dec 184%Feb 2868%Feb 2868%Jan 175%Jan 175%rain
The percentage of days in which various types of precipitation are observed, excluding trace quantities: rain alone, snow alone, and mixed (both rain and snow fell in the same day).

Rainfall

To show variation within the season and not just the monthly totals, we show the rainfall accumulated over a sliding 31-day period centered around each day.

The average sliding 31-day rainfall during the winter in El Cantón de San Pablo is very rapidly decreasing, starting the season at 14.3 inches, when it rarely exceeds 21.0 inches or falls below 6.9 inches, and ending the season at 10.4 inches, when it rarely exceeds 19.3 inches or falls below 3.5 inches.

The lowest average 31-day accumulation is 10.4 inches on February 20.

Average Monthly Rainfall in the Winter in El Cantón de San Pablo

Average Monthly Rainfall in the Winter in El Cantón de San PabloDecJanFeb0 in0 in5 in5 in10 in10 in15 in15 in20 in20 inFallSpringFeb 1710.4 inFeb 1710.4 inDec 114.3 inDec 114.3 inJan 111.8 inJan 111.8 inFeb 110.5 inFeb 110.5 in
The average rainfall (solid line) accumulated over the course of a sliding 31-day period centered on the day in question, with 25th to 75th and 10th to 90th percentile bands. The thin dotted line is the corresponding average snowfall.

Over the course of the winter in El Cantón de San Pablo, the length of the day is essentially constant. The shortest day of the winter is December 21, with 11 hours, 49 minutes of daylight and the longest day is February 28, with 12 hours, 1 minute of daylight.

Hours of Daylight and Twilight in the Winter in El Cantón de San Pablo

Hours of Daylight and Twilight in the Winter in El Cantón de San PabloDecJanFeb0 hr24 hr4 hr20 hr8 hr16 hr12 hr12 hr16 hr8 hr20 hr4 hr24 hr0 hrFallSpringDec 2111 hr, 49 minDec 2111 hr, 49 minnightnightdaydayFeb 2812 hr, 1 minFeb 2812 hr, 1 minFeb 111 hr, 54 minFeb 111 hr, 54 min
The number of hours during which the Sun is visible (black line). From bottom (most yellow) to top (most gray), the color bands indicate: full daylight, twilight (civil, nautical, and astronomical), and full night.

The earliest sunrise of the winter in El Cantón de San Pablo is 6:01 AM on December 1 and the latest sunrise is 22 minutes later at 6:23 AM on February 2.

The earliest sunset is 5:51 PM on December 1 and the latest sunset is 29 minutes later at 6:19 PM on February 22.

Daylight saving time is not observed in El Cantón de San Pablo during 2024.

For reference, on June 20, the longest day of the year, the Sun rises at 5:55 AM and sets 12 hours, 26 minutes later, at 6:21 PM, while on December 21, the shortest day of the year, it rises at 6:10 AM and sets 11 hours, 49 minutes later, at 5:59 PM.

Sunrise & Sunset with Twilight in the Winter in El Cantón de San Pablo

Sunrise & Sunset with Twilight in the Winter in El Cantón de San PabloDecJanFeb12 AM2 AM4 AM6 AM8 AM10 AM12 PM2 PM4 PM6 PM8 PM10 PM12 AMFallSpring6:01 AM6:01 AMDec 15:51 PMDec 15:51 PM6:20 AM6:20 AMFeb 226:19 PMFeb 226:19 PM6:23 AM6:23 AMFeb 26:17 PMFeb 26:17 PM6:16 AM6:16 AMJan 16:05 PMJan 16:05 PMSolarMidnightSolarMidnightSolarNoonSunriseSunset
The solar day in the winter. From bottom to top, the black lines are the previous solar midnight, sunrise, solar noon, sunset, and the next solar midnight. The day, twilights (civil, nautical, and astronomical), and night are indicated by the color bands from yellow to gray.

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.

Solar Elevation and Azimuth in the Winter in El Cantón de San Pablo

Solar Elevation and Azimuth in the Winter in El Cantón de San PabloDecJanFeb12 AM12 AM2 AM2 AM4 AM4 AM6 AM6 AM8 AM8 AM10 AM10 AM12 PM12 PM2 PM2 PM4 PM4 PM6 PM6 PM8 PM8 PM10 PM10 PM12 AM12 AMFallSpring001020203030405050606080001010203030404050606070
northeastsouthwest
Solar elevation and azimuth in the the winter of 2024. The black lines are lines of constant solar elevation (the angle of the sun above the horizon, in degrees). The background color fills indicate the azimuth (the compass bearing) of the sun. The lightly tinted areas at the boundaries of the cardinal compass points indicate the implied intermediate directions (northeast, southeast, southwest, and northwest).

The figure below presents a compact representation of key lunar data for the winter of 2024. 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 the Winter in El Cantón de San Pablo

Moon Rise, Set & Phases in the Winter in El Cantón de San PabloDecJanFeb12 AM12 AM4 AM4 AM8 AM8 AM12 PM12 PM4 PM4 PM8 PM8 PM12 AM12 AMFallSpringNov 17:48 AMNov 17:48 AMNov 154:29 PMNov 154:29 PMDec 11:22 AMDec 11:22 AMDec 154:02 AMDec 154:02 AMDec 305:28 PMDec 305:28 PMJan 135:28 PMJan 135:28 PMJan 297:37 AMJan 297:37 AMFeb 128:54 AMFeb 128:54 AMFeb 277:45 PMFeb 277:45 PMMar 141:55 AMMar 141:55 AMMar 295:58 AMMar 295:58 AM5:57 PM5:57 PM5:41 PM5:41 PM6:31 AM6:31 AM6:14 AM6:14 AM5:23 PM5:23 PM6:18 AM6:18 AM5:56 AM5:56 AM6:01 PM6:01 PM6:10 PM6:10 PM6:58 AM6:58 AM6:41 PM6:41 PM5:48 PM5:48 PM6:26 AM6:26 AM5:58 AM5:58 AM6:15 PM6:15 PM6:02 PM6:02 PM6:24 AM6:24 AM6:39 PM6:39 PM
The time in which the moon is above the horizon (light blue area), with new moons (dark gray lines) and full moons (blue lines) indicated. The shaded overlays indicate night and civil twilight.

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 El Cantón de San Pablo is essentially constant during the winter, remaining around 100% throughout.

For reference, on January 1, the muggiest day of the year, there are muggy conditions 100% of the time, while on March 11, the least muggy day of the year, there are muggy conditions 100% of the time.

Humidity Comfort Levels in the Winter in El Cantón de San Pablo

Humidity Comfort Levels in the Winter in El Cantón de San PabloDecJanFeb0%0%10%10%20%20%30%30%40%40%50%50%60%60%70%70%80%80%90%90%100%100%FallSpringDec 1100%Dec 1100%Feb 28100%Feb 28100%Jan 1100%Jan 1100%Feb 1100%Feb 1100%miserablemiserableoppressiveoppressivemuggymuggy
dry 55°F comfortable 60°F humid 65°F muggy 70°F oppressive 75°F miserable
The percentage of time spent at various humidity comfort levels, categorized by dew point.

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 El Cantón de San Pablo is essentially constant during the winter, remaining within 0.1 miles per hour of 2.0 miles per hour throughout.

For reference, on October 27, the windiest day of the year, the daily average wind speed is 2.1 miles per hour, while on July 3, the calmest day of the year, the daily average wind speed is 1.8 miles per hour.

Average Wind Speed in the Winter in El Cantón de San Pablo

Average Wind Speed in the Winter in El Cantón de San PabloDecJanFeb0.0 mph0.0 mph0.5 mph0.5 mph1.0 mph1.0 mph1.5 mph1.5 mph2.0 mph2.0 mph2.5 mph2.5 mph3.0 mph3.0 mph3.5 mph3.5 mphFallSpringDec 12.1 mphDec 12.1 mphFeb 281.9 mphFeb 281.9 mphJan 12.0 mphJan 12.0 mphFeb 12.0 mphFeb 12.0 mph
The average of mean hourly wind speeds (dark gray line), with 25th to 75th and 10th to 90th percentile bands.

The hourly average wind direction in El Cantón de San Pablo throughout the winter is predominantly from the west, with a peak proportion of 81% on February 23.

Wind Direction in the Winter in El Cantón de San Pablo

Wind Direction in the Winter in El Cantón de San PabloDecJanFeb0%100%20%80%40%60%60%40%80%20%100%0%FallSpringwestsouth
northeastsouthwest
The percentage of hours in which the mean wind direction is from each of the four cardinal wind directions, excluding hours in which the mean wind speed is less than 1.0 mph. The lightly tinted areas at the boundaries are the percentage of hours spent in the implied intermediate directions (northeast, southeast, southwest, and northwest).

El Cantón de San Pablo 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 El Cantón de San Pablo is essentially constant during the winter, remaining around 80°F throughout.

Average Water Temperature in the Winter in El Cantón de San Pablo

Average Water Temperature in the Winter in El Cantón de San PabloDecJanFeb76°F76°F77°F77°F78°F78°F79°F79°F80°F80°F81°F81°F82°F82°F83°F83°FFallSpringDec 180°FDec 180°FFeb 2880°FFeb 2880°FJan 180°FJan 180°FFeb 180°FFeb 180°F
The daily average water temperature (purple line), with 25th to 75th and 10th to 90th percentile bands.

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 El Cantón de San Pablo 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 the Winter in El Cantón de San Pablo

Time Spent in Various Temperature Bands and the Growing Season in the Winter in El Cantón de San PabloDecJanFeb0%100%10%90%20%80%30%70%40%60%50%50%60%40%70%30%80%20%90%10%100%0%FallSpring100%Jan 15100%Jan 15comfortablewarmhot
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 percentage of time spent in various temperature bands. The black line is the percentage chance that a given day is within the growing season.

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 El Cantón de San Pablo are very rapidly decreasing during the winter, decreasing by 8,214°F, from 9,936°F to 1,722°F, over the course of the season.

Growing Degree Days in the Winter in El Cantón de San Pablo

Growing Degree Days in the Winter in El Cantón de San PabloDecJanFeb2,000°F2,000°F4,000°F4,000°F6,000°F6,000°F8,000°F8,000°F10,000°F10,000°FFallSpringDec 19,936°FDec 19,936°FFeb 281,722°FFeb 281,722°F
The average growing degree days accumulated over the course of the winter, with 25th to 75th and 10th to 90th percentile bands.

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 El Cantón de San Pablo is gradually increasing during the winter, rising by 0.7 kWh, from 3.8 kWh to 4.5 kWh, over the course of the season.

The highest average daily incident shortwave solar energy during the winter is 4.5 kWh on February 27.

Average Daily Incident Shortwave Solar Energy in the Winter in El Cantón de San Pablo

Average Daily Incident Shortwave Solar Energy in the Winter in El Cantón de San PabloDecJanFeb0 kWh0 kWh1 kWh1 kWh2 kWh2 kWh3 kWh3 kWh4 kWh4 kWh5 kWh5 kWh6 kWh6 kWhFallSpringFeb 274.5 kWhFeb 274.5 kWhDec 13.8 kWhDec 13.8 kWhJan 14.1 kWhJan 14.1 kWhFeb 14.4 kWhFeb 14.4 kWh
The average daily shortwave solar energy reaching the ground per square meter (orange line), with 25th to 75th and 10th to 90th percentile bands.

For the purposes of this report, the geographical coordinates of El Cantón de San Pablo are 5.339 deg latitude, -76.731 deg longitude, and 174 ft elevation.

The topography within 2 miles of El Cantón de San Pablo contains only modest variations in elevation, with a maximum elevation change of 174 feet and an average elevation above sea level of 218 feet. Within 10 miles contains only modest variations in elevation (640 feet). Within 50 miles contains significant variations in elevation (13,510 feet).

The area within 2 miles of El Cantón de San Pablo is covered by trees (99%), within 10 miles by trees (83%) and grassland (11%), and within 50 miles by trees (72%).

This report illustrates the typical weather in El Cantón de San Pablo, 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 El Cantón de San Pablo.

For each station, the records are corrected for the elevation difference between that station and El Cantón de San Pablo 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 El Cantón de San Pablo is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between El Cantón de San Pablo 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 El Cantón de San Pablo 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.

Other 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.

Disclaimer

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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