Average Weather in May in Tlaltizapán Mexico
Daily high temperatures decrease by 3°F, from 94°F to 92°F, rarely falling below 85°F or exceeding 100°F.
Daily low temperatures are around 68°F, rarely falling below 63°F or exceeding 73°F.
For reference, on April 17, the hottest day of the year, temperatures in Tlaltizapán typically range from 66°F to 94°F, while on January 13, the coldest day of the year, they range from 56°F to 86°F.
Average High and Low Temperature in May
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on May. 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 May
Goiânia, Brazil (4,182 miles away); Mafinga, Tanzania (9,273 miles); and Nanhyanga, Tanzania (9,639 miles) are the far-away foreign places with temperatures most similar to Tlaltizapán (view comparison).
The month of May in Tlaltizapán experiences very rapidly increasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy increasing from 46% to 66%.
The clearest day of the month is May 1, with clear, mostly clear, or partly cloudy conditions 54% of the time.
For reference, on September 15, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 88%, while on February 24, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 71%.
Cloud Cover Categories in May
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Tlaltizapán, the chance of a wet day over the course of May is very rapidly increasing, starting the month at 13% and ending it at 46%.
For reference, the year's highest daily chance of a wet day is 78% on August 27, and its lowest chance is 1% on December 9.
Probability of Precipitation in May
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 May in Tlaltizapán is very rapidly increasing, starting the month at 0.7 inches, when it rarely exceeds 1.5 inches, and ending the month at 3.4 inches, when it rarely exceeds 5.6 inches or falls below 1.2 inches.
Average Monthly Rainfall in May
Over the course of May in Tlaltizapán, the length of the day is gradually increasing. From the start to the end of the month, the length of the day increases by 21 minutes, implying an average daily increase of 42 seconds, and weekly increase of 4 minutes, 54 seconds.
The shortest day of the month is May 1, with 12 hours, 50 minutes of daylight and the longest day is May 31, with 13 hours, 11 minutes of daylight.
Hours of Daylight and Twilight in May
The latest sunrise of the month in Tlaltizapán is 7:08 AM on May 1 and the earliest sunrise is 10 minutes earlier at 6:58 AM on May 31.
The earliest sunset is 7:58 PM on May 1 and the latest sunset is 11 minutes later at 8:09 PM on May 31.
Daylight saving time is observed in Tlaltizapán during 2018, but it neither starts nor ends during May, so the entire month is in daylight saving time.
For reference, on June 21, the longest day of the year, the Sun rises at 7:00 AM and sets 13 hours, 15 minutes later, at 8:16 PM, while on December 21, the shortest day of the year, it rises at 7:04 AM and sets 11 hours, 1 minute later, at 6:04 PM.
Sunrise & Sunset with Twilight in May
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 Tlaltizapán is gradually increasing during May, rising from 0% to 3% over the course of the month.
For reference, on June 21, the muggiest day of the year, there are muggy conditions 5% 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 May
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 Tlaltizapán is gradually decreasing during May, decreasing from 5.0 miles per hour to 4.4 miles per hour over the course of the month.
For reference, on March 13, the windiest day of the year, the daily average wind speed is 5.7 miles per hour, while on September 18, the calmest day of the year, the daily average wind speed is 4.2 miles per hour.
Average Wind Speed in May
Wind Direction in May
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 Tlaltizapán 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 May
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 Tlaltizapán are rapidly increasing during May, increasing by 868°F, from 2,923°F to 3,791°F, over the course of the month.
Growing Degree Days in May
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 Tlaltizapán is gradually decreasing during May, falling by 0.6 kWh, from 7.1 kWh to 6.5 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in May
For the purposes of this report, the geographical coordinates of Tlaltizapán are 18.686 deg latitude, -99.119 deg longitude, and 3,199 ft elevation.
The topography within 2 miles of Tlaltizapán contains very significant variations in elevation, with a maximum elevation change of 820 feet and an average elevation above sea level of 3,187 feet. Within 10 miles contains very significant variations in elevation (2,762 feet). Within 50 miles contains large variations in elevation (15,804 feet).
The area within 2 miles of Tlaltizapán is covered by cropland (83%) and trees (12%), within 10 miles by cropland (55%) and trees (40%), and within 50 miles by cropland (39%) and trees (37%).
This report illustrates the typical weather in Tlaltizapán 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 3 weather stations near enough to contribute to our estimation of the temperature and dew point in Tlaltizapán.
For each station, the records are corrected for the elevation difference between that station and Tlaltizapán 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 Tlaltizapán is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Tlaltizapán and a given station.
The stations contributing to this reconstruction are: Benito Juárez International Airport (37%, 84 kilometers, north); Licenciado Adolfo López Mateos International Airport (28%, 86 kilometers, northwest); and Hermanos Serdán International Airport (35%, 95 kilometers, northeast).
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.