March Weather in Santiago de María El Salvador
Daily high temperatures are around 85°F, rarely falling below 81°F or exceeding 88°F.
Daily low temperatures are around 65°F, rarely falling below 61°F or exceeding 69°F.
For reference, on April 5, the hottest day of the year, temperatures in Santiago de María typically range from 66°F to 85°F, while on January 21, the coldest day of the year, they range from 63°F to 83°F.
Average High and Low Temperature in March in Santiago de María
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on March. 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 March in Santiago de María
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
Mwanza, Tanzania (8,374 miles away); Cimahi, Indonesia (11,269 miles); and Kalilangan, Philippines (9,736 miles) are the far-away foreign places with temperatures most similar to Santiago de María (view comparison).
The month of March in Santiago de María experiences increasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy increasing from 28% to 39%.
The clearest day of the month is March 1, with clear, mostly clear, or partly cloudy conditions 72% of the time.
For reference, on June 5, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 92%, while on January 17, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 79%.
Cloud Cover Categories in March in Santiago de María
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 Santiago de María, the chance of a wet day over the course of March is gradually increasing, starting the month at 1% and ending it at 4%.
For reference, the year's highest daily chance of a wet day is 45% on September 12, and its lowest chance is 1% on January 18.
Probability of Precipitation in March in Santiago de María
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 March in Santiago de María is essentially constant, remaining about 0.2 inches throughout, and rarely exceeding 0.8 inches or falling below -0.0 inches.
Average Monthly Rainfall in March in Santiago de María
Over the course of March in Santiago de María, the length of the day is gradually increasing. From the start to the end of the month, the length of the day increases by 23 minutes, implying an average daily increase of 45 seconds, and weekly increase of 5 minutes, 15 seconds.
The shortest day of the month is March 1, with 11 hours, 53 minutes of daylight and the longest day is March 31, with 12 hours, 15 minutes of daylight.
Hours of Daylight and Twilight in March in Santiago de María
The latest sunrise of the month in Santiago de María is 6:09 AM on March 1 and the earliest sunrise is 19 minutes earlier at 5:50 AM on March 31.
The earliest sunset is 6:02 PM on March 1 and the latest sunset is 3 minutes later at 6:05 PM on March 31.
Daylight saving time is not observed in Santiago de María during 2021.
For reference, on June 21, the longest day of the year, the Sun rises at 5:28 AM and sets 12 hours, 55 minutes later, at 6:23 PM, while on December 21, the shortest day of the year, it rises at 6:12 AM and sets 11 hours, 20 minutes later, at 5:32 PM.
Sunrise & Sunset with Twilight in March in Santiago de María
The figure below presents a compact representation of key lunar data for March 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 March in Santiago de María
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 Santiago de María is very rapidly increasing during March, rising from 29% to 57% over the course of the month.
For reference, on September 18, the muggiest day of the year, there are muggy conditions 100% of the time, while on January 15, the least muggy day of the year, there are muggy conditions 15% of the time.
Humidity Comfort Levels in March in Santiago de María
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 Santiago de María is gradually decreasing during March, decreasing from 7.4 miles per hour to 6.9 miles per hour over the course of the month.
For reference, on January 14, the windiest day of the year, the daily average wind speed is 7.6 miles per hour, while on August 27, the calmest day of the year, the daily average wind speed is 5.1 miles per hour.
Average Wind Speed in March in Santiago de María
The wind direction in Santiago de María during March is predominantly out of the east from March 1 to March 12 and the south from March 12 to March 31.
Wind Direction in March in Santiago de María
Santiago de María 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 Santiago de María is essentially constant during March, remaining within 1°F of 83°F throughout.
Average Water Temperature in March in Santiago de María
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 Santiago de María 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 March in Santiago de María
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 Santiago de María are rapidly increasing during March, increasing by 709°F, from 1,345°F to 2,054°F, over the course of the month.
Growing Degree Days in March in Santiago de María
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 Santiago de María is essentially constant during March, remaining within 0.1 kWh of 6.9 kWh throughout.
The highest average daily incident shortwave solar energy during March is 7.0 kWh on March 24.
Average Daily Incident Shortwave Solar Energy in March in Santiago de María
For the purposes of this report, the geographical coordinates of Santiago de María are 13.483 deg latitude, -88.467 deg longitude, and 2,940 ft elevation.
The topography within 2 miles of Santiago de María contains large variations in elevation, with a maximum elevation change of 2,467 feet and an average elevation above sea level of 3,099 feet. Within 10 miles contains large variations in elevation (5,266 feet). Within 50 miles also contains extreme variations in elevation (7,149 feet).
The area within 2 miles of Santiago de María is covered by trees (68%) and cropland (22%), within 10 miles by cropland (42%) and trees (35%), and within 50 miles by water (31%) and cropland (29%).
This report illustrates the typical weather in Santiago de María, 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 Santiago de María.
For each station, the records are corrected for the elevation difference between that station and Santiago de María 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 Santiago de María is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Santiago de María and a given station.
The stations contributing to this reconstruction are: Aeropuerto Internacional El Salvador (MSLP, 45%, 64 kilometers, west); Soto Cano Air Base (MHSC, 31%, 136 kilometers, northeast); and Choluteca (MHCH, 24%, 140 kilometers, east).
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 © 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.