Average Weather in March in Miranda Brazil
Daily high temperatures are around 89°F, rarely falling below 82°F or exceeding 96°F.
Daily low temperatures are around 73°F, rarely falling below 67°F or exceeding 77°F.
For reference, on October 16, the hottest day of the year, temperatures in Miranda typically range from 72°F to 93°F, while on July 20, the coldest day of the year, they range from 61°F to 83°F.
Average High and Low Temperature in March
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
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 month of March in Miranda experiences rapidly decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 64% to 51%.
The clearest day of the month is March 31, with clear, mostly clear, or partly cloudy conditions 49% of the time.
For reference, on January 23, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 71%, while on August 26, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 73%.
Cloud Cover Categories in March
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 Miranda, the chance of a wet day over the course of March is very rapidly decreasing, starting the month at 54% and ending it at 38%.
For reference, the year's highest daily chance of a wet day is 57% on January 21, and its lowest chance is 10% on July 13.
Probability of Precipitation in March
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 Miranda is rapidly decreasing, starting the month at 5.3 inches, when it rarely exceeds 8.7 inches or falls below 2.7 inches, and ending the month at 3.9 inches, when it rarely exceeds 6.0 inches or falls below 1.6 inches.
Average Monthly Rainfall in March
Over the course of March in Miranda, the length of the day is decreasing. From the start to the end of the month, the length of the day decreases by 35 minutes, implying an average daily decrease of 1 minute, 10 seconds, and weekly decrease of 8 minutes, 9 seconds.
The shortest day of the month is March 31, with 11 hours, 55 minutes of daylight and the longest day is March 1, with 12 hours, 29 minutes of daylight.
Hours of Daylight and Twilight in March
The earliest sunrise of the month in Miranda is 5:42 AM on March 1 and the latest sunrise is 9 minutes later at 5:52 AM on March 31.
The latest sunset is 6:12 PM on March 1 and the earliest sunset is 26 minutes earlier at 5:46 PM on March 31.
Daylight saving time is observed in Miranda during 2019, but it neither starts nor ends during March, so the entire month is in standard time.
For reference, on December 22, the longest day of the year, the Sun rises at 6:03 AM and sets 13 hours, 22 minutes later, at 7:24 PM, while on June 21, the shortest day of the year, it rises at 6:20 AM and sets 10 hours, 54 minutes later, at 5:14 PM.
Sunrise & Sunset with Twilight and Daylight Saving Time in March
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 Miranda is decreasing during March, falling from 96% to 90% over the course of the month.
For reference, on January 23, the muggiest day of the year, there are muggy conditions 97% of the time, while on August 4, the least muggy day of the year, there are muggy conditions 13% of the time.
Humidity Comfort Levels in March
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 Miranda is essentially constant during March, remaining within 0.1 miles per hour of 4.1 miles per hour throughout.
For reference, on September 9, the windiest day of the year, the daily average wind speed is 6.5 miles per hour, while on March 6, the calmest day of the year, the daily average wind speed is 3.9 miles per hour.
The lowest daily average wind speed during March is 3.9 miles per hour on March 6.
Average Wind Speed in March
Wind Direction in March
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 Miranda 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
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 Miranda are rapidly increasing during March, increasing by 886°F, from 6,876°F to 7,762°F, over the course of the month.
Growing Degree Days in March
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 Miranda is essentially constant during March, remaining within 0.2 kWh of 5.9 kWh throughout.
Average Daily Incident Shortwave Solar Energy in March
For the purposes of this report, the geographical coordinates of Miranda are -20.241 deg latitude, -56.378 deg longitude, and 404 ft elevation.
The topography within 2 miles of Miranda contains only modest variations in elevation, with a maximum elevation change of 154 feet and an average elevation above sea level of 408 feet. Within 10 miles contains only modest variations in elevation (636 feet). Within 50 miles contains significant variations in elevation (2,474 feet).
The area within 2 miles of Miranda is covered by cropland (36%), shrubs (26%), trees (21%), and grassland (16%), within 10 miles by trees (40%) and cropland (29%), and within 50 miles by trees (49%) and shrubs (20%).
This report illustrates the typical weather in Miranda 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, Corumbá International Airport, in our network suitable to be used as a proxy for the historical temperature and dew point records of Miranda.
At a distance of 193 kilometers from Miranda, further than our threshold of 150 kilometers, this station is deemed insufficiently nearby to be relied upon as our primary source for temperature and dew point records. Consequently, the station records are blended with interpolated values from NASA's MERRA-2 satellite-era reanalysis , and both are corrected for elevation differences according to the International Standard Atmosphere .
The weight assigned to the MERRA-2 value depends on the distance from Miranda to the nearest station, increasing from 0% at 150 kilometers to 100% at 200 kilometers. In this case, the MERRA-2 weight is 46%, making the weight assigned to the weather station 54%.
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.