Average Weather in May in Beverley Australia
Daily low temperatures decrease by 5°F, from 48°F to 42°F, rarely falling below 34°F or exceeding 56°F.
For reference, on January 19, the hottest day of the year, temperatures in Beverley typically range from 61°F to 94°F, while on July 14, the coldest day of the year, they range from 39°F to 61°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
The month of May in Beverley experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 30% throughout the month.
The clearest day of the month is May 27, with clear, mostly clear, or partly cloudy conditions 71% of the time.
For reference, on April 20, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 31%, while on January 19, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 85%.
Cloud Cover Categories in May
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Beverley, the chance of a wet day over the course of May is very rapidly increasing, starting the month at 14% and ending it at 26%.
For reference, the year's highest daily chance of a wet day is 33% on July 23, and its lowest chance is 5% on December 30.
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 Beverley is rapidly increasing, starting the month at 1.2 inches, when it rarely exceeds 2.6 inches or falls below 0.3 inches, and ending the month at 2.3 inches, when it rarely exceeds 4.0 inches or falls below 0.9 inches.
Average Monthly Rainfall in May
Over the course of May in Beverley, the length of the day is decreasing. From the start to the end of the month, the length of the day decreases by 39 minutes, implying an average daily decrease of 1 minute, 17 seconds, and weekly decrease of 9 minutes, 0 seconds.
The shortest day of the month is May 31, with 10 hours, 12 minutes of daylight and the longest day is May 1, with 10 hours, 51 minutes of daylight.
Hours of Daylight and Twilight in May
The earliest sunrise of the month in Beverley is 6:43 AM on May 1 and the latest sunrise is 20 minutes later at 7:03 AM on May 31.
The latest sunset is 5:34 PM on May 1 and the earliest sunset is 19 minutes earlier at 5:15 PM on May 31.
Daylight saving time is not observed in Beverley during 2018.
For reference, on December 21, the longest day of the year, the Sun rises at 5:02 AM and sets 14 hours, 15 minutes later, at 7:17 PM, while on June 21, the shortest day of the year, it rises at 7:12 AM and sets 10 hours, 3 minutes later, at 5:15 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 Beverley is essentially constant during May, remaining around 0% throughout.
For reference, on February 14, the muggiest day of the year, there are muggy conditions 2% of the time, while on June 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 Beverley is essentially constant during May, remaining within 0.1 miles per hour of 9.4 miles per hour throughout.
For reference, on January 23, the windiest day of the year, the daily average wind speed is 12.6 miles per hour, while on May 18, the calmest day of the year, the daily average wind speed is 9.3 miles per hour.
The lowest daily average wind speed during May is 9.3 miles per hour on May 19.
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).
The growing season in Beverley typically lasts for 8.7 months (264 days), from around September 12 to around June 3, rarely starting before August 9 or after October 16, and rarely ending before April 27 or after July 4.
The month of May in Beverley is more likely than not fully within the growing season, with the chance that a given day is in the growing season rapidly decreasing from 88% to 55% over the course of the month.
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 Beverley are increasing during May, increasing by 212°F, from 4,396°F to 4,608°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 Beverley is gradually decreasing during May, falling by 1.0 kWh, from 4.0 kWh to 3.0 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 Beverley are -32.108 deg latitude, 116.927 deg longitude, and 751 ft elevation.
The topography within 2 miles of Beverley contains only modest variations in elevation, with a maximum elevation change of 358 feet and an average elevation above sea level of 716 feet. Within 10 miles contains only modest variations in elevation (623 feet). Within 50 miles contains significant variations in elevation (1,706 feet).
The area within 2 miles of Beverley is covered by cropland (75%) and sparse vegetation (19%), within 10 miles by cropland (87%) and sparse vegetation (11%), and within 50 miles by cropland (65%) and sparse vegetation (17%).
This report illustrates the typical weather in Beverley 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, Perth Airport, in our network suitable to be used as a proxy for the historical temperature and dew point records of Beverley.
At a distance of 93 kilometers from Beverley, 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 Beverley 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.