Average Weather in May in Auckland New Zealand
Daily low temperatures decrease by 4°F, from 54°F to 51°F, rarely falling below 43°F or exceeding 61°F.
For reference, on February 6, the hottest day of the year, temperatures in Auckland typically range from 63°F to 74°F, while on July 15, the coldest day of the year, they range from 47°F to 57°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 Auckland experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 41% throughout the month.
The clearest day of the month is May 1, with clear, mostly clear, or partly cloudy conditions 61% of the time.
For reference, on June 3, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 44%, while on March 18, 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 Auckland, the chance of a wet day over the course of May is rapidly increasing, starting the month at 25% and ending it at 33%.
For reference, the year's highest daily chance of a wet day is 37% on July 18, and its lowest chance is 17% on January 28.
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 Auckland is essentially constant, remaining about 3.2 inches throughout, and rarely exceeding 5.8 inches or falling below 1.0 inches.
Average Monthly Rainfall in May
Over the course of May in Auckland, the length of the day is decreasing. From the start to the end of the month, the length of the day decreases by 47 minutes, implying an average daily decrease of 1 minute, 33 seconds, and weekly decrease of 10 minutes, 54 seconds.
The shortest day of the month is May 31, with 9 hours, 49 minutes of daylight and the longest day is May 1, with 10 hours, 36 minutes of daylight.
Hours of Daylight and Twilight in May
The earliest sunrise of the month in Auckland is 6:59 AM on May 1 and the latest sunrise is 24 minutes later at 7:23 AM on May 31.
The latest sunset is 5:35 PM on May 1 and the earliest sunset is 23 minutes earlier at 5:13 PM on May 31.
Daylight saving time is observed in Auckland during 2018, but it neither starts nor ends during May, so the entire month is in standard time.
For reference, on December 21, the longest day of the year, the Sun rises at 5:57 AM and sets 14 hours, 42 minutes later, at 8:39 PM, while on June 21, the shortest day of the year, it rises at 7:33 AM and sets 9 hours, 38 minutes later, at 5:11 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 Auckland is essentially constant during May, remaining within 1% of 1% throughout.
For reference, on February 2, the muggiest day of the year, there are muggy conditions 14% of the time, while on June 27, 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 Auckland is increasing during May, increasing from 13.2 miles per hour to 14.7 miles per hour over the course of the month.
For reference, on October 3, the windiest day of the year, the daily average wind speed is 15.7 miles per hour, while on February 8, the calmest day of the year, the daily average wind speed is 12.3 miles per hour.
Average Wind Speed in May
Wind Direction in May
Auckland 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 Auckland is gradually decreasing during May, falling by 3°F, from 65°F to 62°F, over the course of the month.
Average Water Temperature 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 Auckland 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 Auckland are increasing during May, increasing by 221°F, from 3,188°F to 3,409°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 Auckland is gradually decreasing during May, falling by 0.9 kWh, from 3.1 kWh to 2.2 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 Auckland are -36.867 deg latitude, 174.767 deg longitude, and 141 ft elevation.
The topography within 2 miles of Auckland contains significant variations in elevation, with a maximum elevation change of 607 feet and an average elevation above sea level of 182 feet. Within 10 miles contains significant variations in elevation (860 feet). Within 50 miles contains very significant variations in elevation (2,989 feet).
The area within 2 miles of Auckland is covered by artificial surfaces (82%), within 10 miles by water (36%) and grassland (26%), and within 50 miles by water (66%) and trees (17%).
This report illustrates the typical weather in Auckland 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, Auckland International Airport, in our network suitable to be used as a proxy for the historical temperature and dew point records of Auckland.
At a distance of 16 kilometers from Auckland, 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 Auckland 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.