Average Weather in April in Waimanalo Hawaii, United States
Daily high temperatures are around 79°F, rarely falling below 76°F or exceeding 82°F.
Daily low temperatures are around 71°F, rarely falling below 67°F or exceeding 74°F.
For reference, on August 30, the hottest day of the year, temperatures in Waimanalo typically range from 76°F to 84°F, while on January 28, the coldest day of the year, they range from 69°F to 78°F.
Average High and Low Temperature in April
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on April. 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 April
The month of April in Waimanalo experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 32% throughout the month. The highest chance of overcast or mostly cloudy conditions is 34% on April 25.
The clearest day of the month is April 12, with clear, mostly clear, or partly cloudy conditions 71% of the time.
For reference, on October 31, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 41%, while on January 18, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 79%.
Cloud Cover Categories in April
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Waimanalo, the chance of a wet day over the course of April is essentially constant, remaining around 14% throughout.
For reference, the year's highest daily chance of a wet day is 25% on January 11, and its lowest chance is 6% on June 20.
Probability of Precipitation in April
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 April in Waimanalo is gradually decreasing, starting the month at 1.6 inches, when it rarely exceeds 3.7 inches, and ending the month at 1.2 inches, when it rarely exceeds 3.4 inches.
Average Monthly Rainfall in April
Over the course of April in Waimanalo, the length of the day is increasing. From the start to the end of the month, the length of the day increases by 33 minutes, implying an average daily increase of 1 minute, 9 seconds, and weekly increase of 8 minutes, 2 seconds.
The shortest day of the month is April 1, with 12 hours, 22 minutes of daylight and the longest day is April 30, with 12 hours, 55 minutes of daylight.
Hours of Daylight and Twilight in April
The latest sunrise of the month in Waimanalo is 6:23 AM on April 1 and the earliest sunrise is 23 minutes earlier at 6:00 AM on April 30.
The earliest sunset is 6:45 PM on April 1 and the latest sunset is 10 minutes later at 6:55 PM on April 30.
Daylight saving time is not observed in Waimanalo during 2018.
For reference, on June 21, the longest day of the year, the Sun rises at 5:49 AM and sets 13 hours, 26 minutes later, at 7:15 PM, while on December 21, the shortest day of the year, it rises at 7:04 AM and sets 10 hours, 50 minutes later, at 5:54 PM.
Sunrise & Sunset with Twilight in April
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 Waimanalo is increasing during April, rising from 40% to 48% over the course of the month.
For reference, on September 21, the muggiest day of the year, there are muggy conditions 98% of the time, while on March 8, the least muggy day of the year, there are muggy conditions 34% of the time.
Humidity Comfort Levels in April
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 Waimanalo is essentially constant during April, remaining within 0.3 miles per hour of 15.3 miles per hour throughout.
For reference, on July 3, the windiest day of the year, the daily average wind speed is 16.7 miles per hour, while on January 10, the calmest day of the year, the daily average wind speed is 12.4 miles per hour.
The highest daily average wind speed during April is 15.6 miles per hour on April 8.
Average Wind Speed in April
Wind Direction in April
Waimanalo 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 Waimanalo is essentially constant during April, remaining around 76°F throughout.
Average Water Temperature in April
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 Waimanalo 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 April
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 Waimanalo are rapidly increasing during April, increasing by 707°F, from 2,052°F to 2,759°F, over the course of the month.
Growing Degree Days in April
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 Waimanalo is gradually increasing during April, rising by 0.6 kWh, from 6.7 kWh to 7.2 kWh, over the course of the month.
Average Daily Incident Shortwave Solar Energy in April
For the purposes of this report, the geographical coordinates of Waimanalo are 21.346 deg latitude, -157.724 deg longitude, and 164 ft elevation.
The topography within 2 miles of Waimanalo contains large variations in elevation, with a maximum elevation change of 2,454 feet and an average elevation above sea level of 288 feet. Within 10 miles also contains large variations in elevation (3,117 feet). Within 50 miles contains large variations in elevation (4,121 feet).
The area within 2 miles of Waimanalo is covered by artificial surfaces (44%), trees (23%), water (14%), and shrubs (13%), within 10 miles by water (61%) and artificial surfaces (17%), and within 50 miles by water (91%).
This report illustrates the typical weather in Waimanalo 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 Waimanalo.
For each station, the records are corrected for the elevation difference between that station and Waimanalo 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 Waimanalo is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Waimanalo and a given station.
The stations contributing to this reconstruction are: Marine Corps Air Station Kaneohe Bay (65%, 12 kilometers, north); Honolulu International Airport (30%, 21 kilometers, west); and Molokai Airport (5%, 69 kilometers, east).
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.