Average Weather in March in Kendal Indonesia
Daily high temperatures are around 87°F, rarely falling below 84°F or exceeding 90°F.
Daily low temperatures are around 78°F, rarely falling below 75°F or exceeding 80°F.
For reference, on October 4, the hottest day of the year, temperatures in Kendal typically range from 78°F to 90°F, while on August 6, the coldest day of the year, they range from 76°F to 89°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 Kendal experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 85% throughout the month.
The clearest day of the month is March 31, with clear, mostly clear, or partly cloudy conditions 17% of the time.
For reference, on December 1, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 91%, while on August 6, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 43%.
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 Kendal, the chance of a wet day over the course of March is very rapidly decreasing, starting the month at 64% and ending it at 51%.
For reference, the year's highest daily chance of a wet day is 75% on February 1, and its lowest chance is 11% on August 11.
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 Kendal is very rapidly decreasing, starting the month at 9.3 inches, when it rarely exceeds 14.2 inches or falls below 5.2 inches, and ending the month at 6.2 inches, when it rarely exceeds 10.1 inches or falls below 2.6 inches.
Average Monthly Rainfall in March
Over the course of March in Kendal, the length of the day is essentially constant. The shortest day of the month is March 31, with 12 hours, 3 minutes of daylight and the longest day is March 1, with 12 hours, 14 minutes of daylight.
Hours of Daylight and Twilight in March
The latest sunrise of the month in Kendal is 5:44 AM on March 1 and the earliest sunrise is 2 minutes, 20 seconds earlier at 5:42 AM on March 31.
The latest sunset is 5:58 PM on March 1 and the earliest sunset is 14 minutes earlier at 5:44 PM on March 31.
Daylight saving time is not observed in Kendal during 2019.
For reference, on December 22, the longest day of the year, the Sun rises at 5:21 AM and sets 12 hours, 32 minutes later, at 5:53 PM, while on June 21, the shortest day of the year, it rises at 5:49 AM and sets 11 hours, 43 minutes later, at 5:32 PM.
Sunrise & Sunset with Twilight 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 Kendal is essentially constant during March, remaining around 100% throughout.
For reference, on January 1, the muggiest day of the year, there are muggy conditions 100% of the time, while on August 13, the least muggy day of the year, there are muggy conditions 93% 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 Kendal is decreasing during March, decreasing from 7.0 miles per hour to 5.0 miles per hour over the course of the month.
For reference, on January 28, the windiest day of the year, the daily average wind speed is 8.5 miles per hour, while on November 10, the calmest day of the year, the daily average wind speed is 4.9 miles per hour.
Average Wind Speed in March
The wind direction in Kendal during March is predominantly out of the west from March 1 to March 28 and the east from March 28 to March 31.
Wind Direction in March
Kendal 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 Kendal is essentially constant during March, remaining within 1°F of 84°F throughout.
Average Water Temperature 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 Kendal 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
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 Kendal are very rapidly increasing during March, increasing by 936°F, from 7,675°F to 8,611°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 Kendal is essentially constant during March, remaining within 0.1 kWh of 4.6 kWh throughout.
Average Daily Incident Shortwave Solar Energy in March
For the purposes of this report, the geographical coordinates of Kendal are -6.921 deg latitude, 110.202 deg longitude, and 20 ft elevation.
The topography within 2 miles of Kendal is essentially flat, with a maximum elevation change of 49 feet and an average elevation above sea level of 17 feet. Within 10 miles is essentially flat (1,161 feet). Within 50 miles contains very significant variations in elevation (10,879 feet).
The area within 2 miles of Kendal is covered by cropland (76%) and trees (11%), within 10 miles by water (53%) and cropland (26%), and within 50 miles by water (46%) and trees (25%).
This report illustrates the typical weather in Kendal 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 2 weather stations near enough to contribute to our estimation of the temperature and dew point in Kendal.
For each station, the records are corrected for the elevation difference between that station and Kendal 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 Kendal is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Kendal and a given station.
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 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.