Climate and Average Weather Year Round in Bandar Labuan Malaysia
The climate in Bandar Labuan is hot, oppressive, and overcast. Over the course of the year, the temperature typically varies from 77°F to 89°F and is rarely below 74°F or above 92°F.
Based on the beach/pool score, the best time of year to visit Bandar Labuan for hot-weather activities is from late January to late March.
Average Temperature in Bandar Labuan
The temperature in Bandar Labuan varies so little throughout the year that it is not entirely meaningful to discuss hot and cold seasons.
The figure below shows you a compact characterization of the entire year of hourly average temperatures. The horizontal axis is the day of the year, the vertical axis is the hour of the day, and the color is the average temperature for that hour and day.
Barranquilla, Colombia (11,130 miles away) is the far-away foreign place with temperatures most similar to Bandar Labuan (view comparison).
In Bandar Labuan, the average percentage of the sky covered by clouds experiences mild seasonal variation over the course of the year.
The clearer part of the year in Bandar Labuan begins around January 10 and lasts for 3.1 months, ending around April 13.
The clearest month of the year in Bandar Labuan is March, during which on average the sky is clear, mostly clear, or partly cloudy 24% of the time.
The cloudier part of the year begins around April 13 and lasts for 8.9 months, ending around January 10.
The cloudiest month of the year in Bandar Labuan is November, during which on average the sky is overcast or mostly cloudy 90% of the time.
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. The chance of wet days in Bandar Labuan varies significantly throughout the year.
The wetter season lasts 9.0 months, from April 13 to January 12, with a greater than 50% chance of a given day being a wet day. The month with the most wet days in Bandar Labuan is November, with an average of 21.6 days with at least 0.04 inches of precipitation.
The drier season lasts 3.0 months, from January 12 to April 13. The month with the fewest wet days in Bandar Labuan is March, with an average of 10.0 days with at least 0.04 inches of precipitation.
Among wet days, we distinguish between those that experience rain alone, snow alone, or a mixture of the two. The month with the most days of rain alone in Bandar Labuan is November, with an average of 21.6 days. Based on this categorization, the most common form of precipitation throughout the year is rain alone, with a peak probability of 74% on November 20.
To show variation within the months and not just the monthly totals, we show the rainfall accumulated over a sliding 31-day period centered around each day of the year. Bandar Labuan experiences extreme seasonal variation in monthly rainfall.
Rain falls throughout the year in Bandar Labuan. The month with the most rain in Bandar Labuan is November, with an average rainfall of 9.9 inches.
The month with the least rain in Bandar Labuan is March, with an average rainfall of 3.3 inches.
The length of the day in Bandar Labuan does not vary substantially over the course of the year, staying within 25 minutes of 12 hours throughout. In 2023, the shortest day is December 22, with 11 hours, 49 minutes of daylight; the longest day is June 21, with 12 hours, 26 minutes of daylight.
The earliest sunrise is at 6:04 AM on May 24, and the latest sunrise is 31 minutes later at 6:35 AM on February 3. The earliest sunset is at 5:59 PM on November 11, and the latest sunset is 37 minutes later at 6:36 PM on July 18.
Daylight saving time (DST) is not observed in Bandar Labuan during 2023.
The figure below presents a compact representation of the sun's elevation (the angle of the sun above the horizon) and azimuth (its compass bearing) for every hour of every day in the reporting period. The horizontal axis is the day of the year and the vertical axis is the hour of the day. For a given day and hour of that day, the background color indicates the azimuth of the sun at that moment. The black isolines are contours of constant solar elevation.
The figure below presents a compact representation of key lunar data for 2023. The horizontal axis is the day, the vertical axis is the hour of the day, and the colored areas indicate when the moon is above the horizon. The vertical gray bars (new Moons) and blue bars (full Moons) indicate key Moon phases.
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 perceived humidity level in Bandar Labuan, as measured by the percentage of time in which the humidity comfort level is muggy, oppressive, or miserable, does not vary significantly over the course of the year, remaining a virtually constant 100% throughout.
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 Bandar Labuan experiences significant seasonal variation over the course of the year.
The windier part of the year lasts for 3.1 months, from December 12 to March 16, with average wind speeds of more than 6.3 miles per hour. The windiest month of the year in Bandar Labuan is January, with an average hourly wind speed of 7.7 miles per hour.
The calmer time of year lasts for 8.9 months, from March 16 to December 12. The calmest month of the year in Bandar Labuan is May, with an average hourly wind speed of 4.8 miles per hour.
The predominant average hourly wind direction in Bandar Labuan varies throughout the year.
The wind is most often from the west for 6.4 months, from May 3 to November 14, with a peak percentage of 52% on September 24. The wind is most often from the north for 5.6 months, from November 14 to May 3, with a peak percentage of 64% on January 1.
Bandar Labuan 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 water temperature experiences some seasonal variation over the course of the year.
The time of year with warmer water lasts for 5.0 months, from April 24 to September 26, with an average temperature above 85°F. The month of the year in Bandar Labuan with the warmest water is June, with an average temperature of 86°F.
The time of year with cooler water lasts for 2.0 months, from January 14 to March 12, with an average temperature below 82°F. The month of the year in Bandar Labuan with the coolest water is February, with an average temperature of 81°F.
Best Time of Year to Visit
To characterize how pleasant the weather is in Bandar Labuan throughout the year, we compute two travel scores.
The tourism score favors clear, rainless days with perceived temperatures between 65°F and 80°F. Based on this score, the best time of year to visit Bandar Labuan for general outdoor tourist activities is from late January to mid March, with a peak score in the third week of February.
Tourism Score in Bandar Labuan
The beach/pool score favors clear, rainless days with perceived temperatures between 75°F and 90°F. Based on this score, the best time of year to visit Bandar Labuan for hot-weather activities is from late January to late March, with a peak score in the first week of March.
Beach/Pool Score in Bandar Labuan
For each hour between 8:00 AM and 9:00 PM of each day in the analysis period (1980 to 2016), independent scores are computed for perceived temperature, cloud cover, and total precipitation. Those scores are combined into a single hourly composite score, which is then aggregated into days, averaged over all the years in the analysis period, and smoothed.
Our cloud cover score is 10 for fully clear skies, falling linearly to 9 for mostly clear skies, and to 1 for fully overcast skies.
Our precipitation score, which is based on the three-hour precipitation centered on the hour in question, is 10 for no precipitation, falling linearly to 9 for trace precipitation, and to 0 for 0.04 inches of precipitation or more.
Our tourism temperature score is 0 for perceived temperatures below 50°F, rising linearly to 9 for 65°F, to 10 for 75°F, falling linearly to 9 for 80°F, and to 1 for 90°F or hotter.
Our beach/pool temperature score is 0 for perceived temperatures below 65°F, rising linearly to 9 for 75°F, to 10 for 82°F, falling linearly to 9 for 90°F, and to 1 for 100°F or hotter.
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 Bandar Labuan 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.
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.
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 experiences some seasonal variation over the course of the year.
The brighter period of the year lasts for 1.6 months, from February 15 to April 1, with an average daily incident shortwave energy per square meter above 5.7 kWh. The brightest month of the year in Bandar Labuan is March, with an average of 5.9 kWh.
The darker period of the year lasts for 2.5 months, from October 2 to December 20, with an average daily incident shortwave energy per square meter below 4.6 kWh. The darkest month of the year in Bandar Labuan is November, with an average of 4.3 kWh.
For the purposes of this report, the geographical coordinates of Bandar Labuan are 5.289 deg latitude, 115.269 deg longitude, and 39 ft elevation.
The topography within 2 miles of Bandar Labuan contains only modest variations in elevation, with a maximum elevation change of 118 feet and an average elevation above sea level of 16 feet. Within 10 miles also contains only modest variations in elevation (390 feet). Within 50 miles contains only modest variations in elevation (6,460 feet).
The area within 2 miles of Bandar Labuan is covered by water (67%), cropland (17%), and artificial surfaces (11%), within 10 miles by water (84%), and within 50 miles by water (64%) and trees (22%).
This report illustrates the typical weather in Bandar Labuan, 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 Bandar Labuan.
For each station, the records are corrected for the elevation difference between that station and Bandar Labuan 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 Bandar Labuan is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Bandar Labuan and a given station.
The stations contributing to this reconstruction are:
To get a sense of how much these sources agree with each other, you can view a comparison of Bandar Labuan and the stations that contribute to our estimates of its temperature history and climate. Please note that each source's contribution is adjusted for elevation and the relative change present in the MERRA-2 data.
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 airports and weather stations are provided by AskGeo.com .
Maps are © OpenStreetMap contributors.
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.
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