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Spring Weather in Sekadau Indonesia

Daily high temperatures are around 89°F, rarely falling below 85°F or exceeding 92°F. The highest daily average high temperature is 89°F on May 30.

Daily low temperatures are around 75°F, rarely falling below 73°F or exceeding 76°F. The highest daily average low temperature is 75°F on May 4.

For reference, on August 9, the hottest day of the year, temperatures in Sekadau typically range from 74°F to 89°F, while on July 18, the coldest day of the year, they range from 74°F to 89°F.

Average High and Low Temperature in the Spring in Sekadau

Average High and Low Temperature in the Spring in SekadauMarAprMay70°F70°F75°F75°F80°F80°F85°F85°F90°F90°F95°F95°F100°F100°FWinterSummerMay 3089°FMay 3089°F75°F75°FMar 188°FMar 188°F74°F74°FApr 188°FApr 188°F74°F74°FMay 189°FMay 189°F75°F75°F
The daily average high (red line) and low (blue line) temperature, with 25th to 75th and 10th to 90th percentile bands. The thin dotted lines are the corresponding average perceived temperatures.

The figure below shows you a compact characterization of the hourly average spring temperatures. 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 the Spring in Sekadau

Average Hourly Temperature in the Spring in SekadauMarAprMay12 AM12 AM2 AM2 AM4 AM4 AM6 AM6 AM8 AM8 AM10 AM10 AM12 PM12 PM2 PM2 PM4 PM4 PM6 PM6 PM8 PM8 PM10 PM10 PM12 AM12 AMWinterSummercomfortablecomfortablewarmwarmhot
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 average hourly temperature, color coded into bands. The shaded overlays indicate night and civil twilight.

Antioquia, Colombia (11,801 miles away) is the far-away foreign place with temperatures most similar to Sekadau (view comparison).

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The spring in Sekadau experiences decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 86% to 76%.

The clearest day of the spring is May 31, with clear, mostly clear, or partly cloudy conditions 24% of the time.

For reference, on January 24, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 90%, while on June 25, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 31%.

Cloud Cover Categories in the Spring in Sekadau

Cloud Cover Categories in the Spring in SekadauMarAprMay0%100%10%90%20%80%30%70%40%60%50%50%60%40%70%30%80%20%90%10%100%0%WinterSummerMar 114%Mar 114%May 3124%May 3124%Apr 116%Apr 116%May 119%May 119%mostly clearpartly cloudymostly cloudyovercast
0% clear 20% mostly clear 40% partly cloudy 60% mostly cloudy 80% overcast 100%
The percentage of time spent in each cloud cover band, categorized by the percentage of the sky covered by clouds.

A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Sekadau, the chance of a wet day over the course of the spring is gradually decreasing, starting the season at 51% and ending it at 47%.

For reference, the year's highest daily chance of a wet day is 72% on November 22, and its lowest chance is 34% on August 10.

Probability of Precipitation in the Spring in Sekadau

Probability of Precipitation in the Spring in SekadauMarAprMay0%0%10%10%20%20%30%30%40%40%50%50%60%60%WinterSummerApr 1460%Apr 1460%Mar 151%Mar 151%May 3147%May 3147%Apr 160%Apr 160%May 156%May 156%rain
The percentage of days in which various types of precipitation are observed, excluding trace quantities: rain alone, snow alone, and mixed (both rain and snow fell in the same day).

Rainfall

To show variation within the season and not just the monthly totals, we show the rainfall accumulated over a sliding 31-day period centered around each day.

The average sliding 31-day rainfall during the spring in Sekadau is rapidly decreasing, starting the season at 9.0 inches, when it rarely exceeds 15.0 inches or falls below 4.3 inches, and ending the season at 7.5 inches, when it rarely exceeds 12.0 inches or falls below 3.6 inches.

Average Monthly Rainfall in the Spring in Sekadau

Average Monthly Rainfall in the Spring in SekadauMarAprMay0 in0 in2 in2 in4 in4 in6 in6 in8 in8 in10 in10 in12 in12 in14 in14 in16 in16 inWinterSummerMar 19.0 inMar 19.0 inMay 317.5 inMay 317.5 inApr 19.6 inApr 19.6 inMay 19.3 inMay 19.3 in
The average rainfall (solid line) accumulated over the course of a sliding 31-day period centered on the day in question, with 25th to 75th and 10th to 90th percentile bands. The thin dotted line is the corresponding average snowfall.

Over the course of the spring in Sekadau, the length of the day is essentially constant. The shortest day of the spring is March 24, with 12 hours, 7 minutes of daylight and the longest day is May 31, with 12 hours, 7 minutes of daylight.

Hours of Daylight and Twilight in the Spring in Sekadau

Hours of Daylight and Twilight in the Spring in SekadauMarAprMay0 hr24 hr4 hr20 hr8 hr16 hr12 hr12 hr16 hr8 hr20 hr4 hr24 hr0 hrWinterSummerMar 2012 hr, 7 minMar 2012 hr, 7 minnightnightdaydayMay 3112 hr, 7 minMay 3112 hr, 7 minMay 112 hr, 7 minMay 112 hr, 7 min
The number of hours during which the Sun is visible (black line). From bottom (most yellow) to top (most gray), the color bands indicate: full daylight, twilight (civil, nautical, and astronomical), and full night.

The latest sunrise of the spring in Sekadau is 5:45 AM on March 1 and the earliest sunrise is 16 minutes earlier at 5:29 AM on May 15.

The latest sunset is 5:51 PM on March 1 and the earliest sunset is 16 minutes earlier at 5:36 PM on May 14.

Daylight saving time is not observed in Sekadau during 2024.

For reference, on June 20, the longest day of the year, the Sun rises at 5:34 AM and sets 12 hours, 7 minutes later, at 5:41 PM, while on December 21, the shortest day of the year, it rises at 5:30 AM and sets 12 hours, 7 minutes later, at 5:38 PM.

Sunrise & Sunset with Twilight in the Spring in Sekadau

Sunrise & Sunset with Twilight in the Spring in SekadauMarAprMay12 AM2 AM4 AM6 AM8 AM10 AM12 PM2 PM4 PM6 PM8 PM10 PMWinterSummer5:29 AM5:29 AMMay 155:36 PMMay 155:36 PM5:45 AM5:45 AMMar 15:51 PMMar 15:51 PM5:30 AM5:30 AMMay 315:37 PMMay 315:37 PM5:36 AM5:36 AMApr 15:43 PMApr 15:43 PMSolarMidnightSolarMidnightSolarNoonSunriseSunset
The solar day in the spring. From bottom to top, the black lines are the previous solar midnight, sunrise, solar noon, sunset, and the next solar midnight. The day, twilights (civil, nautical, and astronomical), and night are indicated by the color bands from yellow to gray.

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.

Solar Elevation and Azimuth in the Spring in Sekadau

Solar Elevation and Azimuth in the Spring in SekadauMarAprMay12 AM12 AM2 AM2 AM4 AM4 AM6 AM6 AM8 AM8 AM10 AM10 AM12 PM12 PM2 PM2 PM4 PM4 PM6 PM6 PM8 PM8 PM10 PM10 PM12 AM12 AMWinterSummer001020203030405050606070800010102030304040506060707080
northeastsouthwest
Solar elevation and azimuth in the the spring of 2024. The black lines are lines of constant solar elevation (the angle of the sun above the horizon, in degrees). The background color fills indicate the azimuth (the compass bearing) of the sun. The lightly tinted areas at the boundaries of the cardinal compass points indicate the implied intermediate directions (northeast, southeast, southwest, and northwest).

The figure below presents a compact representation of key lunar data for the spring of 2024. 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. The label associated with each bar indicates the date and time that the phase is obtained, and the companion time labels indicate the rise and set times of the Moon for the nearest time interval in which the moon is above the horizon.

Moon Rise, Set & Phases in the Spring in Sekadau

Moon Rise, Set & Phases in the Spring in SekadauMarAprMay12 AM12 AM4 AM4 AM8 AM8 AM12 PM12 PM4 PM4 PM8 PM8 PM12 AM12 AMWinterSummerFeb 106:00 AMFeb 106:00 AMFeb 247:31 PMFeb 247:31 PMMar 104:01 PMMar 104:01 PMMar 252:01 PMMar 252:01 PMApr 91:22 AMApr 91:22 AMApr 246:50 AMApr 246:50 AMMay 810:23 AMMay 810:23 AMMay 238:54 PMMay 238:54 PMJun 67:38 PMJun 67:38 PMJun 228:09 AMJun 228:09 AM5:56 AM5:56 AM6:24 PM6:24 PM5:51 PM5:51 PM6:12 AM6:12 AM5:27 AM5:27 AM5:54 PM5:54 PM5:49 PM5:49 PM6:09 AM6:09 AM5:46 AM5:46 AM6:12 PM6:12 PM5:08 PM5:08 PM5:29 AM5:29 AM5:18 AM5:18 AM5:46 PM5:46 PM5:22 PM5:22 PM5:48 AM5:48 AM4:58 AM4:58 AM5:02 PM5:02 PM5:32 AM5:32 AM
The time in which the moon is above the horizon (light blue area), with new moons (dark gray lines) and full moons (blue lines) indicated. The shaded overlays indicate night and civil twilight.

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 Sekadau is essentially constant during the spring, remaining around 100% throughout.

Humidity Comfort Levels in the Spring in Sekadau

Humidity Comfort Levels in the Spring in SekadauMarAprMay0%0%10%10%20%20%30%30%40%40%50%50%60%60%70%70%80%80%90%90%100%100%WinterSummerApr 16100%Apr 16100%Mar 1100%Mar 1100%May 31100%May 31100%Apr 1100%Apr 1100%May 1100%May 1100%miserablemiserableoppressiveoppressive
dry 55°F comfortable 60°F humid 65°F muggy 70°F oppressive 75°F miserable
The percentage of time spent at various humidity comfort levels, categorized by dew point.

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 Sekadau is essentially constant during the spring, remaining around 1.3 miles per hour throughout.

For reference, on August 7, the windiest day of the year, the daily average wind speed is 1.5 miles per hour, while on April 26, the calmest day of the year, the daily average wind speed is 1.3 miles per hour.

The lowest daily average wind speed during the spring is 1.3 miles per hour on April 26.

Average Wind Speed in the Spring in Sekadau

Average Wind Speed in the Spring in SekadauMarAprMay0.0 mph0.0 mph0.5 mph0.5 mph1.0 mph1.0 mph1.5 mph1.5 mph2.0 mph2.0 mphWinterSummerApr 261.3 mphApr 261.3 mphMar 11.3 mphMar 11.3 mphMay 311.3 mphMay 311.3 mphApr 11.3 mphApr 11.3 mph
The average of mean hourly wind speeds (dark gray line), with 25th to 75th and 10th to 90th percentile bands.

The wind direction in Sekadau during the spring is predominantly out of the north from March 1 to March 3, the west from March 3 to May 4, and the south from May 4 to May 31.

Wind Direction in the Spring in Sekadau

Wind Direction in the Spring in SekadauNWSMarAprMay0%100%20%80%40%60%60%40%80%20%100%0%WinterSummerwestsoutheastnorth
northeastsouthwest
The percentage of hours in which the mean wind direction is from each of the four cardinal wind directions, excluding hours in which the mean wind speed is less than 1.0 mph. The lightly tinted areas at the boundaries are the percentage of hours spent in the implied intermediate directions (northeast, southeast, southwest, and northwest).

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 Sekadau 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 the Spring in Sekadau

Time Spent in Various Temperature Bands and the Growing Season in the Spring in SekadauMarAprMay0%100%10%90%20%80%30%70%40%60%50%50%60%40%70%30%80%20%90%10%100%0%WinterSummer100%Apr 16100%Apr 16comfortablewarmhot
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 percentage of time spent in various temperature bands. The black line is the percentage chance that a given day is within the growing season.

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 Sekadau are very rapidly increasing during the spring, increasing by 2,727°F, from 1,751°F to 4,478°F, over the course of the season.

Growing Degree Days in the Spring in Sekadau

Growing Degree Days in the Spring in SekadauMarAprMay2,000°F2,000°F2,500°F2,500°F3,000°F3,000°F3,500°F3,500°F4,000°F4,000°F4,500°F4,500°FWinterSummerMar 11,751°FMar 11,751°FMay 314,478°FMay 314,478°FApr 12,666°FApr 12,666°FMay 13,568°FMay 13,568°F
The average growing degree days accumulated over the course of the spring, with 25th to 75th and 10th to 90th percentile bands.

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 Sekadau is essentially constant during the spring, remaining within 0.2 kWh of 4.5 kWh throughout.

The lowest average daily incident shortwave solar energy during the spring is 4.4 kWh on May 24.

Average Daily Incident Shortwave Solar Energy in the Spring in Sekadau

Average Daily Incident Shortwave Solar Energy in the Spring in SekadauMarAprMay0 kWh0 kWh1 kWh1 kWh2 kWh2 kWh3 kWh3 kWh4 kWh4 kWh5 kWh5 kWh6 kWh6 kWhWinterSummerMay 244.4 kWhMay 244.4 kWhMar 14.7 kWhMar 14.7 kWhApr 14.6 kWhApr 14.6 kWhMay 14.5 kWhMay 14.5 kWh
The average daily shortwave solar energy reaching the ground per square meter (orange line), with 25th to 75th and 10th to 90th percentile bands.

For the purposes of this report, the geographical coordinates of Sekadau are 0.017 deg latitude, 110.900 deg longitude, and 62 ft elevation.

The topography within 2 miles of Sekadau contains only modest variations in elevation, with a maximum elevation change of 164 feet and an average elevation above sea level of 81 feet. Within 10 miles contains only modest variations in elevation (846 feet). Within 50 miles contains very significant variations in elevation (5,640 feet).

The area within 2 miles of Sekadau is covered by trees (51%), cropland (21%), and water (17%), within 10 miles by trees (55%) and cropland (31%), and within 50 miles by trees (59%) and cropland (29%).

This report illustrates the typical weather in Sekadau, 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 Sekadau.

For each station, the records are corrected for the elevation difference between that station and Sekadau 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 Sekadau is computed as the weighted average of the individual contributions from each station, with weights proportional to the inverse of the distance between Sekadau 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 Sekadau 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.

Other 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.

Disclaimer

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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