Average Weather in August in New Delhi India
In New Delhi, the month of August is characterized by essentially constant daily high temperatures, with daily highs around 92°F throughout the month, rarely exceeding 98°F or dropping below 86°F.
Daily low temperatures are around 80°F, rarely falling below 77°F or exceeding 84°F.
For reference, on May 27, the hottest day of the year, temperatures in New Delhi typically range from 81°F to 103°F, while on January 7, the coldest day of the year, they range from 46°F to 67°F.
Average High and Low Temperature in August
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on August. 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 August
The month of August in New Delhi experiences very rapidly decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 59% to 35%.
The clearest day of the month is August 31, with clear, mostly clear, or partly cloudy conditions 65% of the time.
For reference, on July 31, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 59%, while on October 14, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 96%.
Cloud Cover Categories in August
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In New Delhi, the chance of a wet day over the course of August is very rapidly decreasing, starting the month at 54% and ending it at 42%.
For reference, the year's highest daily chance of a wet day is 55% on July 22, and its lowest chance is 2% on November 26.
Probability of Precipitation in August
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 August in New Delhi is decreasing, starting the month at 6.9 inches, when it rarely exceeds 12.0 inches or falls below 2.6 inches, and ending the month at 5.9 inches, when it rarely exceeds 11.9 inches or falls below 2.1 inches.
The highest average 31-day accumulation is 6.9 inches on August 4.
Average Monthly Rainfall in August
Over the course of August in New Delhi, the length of the day is decreasing. From the start to the end of the month, the length of the day decreases by 44 minutes, implying an average daily decrease of 1 minute, 29 seconds, and weekly decrease of 10 minutes, 20 seconds.
The shortest day of the month is August 31, with 12 hours, 45 minutes of daylight and the longest day is August 1, with 13 hours, 30 minutes of daylight.
Hours of Daylight and Twilight in August
The earliest sunrise of the month in New Delhi is 5:42 AM on August 1 and the latest sunrise is 16 minutes later at 5:58 AM on August 31.
The latest sunset is 7:12 PM on August 1 and the earliest sunset is 28 minutes earlier at 6:43 PM on August 31.
Daylight saving time is not observed in New Delhi during 2017.
For reference, on June 21, the longest day of the year, the Sun rises at 5:23 AM and sets 13 hours, 58 minutes later, at 7:22 PM, while on December 21, the shortest day of the year, it rises at 7:09 AM and sets 10 hours, 19 minutes later, at 5:28 PM.
Sunrise & Sunset with Twilight in August
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 New Delhi is essentially constant during August, remaining within 1% of 99% throughout.
The highest chance of a muggy day during August is 99% on August 17.
For reference, on August 16, the muggiest day of the year, there are muggy conditions 99% of the time, while on January 28, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in August
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 New Delhi is gradually decreasing during August, decreasing from 6.6 miles per hour to 5.9 miles per hour over the course of the month.
For reference, on May 30, the windiest day of the year, the daily average wind speed is 8.4 miles per hour, while on October 16, the calmest day of the year, the daily average wind speed is 5.1 miles per hour.
Average Wind Speed in August
Wind Direction in August
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 New Delhi 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 August
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 New Delhi is very rapidly increasing during August, increasing by 1,019°F, from 5,389°F to 6,408°F, over the course of the month.
Growing Degree Days in August
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 New Delhi is essentially constant during August, remaining within 0.1 kWh of 5.7 kWh throughout.
The lowest average daily incident shortwave solar energy during August is 5.6 kWh on August 11.
Average Daily Incident Shortwave Solar Energy in August
For the purposes of this report, the geographical coordinates of New Delhi are 28.636 deg latitude, 77.224 deg longitude, and 712 ft elevation.
The topography within 2 miles of New Delhi contains only modest variations in elevation, with a maximum elevation change of 177 feet and an average elevation above sea level of 721 feet. Within 10 miles also contains only modest variations in elevation (328 feet). Within 50 miles contains only modest variations in elevation (797 feet).
The area within 2 miles of New Delhi is covered by artificial surfaces (99%), within 10 miles by artificial surfaces (79%) and cropland (14%), and within 50 miles by cropland (91%).
This report illustrates the typical weather in New Delhi 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, Safdarjung Airport, in our network suitable to be used as a proxy for the historical temperature and dew point records of New Delhi.
At a distance of 6 kilometers from New Delhi, 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 New Delhi 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.