November Weather in Ahonglukumu ChinaDaily high temperatures decrease by 19°F, from 60°F to 42°F, rarely falling below 33°F or exceeding 68°F. Daily low temperatures decrease by 12°F, from 35°F to 23°F, rarely falling below 17°F or exceeding 43°F. For reference, on July 23, the hottest day of the year, temperatures in Ahonglukumu typically range from 71°F to 91°F, while on January 13, the coldest day of the year, they range from 13°F to 31°F. The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on November. 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. Moab, Utah, United States (7,054 miles away) and Marysville, Kansas, United States (6,970 miles) are the far-away foreign places with temperatures most similar to Ahonglukumu (view comparison). CloudsThe month of November in Ahonglukumu experiences gradually increasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy increasing from 36% to 43%. The clearest day of the month is November 1, with clear, mostly clear, or partly cloudy conditions 64% of the time. For reference, on March 23, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 62%, while on August 9, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 90%. PrecipitationA wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Ahonglukumu, the chance of a wet day over the course of November is essentially constant, remaining around 1% throughout. For reference, the year's highest daily chance of a wet day is 7% on July 25, and its lowest chance is 0% on December 20. SunOver the course of November in Ahonglukumu, the length of the day is decreasing. From the start to the end of the month, the length of the day decreases by 53 minutes, implying an average daily decrease of 1 minute, 49 seconds, and weekly decrease of 12 minutes, 44 seconds. The shortest day of the month is November 30, with 9 hours, 38 minutes of daylight and the longest day is November 1, with 10 hours, 31 minutes of daylight. The earliest sunrise of the month in Ahonglukumu is 9:18 AM on November 1 and the latest sunrise is 32 minutes later at 9:50 AM on November 30. The latest sunset is 7:49 PM on November 1 and the earliest sunset is 21 minutes earlier at 7:28 PM on November 30. Daylight saving time is not observed in Ahonglukumu during 2024. For reference, on June 20, the longest day of the year, the Sun rises at 7:24 AM and sets 14 hours, 56 minutes later, at 10:20 PM, while on December 21, the shortest day of the year, it rises at 10:06 AM and sets 9 hours, 25 minutes later, at 7:31 PM. 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. MoonThe figure below presents a compact representation of key lunar data for November 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.
HumidityWe 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 Ahonglukumu is essentially constant during November, remaining around 0% throughout. For reference, on July 26, the muggiest day of the year, there are muggy conditions 2% of the time, while on January 1, the least muggy day of the year, there are muggy conditions 0% of the time. WindThis 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 Ahonglukumu is gradually decreasing during November, decreasing from 5.0 miles per hour to 4.5 miles per hour over the course of the month. For reference, on May 3, the windiest day of the year, the daily average wind speed is 7.6 miles per hour, while on December 23, the calmest day of the year, the daily average wind speed is 4.2 miles per hour. The hourly average wind direction in Ahonglukumu throughout November is predominantly from the east, with a peak proportion of 60% on November 28. Growing SeasonDefinitions 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). The growing season in Ahonglukumu typically lasts for 7.6 months (234 days), from around March 13 to around November 2, rarely starting before February 26 or after March 29, and rarely ending before October 13 or after November 22. During November in Ahonglukumu, the chance that a given day is within the growing season is rapidly decreasing falling from 52% to 2% over the course of the month. 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 Ahonglukumu are gradually increasing during November, increasing by 40°F, from 4,777°F to 4,817°F, over the course of the month. Solar EnergyThis 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 Ahonglukumu is gradually decreasing during November, falling by 0.9 kWh, from 3.6 kWh to 2.6 kWh, over the course of the month. TopographyFor the purposes of this report, the geographical coordinates of Ahonglukumu are 39.194 deg latitude, 77.326 deg longitude, and 3,848 ft elevation. The topography within 2 miles of Ahonglukumu contains only modest variations in elevation, with a maximum elevation change of 105 feet and an average elevation above sea level of 3,839 feet. Within 10 miles also contains only modest variations in elevation (184 feet). Within 50 miles contains only modest variations in elevation (4,288 feet). The area within 2 miles of Ahonglukumu is covered by grassland (32%), bare soil (27%), sparse vegetation (27%), and cropland (14%), within 10 miles by bare soil (38%) and sparse vegetation (38%), and within 50 miles by grassland (42%) and bare soil (21%). Data SourcesThis report illustrates the typical weather in Ahonglukumu, based on a statistical analysis of historical hourly weather reports and model reconstructions from January 1, 1980 to December 31, 2016. Temperature and Dew PointThere is only a single weather station, Kashgar Airport, in our network suitable to be used as a proxy for the historical temperature and dew point records of Ahonglukumu. At a distance of 119 kilometers from Ahonglukumu, 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 Ahonglukumu 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. Other DataAll 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. DisclaimerThe 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. 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