July Weather in Lichuan ChinaDaily high temperatures increase by 2°F, from 78°F to 80°F, rarely falling below 73°F or exceeding 84°F. Daily low temperatures are around 65°F, rarely falling below 59°F or exceeding 69°F. The highest daily average low temperature is 66°F on July 22. For reference, on July 31, the hottest day of the year, temperatures in Lichuan typically range from 66°F to 80°F, while on January 19, the coldest day of the year, they range from 27°F to 42°F. The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on July. 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. Bluewell, United States (7,728 miles away) is the far-away foreign place with temperatures most similar to Lichuan (view comparison). CloudsThe month of July in Lichuan experiences decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 65% to 55%. The highest chance of overcast or mostly cloudy conditions is 65% on July 3. The clearest day of the month is July 31, with clear, mostly clear, or partly cloudy conditions 45% of the time. For reference, on July 3, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 65%, while on January 14, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 67%. PrecipitationA wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Lichuan, the chance of a wet day over the course of July is very rapidly decreasing, starting the month at 49% and ending it at 39%. For reference, the year's highest daily chance of a wet day is 49% on July 4, and its lowest chance is 6% on December 30. RainfallTo 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 July in Lichuan is very rapidly decreasing, starting the month at 7.8 inches, when it rarely exceeds 12.3 inches or falls below 4.3 inches, and ending the month at 5.6 inches, when it rarely exceeds 10.0 inches or falls below 1.9 inches. SunOver the course of July in Lichuan, the length of the day is gradually decreasing. From the start to the end of the month, the length of the day decreases by 28 minutes, implying an average daily decrease of 55 seconds, and weekly decrease of 6 minutes, 26 seconds. The shortest day of the month is July 31, with 13 hours, 37 minutes of daylight and the longest day is July 1, with 14 hours, 4 minutes of daylight. The earliest sunrise of the month in Lichuan is 5:46 AM on July 1 and the latest sunrise is 16 minutes later at 6:02 AM on July 31. The latest sunset is 7:50 PM on July 1 and the earliest sunset is 11 minutes earlier at 7:39 PM on July 31. Daylight saving time is not observed in Lichuan during 2024. For reference, on June 20, the longest day of the year, the Sun rises at 5:43 AM and sets 14 hours, 6 minutes later, at 7:49 PM, while on December 21, the shortest day of the year, it rises at 7:37 AM and sets 10 hours, 11 minutes later, at 5:48 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 July 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 Lichuan is rapidly increasing during July, rising from 65% to 84% over the course of the month. The highest chance of a muggy day during July is 85% on July 26. For reference, on July 25, the muggiest day of the year, there are muggy conditions 85% of the time, while on October 31, 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 Lichuan is essentially constant during July, remaining within 0.3 miles per hour of 5.5 miles per hour throughout. For reference, on March 9, the windiest day of the year, the daily average wind speed is 6.2 miles per hour, while on October 17, the calmest day of the year, the daily average wind speed is 4.6 miles per hour. The highest daily average wind speed during July is 5.8 miles per hour on July 13. The hourly average wind direction in Lichuan throughout July is predominantly from the south, with a peak proportion of 63% on July 20. 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 Lichuan typically lasts for 7.9 months (243 days), from around March 20 to around November 18, rarely starting before March 1 or after April 9, and rarely ending before October 31 or after December 5. The month of July in Lichuan is reliably fully 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 Lichuan are rapidly increasing during July, increasing by 663°F, from 1,227°F to 1,890°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 Lichuan is essentially constant during July, remaining within 0.1 kWh of 5.9 kWh throughout. The highest average daily incident shortwave solar energy during July is 6.0 kWh on July 25. TopographyFor the purposes of this report, the geographical coordinates of Lichuan are 30.300 deg latitude, 108.850 deg longitude, and 4,117 ft elevation. The topography within 2 miles of Lichuan contains very significant variations in elevation, with a maximum elevation change of 1,253 feet and an average elevation above sea level of 3,869 feet. Within 10 miles contains very significant variations in elevation (2,572 feet). Within 50 miles contains large variations in elevation (6,585 feet). The area within 2 miles of Lichuan is covered by trees (51%), cropland (25%), and grassland (19%), within 10 miles by trees (57%) and cropland (22%), and within 50 miles by trees (52%) and cropland (21%). Data SourcesThis report illustrates the typical weather in Lichuan, based on a statistical analysis of historical hourly weather reports and model reconstructions from January 1, 1980 to December 31, 2016. Lichuan is further than 200 kilometers from the nearest reliable weather station, so the weather-related data on this page were taken entirely from NASA's MERRA-2 satellite-era reanalysis . 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. The temperature and dew point estimates are corrected for the difference between the reference elevation of the MERRA-2 grid cell and the elevation of Lichuan, according to the International Standard Atmosphere . 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. 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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