Average Weather at Scholes Field Texas, United States
At Scholes Field, the summers are long, hot, and oppressive; the winters are short, cool, and windy; and it is wet and partly cloudy year round. Over the course of the year, the temperature typically varies from 49°F to 90°F and is rarely below 37°F or above 93°F.
Based on the tourism score, the best times of year to visit Scholes Field for warm-weather activities are from late March to mid May and from mid October to mid November.
The hot season lasts for 4.0 months, from May 27 to September 26, with an average daily high temperature above 84°F. The hottest day of the year is August 5, with an average high of 90°F and low of 80°F.
The cool season lasts for 2.9 months, from December 3 to March 1, with an average daily high temperature below 66°F. The coldest day of the year is January 6, with an average low of 49°F and high of 60°F.
Average High and Low Temperature
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.
Average Hourly Temperature
At Scholes Field, the average percentage of the sky covered by clouds experiences significant seasonal variation over the course of the year.
The clearer part of the year at Scholes Field begins around September 16 and lasts for 2.7 months, ending around December 6. On October 25, the clearest day of the year, the sky is clear, mostly clear, or partly cloudy 69% of the time, and overcast or mostly cloudy 31% of the time.
The cloudier part of the year begins around December 6 and lasts for 9.3 months, ending around September 16. On August 20, the cloudiest day of the year, the sky is overcast or mostly cloudy 53% of the time, and clear, mostly clear, or partly cloudy 47% of the time.
Cloud Cover Categories
0% clear 20% mostly clear 40% partly cloudy 60% mostly cloudy 80% overcast 100%
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. The chance of wet days at Scholes Field varies throughout the year.
The wetter season lasts 3.9 months, from May 23 to September 21, with a greater than 32% chance of a given day being a wet day. The chance of a wet day peaks at 42% on September 3.
The drier season lasts 8.1 months, from September 21 to May 23. The smallest chance of a wet day is 22% on March 31.
Among wet days, we distinguish between those that experience rain alone, snow alone, or a mixture of the two. Based on this categorization, the most common form of precipitation throughout the year is rain alone, with a peak probability of 42% on September 3.
Daily Chance of Precipitation
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. Scholes Field experiences significant seasonal variation in monthly rainfall.
Rain falls throughout the year at Scholes Field. The most rain falls during the 31 days centered around September 7, with an average total accumulation of 5.1 inches.
The least rain falls around March 3, with an average total accumulation of 3.1 inches.
Average Monthly Rainfall
The length of the day at Scholes Field varies significantly over the course of the year. In 2020, the shortest day is December 21, with 10 hours, 16 minutes of daylight; the longest day is June 20, with 14 hours, 1 minute of daylight.
Hours of Daylight and Twilight
The earliest sunrise is at 6:19 AM on June 10, and the latest sunrise is 1 hour, 17 minutes later at 7:36 AM on March 8. The earliest sunset is at 5:20 PM on December 1, and the latest sunset is 3 hours, 2 minutes later at 8:22 PM on June 30.
Daylight saving time (DST) is observed at Scholes Field during 2020, starting in the spring on March 8, lasting 7.8 months, and ending in the fall on November 1.
Sunrise & Sunset with Twilight and Daylight Saving Time
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.
Scholes Field experiences extreme seasonal variation in the perceived humidity.
The muggier period of the year lasts for 7.8 months, from March 25 to November 20, during which time the comfort level is muggy, oppressive, or miserable at least 27% of the time. The muggiest day of the year is July 20, with muggy conditions 100% of the time.
The least muggy day of the year is January 23, with muggy conditions 3% of the time.
Humidity Comfort Levels
dry 55°F comfortable 60°F humid 65°F muggy 70°F oppressive 75°F miserable
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 at Scholes Field experiences significant seasonal variation over the course of the year.
The windier part of the year lasts for 8.4 months, from September 27 to June 8, with average wind speeds of more than 10.3 miles per hour. The windiest day of the year is December 24, with an average hourly wind speed of 12.2 miles per hour.
The calmer time of year lasts for 3.6 months, from June 8 to September 27. The calmest day of the year is August 14, with an average hourly wind speed of 8.4 miles per hour.
Average Wind Speed
The predominant average hourly wind direction at Scholes Field varies throughout the year.
The wind is most often from the south for 6.9 months, from February 5 to September 3 and for 3.6 weeks, from November 10 to December 5, with a peak percentage of 72% on June 26. The wind is most often from the east for 2.2 months, from September 3 to November 10, with a peak percentage of 45% on September 21. The wind is most often from the north for 2.0 months, from December 5 to February 5, with a peak percentage of 36% on January 1.
Scholes Field 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 significant seasonal variation over the course of the year.
The time of year with warmer water lasts for 4.0 months, from June 1 to October 2, with an average temperature above 80°F. The day of the year with the warmest water is August 14, with an average temperature of 86°F.
The time of year with cooler water lasts for 3.3 months, from December 11 to March 20, with an average temperature below 65°F. The day of the year with the coolest water is January 30, with an average temperature of 60°F.
Average Water Temperature
Best Time of Year to Visit
To characterize how pleasant the weather is at Scholes Field 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 times of year to visit Scholes Field for general outdoor tourist activities are from late March to mid May and from mid October to mid November, with a peak score in the third week of April.
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 Scholes Field for hot-weather activities is from early May to mid June, with a peak score in the third week of May.
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).
While it does not do so every year, freezing temperatures are seen at Scholes Field over some winters. The day least likely to be in the growing season is January 16, with a 66% chance.
Time Spent in Various Temperature Bands and 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.
Based on growing degree days alone, the first spring blooms at Scholes Field should appear around January 16, only rarely appearing before January 10 or after January 29.
Growing Degree Days
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 significant seasonal variation over the course of the year.
The brighter period of the year lasts for 2.9 months, from April 4 to June 30, with an average daily incident shortwave energy per square meter above 5.9 kWh. The brightest day of the year is June 2, with an average of 6.6 kWh.
The darker period of the year lasts for 2.6 months, from November 14 to February 2, with an average daily incident shortwave energy per square meter below 3.7 kWh. The darkest day of the year is December 23, with an average of 3.0 kWh.
Average Daily Incident Shortwave Solar Energy
For the purposes of this report, the geographical coordinates of Scholes Field are 29.266 deg latitude, -94.860 deg longitude, and 0 ft elevation.
The topography within 2 miles of Scholes Field is essentially flat, with a maximum elevation change of 10 feet and an average elevation above sea level of 2 feet. Within 10 miles is also essentially flat (26 feet). Within 50 miles is essentially flat (112 feet).
The area within 2 miles of Scholes Field is covered by artificial surfaces (45%), water (26%), and herbaceous vegetation (14%), within 10 miles by water (73%) and herbaceous vegetation (10%), and within 50 miles by water (57%) and cropland (18%).
This report illustrates the typical weather at Scholes Field, 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
Scholes Field has a weather station that reported reliably enough during the analysis period that we have included it in our network. When available, historical temperature and dew point measurements are taken directly from this weather station. These records are obtained from NOAA's Integrated Surface Hourly data set, falling back on ICAO METAR records as required.
In the case of missing or erroneous measurements from this station, we fall back on records from nearby stations, adjusted according to typical seasonal and diurnal intra-station differences. For a given day of the year and hour of the day, the fallback station is selected to minimize the prediction error over the years for which there are measurements for both stations.
The stations on which we may fall back include but are not limited to Galveston Coast Guard Station, Pearland Regional Airport, Ellington Field, William P Hobby Airport, Texas Gulf Coast Regional Airport, Houston Southwest Airport, Houston Dunn Helistop, and George Bush Intercontinental Airport.
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 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.