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Summer Weather in Antelope Valley-Crestview Wyoming, United States

Daily high temperatures increase by 10°F, from 71°F to 81°F, rarely falling below 58°F or exceeding 95°F. The highest daily average high temperature is 86°F on July 26.

Daily low temperatures increase by 6°F, from 46°F to 52°F, rarely falling below 38°F or exceeding 65°F. The highest daily average low temperature is 58°F on July 29.

For reference, on July 26, the hottest day of the year, temperatures in Antelope Valley-Crestview typically range from 58°F to 86°F, while on December 28, the coldest day of the year, they range from 14°F to 33°F.

Average High and Low Temperature in the Summer in Antelope Valley-Crestview

Average High and Low Temperature in the Summer in Antelope Valley-CrestviewJunJulAug30°F30°F40°F40°F50°F50°F60°F60°F70°F70°F80°F80°F90°F90°F100°F100°FSpringFallJul 2686°FJul 2686°F58°F58°FJun 171°FJun 171°F46°F46°FAug 3181°FAug 3181°F52°F52°FJul 183°FJul 183°F54°F54°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 summer 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 Summer in Antelope Valley-Crestview

Average Hourly Temperature in the Summer in Antelope Valley-CrestviewJunJulAug12 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 AMSpringFallvery coldcoldcoldcoldcoldcoolcomfortablewarmvery cold
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.

Kelkit, Turkey (6,221 miles away); Yüksekova, Turkey (6,485 miles); and Fareydūnshahr, Iran (6,896 miles) are the far-away foreign places with temperatures most similar to Antelope Valley-Crestview (view comparison).

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The summer in Antelope Valley-Crestview experiences rapidly decreasing cloud cover, with the percentage of time that the sky is overcast or mostly cloudy decreasing from 43% to 28%. The lowest chance of overcast or mostly cloudy conditions is 23% on July 3.

The clearest day of the summer is July 3, with clear, mostly clear, or partly cloudy conditions 77% of the time.

For reference, on March 19, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 55%, while on July 3, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 77%.

Cloud Cover Categories in the Summer in Antelope Valley-Crestview

Cloud Cover Categories in the Summer in Antelope Valley-CrestviewJunJulAug0%100%10%90%20%80%30%70%40%60%50%50%60%40%70%30%80%20%90%10%100%0%SpringFallMar 1945%Mar 1945%Jun 157%Jun 157%Aug 3172%Aug 3172%Jul 176%Jul 176%Aug 176%Aug 176%clearmostly clearpartly 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 Antelope Valley-Crestview, the chance of a wet day over the course of the summer is very rapidly decreasing, starting the season at 31% and ending it at 12%.

For reference, the year's highest daily chance of a wet day is 31% on June 1, and its lowest chance is 3% on January 15.

Probability of Precipitation in the Summer in Antelope Valley-Crestview

Probability of Precipitation in the Summer in Antelope Valley-CrestviewJunJulAug0%0%5%5%10%10%15%15%20%20%25%25%30%30%SpringFallJun 131%Jun 131%Aug 3112%Aug 3112%Jul 118%Jul 118%Aug 118%Aug 118%rainmixed
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 summer in Antelope Valley-Crestview is rapidly decreasing, starting the season at 2.0 inches, when it rarely exceeds 3.8 inches or falls below 0.6 inches, and ending the season at 0.7 inches, when it rarely exceeds 1.5 inches or falls below 0.1 inches.

The lowest average 31-day accumulation is 0.7 inches on August 25.

Average Monthly Rainfall in the Summer in Antelope Valley-Crestview

Average Monthly Rainfall in the Summer in Antelope Valley-CrestviewJunJulAug0 in0 in1 in1 in2 in2 in3 in3 in4 in4 inSpringFallAug 250.7 inAug 250.7 inJun 12.0 inJun 12.0 inJul 11.1 inJul 11.1 inAug 10.9 inAug 10.9 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 summer in Antelope Valley-Crestview, the length of the day is very rapidly decreasing. From the start to the end of the season, the length of the day decreases by 2 hours, 4 minutes, implying an average daily decrease of 1 minute, 22 seconds, and weekly decrease of 9 minutes, 33 seconds.

The shortest day of the summer is August 31, with 13 hours, 14 minutes of daylight and the longest day is June 20, with 15 hours, 31 minutes of daylight.

Hours of Daylight and Twilight in the Summer in Antelope Valley-Crestview

Hours of Daylight and Twilight in the Summer in Antelope Valley-CrestviewJunJulAug0 hr24 hr4 hr20 hr8 hr16 hr12 hr12 hr16 hr8 hr20 hr4 hr24 hr0 hrSpringFallJun 2015 hr, 31 minJun 2015 hr, 31 minnightnightdaydayAug 3113 hr, 14 minAug 3113 hr, 14 minAug 114 hr, 35 minAug 114 hr, 35 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 earliest sunrise of the summer in Antelope Valley-Crestview is 5:17 AM on June 14 and the latest sunrise is 1 hour, 7 minutes later at 6:24 AM on August 31.

The latest sunset is 8:49 PM on June 25 and the earliest sunset is 1 hour, 11 minutes earlier at 7:38 PM on August 31.

Daylight saving time is observed in Antelope Valley-Crestview during 2024, but it neither starts nor ends during the summer, so the entire season is in standard time.

For reference, on June 20, the longest day of the year, the Sun rises at 5:18 AM and sets 15 hours, 31 minutes later, at 8:49 PM, while on December 21, the shortest day of the year, it rises at 7:34 AM and sets 8 hours, 52 minutes later, at 4:26 PM.

Sunrise & Sunset with Twilight in the Summer in Antelope Valley-Crestview

Sunrise & Sunset with Twilight in the Summer in Antelope Valley-CrestviewJunJulAug2 AM4 AM6 AM8 AM10 AM12 PM2 PM4 PM6 PM8 PM10 PM12 AMSpringFall5:17 AM5:17 AMJun 148:47 PMJun 148:47 PM6:24 AM6:24 AMAug 317:38 PMAug 317:38 PM5:22 AM5:22 AMJul 18:49 PMJul 18:49 PM5:50 AM5:50 AMAug 18:25 PMAug 18:25 PMSolarMidnightSolarMidnightSolarNoonSunriseSunset
The solar day in the summer. 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 Summer in Antelope Valley-Crestview

Solar Elevation and Azimuth in the Summer in Antelope Valley-CrestviewJunJulAug12 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 AMSpringFall00102020303040506000101020303040405060
northeastsouthwest
Solar elevation and azimuth in the the summer 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 summer 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 Summer in Antelope Valley-Crestview

Moon Rise, Set & Phases in the Summer in Antelope Valley-CrestviewJunJulAug12 AM12 AM4 AM4 AM8 AM8 AM12 PM12 PM4 PM4 PM8 PM8 PM12 AM12 AMSpringFallMay 79:23 PMMay 79:23 PMMay 237:54 AMMay 237:54 AMJun 66:38 AMJun 66:38 AMJun 217:09 PMJun 217:09 PMJul 54:58 PMJul 54:58 PMJul 214:18 AMJul 214:18 AMAug 45:14 AMAug 45:14 AMAug 1912:26 PMAug 1912:26 PMSep 27:56 PMSep 27:56 PMSep 178:35 PMSep 178:35 PM5:13 AM5:13 AM8:13 PM8:13 PM8:07 PM8:07 PM5:06 AM5:06 AM4:55 AM4:55 AM9:40 PM9:40 PM9:15 PM9:15 PM5:22 AM5:22 AM9:19 PM9:19 PM8:47 PM8:47 PM5:28 AM5:28 AM8:56 PM8:56 PM7:54 PM7:54 PM5:45 AM5:45 AM7:42 PM7:42 PM7:06 PM7:06 PM7:22 AM7:22 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 Antelope Valley-Crestview is essentially constant during the summer, remaining around 0% throughout.

For reference, on July 3, the muggiest day of the year, there are muggy conditions 0% of the time, while on January 1, the least muggy day of the year, there are muggy conditions 0% of the time.

Humidity Comfort Levels in the Summer in Antelope Valley-Crestview

Humidity Comfort Levels in the Summer in Antelope Valley-CrestviewJunJulAug0%0%10%10%20%20%30%30%40%40%50%50%60%60%70%70%80%80%90%90%100%100%SpringFallJul 30%Jul 30%Jun 10%Jun 10%Aug 310%Aug 310%Aug 10%Aug 10%drydryhumidhumid
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 Antelope Valley-Crestview is gradually decreasing during the summer, decreasing from 10.1 miles per hour to 9.5 miles per hour over the course of the season.

For reference, on January 17, the windiest day of the year, the daily average wind speed is 11.5 miles per hour, while on July 25, the calmest day of the year, the daily average wind speed is 8.8 miles per hour.

The lowest daily average wind speed during the summer is 8.8 miles per hour on July 25.

Average Wind Speed in the Summer in Antelope Valley-Crestview

Average Wind Speed in the Summer in Antelope Valley-CrestviewJunJulAug0 mph0 mph5 mph5 mph10 mph10 mph15 mph15 mphSpringFallJul 258.8 mphJul 258.8 mphJun 110.1 mphJun 110.1 mphAug 319.5 mphAug 319.5 mphJul 19.3 mphJul 19.3 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 Antelope Valley-Crestview during the summer is predominantly out of the north from June 1 to June 25 and the south from June 25 to August 31.

Wind Direction in the Summer in Antelope Valley-Crestview

Wind Direction in the Summer in Antelope Valley-CrestviewNSNJunJulAug0%100%20%80%40%60%60%40%80%20%100%0%SpringFallwestsouthnortheast
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).

The growing season in Antelope Valley-Crestview typically lasts for 4.4 months (136 days), from around May 15 to around September 28, rarely starting before April 28 or after June 1, and rarely ending before September 9 or after October 15.

The summer in Antelope Valley-Crestview is more likely than not fully within the growing season, with the chance that a given day is in the growing season reaching a high of 100% on July 24.

Time Spent in Various Temperature Bands and the Growing Season in the Summer in Antelope Valley-Crestview

Time Spent in Various Temperature Bands and the Growing Season in the Summer in Antelope Valley-Crestviewgrowing seasonJunJulAug0%100%10%90%20%80%30%70%40%60%50%50%60%40%70%30%80%20%90%10%100%0%SpringFall90%Jun 190%Jun 198%Aug 3198%Aug 31100%Jul 1100%Jul 1100%Aug 1100%Aug 150%May 1550%May 1550%Sep 2850%Sep 28Jul 24100%Jul 24100%very coldcoldcoolcomfortablewarmhotfreezing
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 Antelope Valley-Crestview are very rapidly increasing during the summer, increasing by 1,564°F, from 299°F to 1,863°F, over the course of the season.

Growing Degree Days in the Summer in Antelope Valley-Crestview

Growing Degree Days in the Summer in Antelope Valley-CrestviewJunJulAug200°F200°F400°F400°F600°F600°F800°F800°F1,000°F1,000°F1,200°F1,200°F1,400°F1,400°F1,600°F1,600°F1,800°F1,800°F2,000°F2,000°FSpringFallJun 1299°FJun 1299°FAug 311,863°FAug 311,863°FJul 1691°FJul 1691°FAug 11,308°FAug 11,308°F
The average growing degree days accumulated over the course of the summer, 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 Antelope Valley-Crestview is decreasing during the summer, falling by 1.2 kWh, from 7.3 kWh to 6.1 kWh, over the course of the season.

The highest average daily incident shortwave solar energy during the summer is 7.9 kWh on July 2.

Average Daily Incident Shortwave Solar Energy in the Summer in Antelope Valley-Crestview

Average Daily Incident Shortwave Solar Energy in the Summer in Antelope Valley-CrestviewJunJulAug0 kWh0 kWh1 kWh1 kWh2 kWh2 kWh3 kWh3 kWh4 kWh4 kWh5 kWh5 kWh6 kWh6 kWh7 kWh7 kWh8 kWh8 kWh9 kWh9 kWhSpringFallJul 27.9 kWhJul 27.9 kWhJun 17.3 kWhJun 17.3 kWhAug 316.1 kWhAug 316.1 kWhAug 17.2 kWhAug 17.2 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 Antelope Valley-Crestview are 44.225 deg latitude, -105.474 deg longitude, and 4,678 ft elevation.

The topography within 2 miles of Antelope Valley-Crestview contains significant variations in elevation, with a maximum elevation change of 528 feet and an average elevation above sea level of 4,688 feet. Within 10 miles also contains significant variations in elevation (794 feet). Within 50 miles contains significant variations in elevation (2,667 feet).

The area within 2 miles of Antelope Valley-Crestview is covered by grassland (94%), within 10 miles by grassland (91%), and within 50 miles by grassland (85%) and shrubs (14%).

This report illustrates the typical weather in Antelope Valley-Crestview, 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 Antelope Valley-Crestview.

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