There are an average of 24 days annually with measurable precipitation. Snowfall is uncommon in winter, and many years can go by without any measurable snowfall. The average annual precipitation is 4.96 inches (12.6 cm), with nearly 80% of rain typically falling during the cooler months (Nov–Apr). There are an average of 133 days with highs of 90 ☏ (32 ☌) or higher, an average of 68 days with highs of 100 ☏ (38 ☌) degrees or higher, and an average of 32 days with lows of 32 ☏ (0 ☌) or lower. Daily temperature ranges are largely a result of the low atmospheric moisture, typically between 25 and 30 ☏ (14 and 17 ☌) difference. Winter, in contrast, is characterized by cold mornings, with lows near 30 ☏ (−1 ☌). Summer days are very hot, with highs typically exceeding 100 ☏ (38 ☌). Climate īarstow experiences an arid climate, and has four seasons. Geography Īccording to the United States Census Bureau, the city has a total area of 107.2 km 2 (41.4 sq mi), 99.98% land and 0.02% water. Some early Barstow names were Camp Sugarloaf, Grapevine, Waterman Junction and Fishpond. The two routes met in downtown Barstow and continued west together to Los Angeles.īarstow is named after William Barstow Strong, former president of the Atchison, Topeka and Santa Fe Railway. Before the advent of the interstate highway system, Barstow was an important stop on both Routes 66 and 91. Much of its economy depends on transportation. Paving the major highways through Barstow led to further development of the city. In 1884, ownership of the line from Needles to Mojave was transferred to the Santa Fe Railroad. The Southern Pacific built a line from Mojave, California through Barstow to Needles in 1883. Due to the influx of miners arriving in Calico and Daggett, railroads were constructed to transport goods and people. īarstow's roots also lie in the rich mining history of the Mojave Desert following the discovery of gold and silver in the Owens Valley and in mountains to the east in the 1860s and 1870s. Trading posts were established at Grapevines and Fish Ponds that supplied travelers on the roads and increasingly the miners that came into the Mojave Desert after the end of hostilities with the native people. Army post 20 miles (32 km) east of Barstow, was occupied sporadically until 1864, then permanently, by soldiers occupying other posts on the Mojave Road or patrolling in the region until 1871. Troubles with the Paiute, Mojave, and Chemehuevi tribes followed, and from 1860 Camp Cady, a U.S. In 1859, the Mojave Road followed a route that was established from Los Angeles to Fort Mojave through Grapevines that linked eastward with the Beale Wagon Road across northern New Mexico Territory to Santa Fe. These travelers followed the course of the Mojave River, watering and camping at Fish Ponds on its south bank (west of Nebo Center) or 3.625 miles up river on the north bank, at a riverside grove of willows and cottonwoods, festooned with wild grapes, called Grapevines (later the site of North Barstow). Trains of freight wagons traveled back to Salt Lake City and other points in the interior. People, goods, and animal herds would move from New Mexico and later Utah to Los Angeles, along the Old Spanish Trail from Santa Fe, or after 1848, on the Mormon Road from Salt Lake City. Every fall and winter, as the weather cooled, the rain produced new grass growth and replenished the water sources in the Mojave Desert. » Click here for Salt Lake City Time to Local Time Conversion.The settlement of Barstow began in the late 1840s in the Mormon Corridor. » Click here for NZDT to Local Time Conversion.
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