CLIMATE OF NEVADA

 

TOPOGRAPHIC FEATURES – Nevada is predominately a plateau.  The eastern part has an average elevation of between 5,000 and 6,000 feet.  The western part is between 3,800 and 5,000 feet, the lower limit being in the vicinity of Pyramid Lake and Carson Sink.  The southern part is generally between 2,000 and 3,000 feet.  From the lower elevations of the western portion there is a fairly rapid rise westward toward the summits of the Sierra Nevada.  The southwestern part slopes down toward Death Valley, California; the southern portion slopes toward the channel of the Colorado River, which is less than 1,000 feet above sea level.  The northeastern part slopes toward the north, draining into the Snake River and thence into the Columbia River Basin.

 

The Nevada plateau has several mountain ranges, most of them 50 to 100 miles long, running generally north-south.  The only east-west range is in the northeast where it forms the southern limit of the Columbia River Basin.  Except for this small drainage area and another limited region in the southeast which drains into the Colorado River, the State lies within the Great Basin, and the waters of its streams disappear into sinks or flow into lakes with no outlets.  Nevada has great climatic diversity, ranging from scorching lowland desert in the south to cool mountain forests in the north.  Its varied and rugged topography, mountain ranges, and narrow valleys range in elevation from about 1,500 to more than 10,000 feet above sea level.  Wide local variations of temperature and rainfall are common.  The principal climatic features are bright sunshine, small annual precipitation, (averaging nine inches in the valleys and deserts) heavy snowfall in the higher mountains, clean, dry air, and exceptionally large daily ranges of temperature.

 

TEMPERATURE – The mean annual temperatures vary from the middle 40’s in the northeast to about 50° F in the west and central areas and to the middle 60’s in the south.  In the northeast, summers are short and hot; winters are long and cold.  In the west, the summers are also short and hot, but the winters are only moderately cold;  in the south the summers are long and hot and the winters short and mild.  Long periods of extremely cold weather are rare, primarily because the mountains east and north of the State act as a barrier to the intensely cold continental arctic air masses.  However, on occasion, a cold air mass spills over these barriers and produces prolonged cold waves.

 

There is strong surface heating during the day and rapid nighttime cooling because of the dry air, resulting in wide daily ranges in temperature.  Even after the hottest days, the nights are usually cool.  The average range between the highest and the lowest daily temperatures is about 30 to 35 degrees.  Daily ranges are larger in summer than the winter.  Extreme temperatures have ranged from 120° F to 50° below zero.

 

Summer temperatures above 100° F occur rather frequently in the south and occasionally over the rest of the State.  Humidity is usually low so that the higher temperatures are less disagreeable in Nevada than in more humid climates.  During the warmer season of the year, air conditioning is used in a large percentage of the commercial establishments and in many homes.  Owing to the dryness of the air, evaporative coolers operate very efficiently.  Over the northern and central portions of the State, freezes begin early in the autumn and continue until late in the spring.  The freeze-free season varies from less than 70 days in the northwest and northeast to about 140 days in the west and south-central areas, to over 225 in the south.

 

PRECIPITATION – Nevada lies on the eastern, lee side of the Sierra Nevada Range, a massive mountain barrier that markedly influences the climate of the State.  One of the greatest contrasts in precipitation found within a short distance in the United States occurs between the western slopes of the Sierras in California and the valleys just to the east of this range.  The prevailing winds are from the west, and as the warm moist air from the Pacific Ocean ascends the western slopes of the Sierra Range, the air cools, condensation takes place and most of the moisture falls as precipitation.  As the air descends the eastern slope, it is warmed by compression, and very little precipitation occurs.  The effects of this mountain barrier are felt not only in the west but throughout the State, with the result that the lowlands of Nevada are largely desert or steppes.

 

A winter precipitation maximum occurs in the western and south-central portions of the State, a spring maximum in the central and northeastern sections, and a summer maximum primarily in the eastern portion where thunderstorms are most frequent.  Precipitation is lightest over the lower parts of the western plateau, a series of long valleys extending from the State border opposite Death Valley in California northward to the Idaho line.  In the southern part of those valleys, the average annual precipitation is less than five inches.  It increases to 18 inches in Lamoille Canyon on the western side of the Ruby Mountains of northeast Nevada and to about 40 inches in the Sierra Nevada.  Variations in precipitation are due mainly to differences in elevation and exposure to precipitation-bearing storms.

 

The average annual number of days with precipitation of 0.01 inch or more varies considerably; Las Vegas averages 23, Reno 49, Winnemucca 67, Ely 72, and Elko 78.

 

Snowfall is usually heavy in the mountains, particularly in the north.  This is conducive to many winter sports activities, including skiing and hunting.  Twenty-four hour snowfall can amount to over 45 inches, while seasonal totals of over 300 inches have been recorded.

 

FLOODS – Mountain snowfall forms the main source of water for streamflow.  Melting of the mountain snowpack in the spring usually causes some flooding in northern and western streams during April to June, but damaging floods of this type are infrequent; however, extensive flooding from melting of heavy snowpack has occurred in both the southern and northern parts of the State.  Flooding can also be caused by a combination of warm rains and melting snow, especially in the western section.  Heavy summer thunderstorms occasionally cause flooding of local streams, but they usually occur in sparsely settled mountainous areas and are seldom destructive.  These storms, locally termed cloudbursts, may bring to a locality as much rain in a few hours as would normally fall in several months.

 

SEVERE STORMS – Thunderstorms in most areas are infrequent, the average annual number of days being 13 at Reno, 15 at Las Vegas and Winnemucca, 21 at Elko, and 33 at Ely.  Tornadoes are rare, but have occurred in all months from April through September.  Winds are generally light.  Storms with high winds rarely occur and seldom cause appreciable damage, except locally along the east slope of the Sierras.  The prevailing wind direction is west; at a few stations it is south or southwest because of local topography.  In the valleys winds are light in the morning and stronger in the afternoon.  In Reno and Las Vegas, for example, winds of zero to three miles per hour are most common about 8 AM.  This is also the time of peak automobile traffic and pollutants accumulate due to the light winds.

 

Dust or sand storms occur occasionally, particularly in the south during the spring, when storms move through the region more frequently than at other seasons.

 

AGRICULTURE – The State has a generous supply of sunshine, the average percentage of possible sunshine being abut 65 to 75 at northern and central locations and above 80 percent in the south.  The low humidity and abundant sunshine produce rapid evaporation.  Annual amounts in the southern portion of the State, as measured in evaporation pans, average over 100 inches.  In northern and central sections, evaporation amounts average roughly half as much.

 

Because of the generally arid climate only about six percent of the 110,000 square miles of land is under cultivation.  Irrigation is maintained in the cultivated areas by impounding the water from melting snow.  The Sierra Nevada snowpack provides water for the valleys of Walker, Carson, Truckee and Fallon.  Well water is also used to irrigate a large number of acres.  In the vicinity of Lovelock, water is impounded in the Rye Patch Reservoir.  A small additional area in pastures and wild hay is watered by flooding when snows melt in the spring.  A light snowfall in winter and spring creates a shortage of water for irrigation.

 

Long dry spells in summer, which occur rather frequently, result in injury to ranges and pastures, but have little effect on irrigated crops which depend almost entirely on stored water.

 

Livestock raising is one of the principal activities of the State.  Alfalfa for hay and for seed is by far the most important agricultural crop, although small quantities of grains, fruits, vegetables, and cotton are grown.

 

OTHER FEATURES – Mining is the other basic industry in Nevada.  The State ranks high in the amount and value of minerals it produces each year, principally manganese, tungsten, mercury, copper, silver, gold, lead, and zinc.

 

Many tourists come to Nevada each year to vacation at Lake Tahoe, the “sky-high” lake that straddles the Nevada-California line in the rugged Sierras, to visit the numerous ghost towns, to fish or boat in the lakes such as Lake Mead, Pyramid Lake and Walker Lake, or to enjoy the cool mountain streams of the State.  The spectacular manmade landmark of the Far West, Hoover Dam, is located on the State line between Nevada and Arizona.  Las Vegas and Reno are also popular spots with their many hotels, casinos, and golf courses.