Английская Википедия:Climate of Oregon

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Шаблон:Short description

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Köppen climate types of Oregon, using 1991-2020 climate normals.
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Trewartha climate types of Oregon

According to the Köppen climate classification, most of Western Oregon has a warm-summer Mediterranean climate (or Csb type), which features warm, dry summers, and wet winters with frequent overcast and cloudy skies. Eastern Oregon falls into the cold semi-arid climate (or BSk type), which features drier weather.

West of the Cascade Range, winters are chilly with frequent rain and occasional snow. Temperatures can get very cold, but only occasionally, as the result of Arctic cold waves. The high desert region of the state is much drier, with less rain, more snow, colder winters, and hotter summers.[1]

Precipitation

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Oregon rainfall varies widely from region to region.

Precipitation in the state varies widely: some western coastal slopes approach Шаблон:Convert annually, while the driest places, such as the Alvord Desert (in the rain shadow of Steens Mountain) in eastern Oregon, get as little as Шаблон:Convert.Шаблон:Sfn[2]

The Pacific Ocean, the moisture-laden air above it, and the storms moving from it over the Oregon coast, are major factors in the state's precipitation patterns. As humid ocean air flows east from the ocean and encounters the Coast Range, it rises steeply, cools, and loses moisture through condensation, which produces heavy rain. The heaviest precipitation in the state occurs at Шаблон:Convert above sea level in these coastal mountains. At lower elevations along the coast, orographic precipitation is less intense but still produces Шаблон:Convert a year.Шаблон:Sfn

In the Willamette Valley east of the Coast Range, storms "blowing" from the Pacific retain enough moisture to drop from Шаблон:Convert annually in the most heavily populated part of the state. East of the valley, the storm air rises again as it meets the Cascade Range, cooling once more and forming condensate at elevations often as low as Шаблон:Convert.Шаблон:Sfn Since volcanic peaks in the range are quite high—more than Шаблон:Convert in the case of Mount HoodШаблон:Sfn—most of the remaining Pacific moisture falls here in the form of rain or snow.Шаблон:Sfn

The remaining two-thirds of the state is relatively dry, classified as semi-arid, with large areas receiving no more than Шаблон:Convert a year. Exceptions occur at higher elevations in the Blue Mountains and the Wallowa Mountains to the northeast, which get Шаблон:Convert a year.Шаблон:Sfn

Across Oregon, the wet season runs from November through March, when the jet stream is strongest in the Northern Hemisphere. Precipitation is less in the months between winter and summer: April through June in the spring and September and October in the fall. Statewide, the dry months are July and August, when moisture arrives during afternoon thunderstorms, mainly in the mountains, and less often from storms that reach the north coast and adjacent counties.Шаблон:Sfn

Snow

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The heaviest snowfalls in Oregon occur in the Cascade Range.

Snowfall in Oregon is greatest in the Cascade Range. Based on data from ski resorts and a few official weather stations, average annual snowfall in the Cascades can range from Шаблон:Convert.[2] The state's largest annual snowfall on record, Шаблон:Convert, occurred at Crater Lake in the Cascades in 1950.Шаблон:Sfn In the Blue Mountains of eastern Oregon, snowfall totals can also be large, between Шаблон:Convert. On the other hand, most winter precipitation in the Coast Range falls as rain, though heavy snow sometimes occurs.[2]

In most mountain areas in Oregon, the ground above Шаблон:Convert is covered with snow from December through April. Snow depths, which vary with elevation and time of year, average an estimated Шаблон:Convert in the Cascades and Шаблон:Convert in the Blue Mountains at the end of January; by the end of April, they diminish to Шаблон:Convert in the Cascades and Шаблон:Convert in the Blues. Glaciers remain year-round on some Cascade peaks higher than Шаблон:Convert above sea level.[2]

Annual snowfall along the coastal plain averages Шаблон:Convert a year, including years with none. Further inland, between the Coast Range and the Cascades, snowfall generally averages from Шаблон:Convert a year. East of the Cascades, in non-mountain settings, the annual totals range from Шаблон:Convert, depending on location; they are smallest in the north-central region and the Snake River basin in the southeast and largest in the northeastern valleys and in the high plateaus of the south-central part of the state.[2]

Temperature

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The High Desert region of Oregon

In addition to seasonal cycles in solar radiation (more in summer, less in winter), major factors affecting temperatures in Oregon include the moderating influence of the Pacific Ocean combined with variations in surface elevation, especially the Cascade Range. In general, temperatures on Earth drop by about 4 °F (2 °C) per each Шаблон:Convert increase in elevation. Throughout the year, high elevations across the state tend to be cooler than low elevations. In addition, the Cascades, running north–south from border to border, generally retain relatively warm Pacific air masses on the western side of the state and relatively cool continental air masses on the eastern side. This prevailing pattern breaks down occasionally when dense cold air flows down the Columbia Gorge into the Willamette Valley and lowers temperatures more than usual from Portland to Eugene.Шаблон:Sfn

Oregon has a wide range of temperatures, though the extremes are rare.[2] The highest was recorded on July 29, 1898, in Hermiston, Oregon, and again on August 10, 1898, in Redmond, Oregon, both east of the Cascades, when the temperature reached Шаблон:Convert.Шаблон:Sfn The lowest occurred on February 9, 1933, in Ukiah, and again on February 10, 1933, in Seneca, also both east of the Cascades, when the temperature dropped to Шаблон:Convert.Шаблон:Sfn The temperature in the Willamette Valley is mild compared to the desert regions of the state, with high temperatures at or above Шаблон:Convert occurring only five to fifteen times per year, and low temperatures below Шаблон:Convert similarly infrequent.[3] The hottest area of the state is the southwest; Jackson County is the warmest place in the state during summer.[4]

Selected climate charts

Шаблон:Location map+

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See also

References

Шаблон:Reflist

Works cited

Шаблон:Oregon Шаблон:ClimateUS