Inmeteorology,diurnal temperature variation is the variation between a highair temperature and a low temperature that occurs during the sameday.
Temperature lag, also known asthermal inertia, is an important factor in diurnal temperature variation. Peak daily temperature generally occursafter noon, as air keeps absorbing net heat for a period of time from morning through noon and some time thereafter. Similarly, minimum daily temperature generally occurs substantially after midnight, indeed occurring during early morning in the hour around dawn, since heat is lost all night long. The analogous annual phenomenon isseasonal lag.
As solar energy strikes the Earth's surface each morning, a shallow 1–3-centimetre (0.39–1.18 in) layer of air directly above the ground is heated by conduction. Heat exchange between this shallow layer of warm air and the cooler air above is very inefficient. On a warm summer's day, for example, air temperatures may vary by 16.5 °C (30 °F) from just above the ground to chest height. Incoming solar radiation exceeds outgoing heat energy for many hours after noon and equilibrium is usually reached from 3–5 p.m., but this may be affected by a variety of factors such as large bodies of water, soil type and cover, wind, cloud cover/water vapor, and moisture on the ground.[1]
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Diurnal temperature variations are greatest very near Earth's surface. TheTibetan andAndean Plateaus present one of the largest differences in daily temperature on the planet, as does theWestern US and the western portion ofsouthern Africa.
High desert regions typically have the greatest diurnal-temperature variations, while low-lying humid areas near the shores (tropical, oceanic, and arctic) typically have the least. Large cities (urban heat islands) also tend to have a lower diurnal temperature variation than surrounding areas. This explains why an area like thePinnacles National Park can have high temperatures of 38 °C (100 °F) during a summer day, and then have lows of 5–10 °C (41–50 °F). At the same time,Washington D.C., which is much more humid, has temperature variations of only 8 °C (14 °F);[1]urbanHong Kong has a diurnal temperature range of little more than 4 °C (7.2 °F).
While theNational Park Service claimed that the world single-day record is a variation of 102 °F (56.7 °C) (from 46 °F or 7.8 °C to −56 °F or −48.9 °C) inBrowning, Montana in 1916,[2] the Montana Department of Environmental Quality claimed thatLoma, Montana also had a variation of 102 °F (56.7 °C) (from −54 °F or −47.8 °C to 48 °F or 8.9 °C) in 1972.[3] Both these extreme daily temperature changes were the result of sharp air-mass changes within a single day. The 1916 event was an extreme temperature drop, resulting from frigid Arctic air from Canada invading northern Montana, displacing a much warmer air mass. The 1972 event was achinook event, where air from the Pacific Ocean overtopped mountain ranges to the west, and dramatically warmed in its descent into Montana, displacing frigid Arctic air and causing a drastic temperature rise.
In the absence of such extreme air-mass changes, diurnal temperature variations typically range from 10 °F (5.6 °C) or smaller in humid, tropical areas, up to 40 to 50 °F (22.2 to 27.8 °C) in higher-elevation, arid to semi-arid areas, such as parts of the U.S. Western states' Intermountain Plateau areas, for exampleElko, Nevada,Ashton, Idaho andBurns, Oregon. The higher thehumidity is, the lower the diurnal temperature variation is.
InEurope, due to its more northern latitude and close proximity to large warm water bodies (such as theMediterranean), differences in daily temperature are not as pronounced as in other continents. However, places inSouthern Europe significantly far from the Mediterranean tend to have high differences in daily temperatures, some around 14 °C (25 °F). These include SouthwesternIberia (e.g.Alvega orBadajoz) or the high-altitude plateaus of Turkey (if considered part of Europe) (e.g.Kayseri).
InAustralia, significant diurnal temperature variations generally occur in theRed Centre aroundAlice Springs andUluru.
Diurnal temperature variation is of particular importance inviticulture.Wine regions situated in areas of highaltitude experience the most dramatic swing in temperature variation during the course of a day. Ingrapes, this variation has the effect of producing highacid and highsugar content as the grapes' exposure tosunlight increases the ripening qualities while the sudden drop in temperature at night preserves the balance of natural acids in the grape.[4]