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Encyclopedia > Megathermal

In climatology, the term megathermal (or less commonly, macrothermal) is sometimes used as a synonym for "tropical." Climatology is the science that studies climates and investigates their phenomena and causes. ... The tropics are the geographic region of the Earth centered on the equator and limited in latitude by the two tropics: the Tropic of Cancer in the north and the Tropic of Capricorn in the southern hemisphere. ...


The word megathermal is derived from two Greek words meaning "having great heat."


In order for a particular place to qualify as having a megathermal climate, every single month out of the year must have an average temperature of 18°C or above. Temperature is the physical property of a system which underlies the common notions of hot and cold; the material with the higher temperature is said to be hotter. ...


Megathermal climates are sometimes split into two temperature-based subsets — equatorial and tropical (the latter used here in the sense of "outer tropical") — with "equatorial" denoting little or no variation in temperature throughout the year and "tropical" denoting significant seasonal variation, even though no month has an average temperature of below 18°C. In addition, what temperature fluctuations do exist in an equatorial climate will typically bear no relationship to the astronomical seasons for the applicable side of the equator, while in the (outer) tropical subtype the temperature will move in concert with the seasons, the time of higher sun and longer days being warmest and the time of lower sun and shorter days coolest. The equator is an imaginary line drawn around a planet, halfway between the poles. ...


These climates can also be subdivided on the basis of rainfall, as examples of humid, semiarid and arid places can all be found within the megathermal category (although the region of arid megathermal climate is small compared with the extent of deserts existing in other climate zones, particularly the neighboring subtropical zone). Rain falling For other uses see Rain (disambiguation). ... Humidity is the quantity of moisture in the air. ... The steppe of Western Kazakhstan in early spring In physical geography, steppe (from Slavic step) is a plain without trees (apart from those near rivers and lakes); it is similar to a prairie, although a prairie is generally reckoned as being dominated by tall grasses, while short grasses are said... A dune in the Egyptian desert In geography, a desert is a landscape form or region that receives little precipitation. ... Subtropical climate is the form of climate found immediately poleward of the zone of tropical climate. ...


See also

Mesothermal
Microthermal In climatology, the term microthermal is used to denote the continental climates of Eurasia and North America. ...


  Results from FactBites:
 
Handbook of Texas Online: (4171 words)
The coast line from the Guadalupe River of Texas southward to central Tamaulipas has a chain of elongated, offshore barrier islands, behind which are shallow bays and lagoons.
The region's climate is megathermal and generally semiarid.
Though rainfall declines with distance from the coast, the region is not a true desert.
FLORA OF NORTH AMERICA - Volume 1, Chapter 3 (6296 words)
At the end of the Cretaceous, much of southeastern North America (30°--45° N) was covered by megathermal (mean annual temperature above 20° C) evergreen tropical woodland (estimated mean annual temperature above 25° C), and in the west by broad-leaved evergreen forests of dicotyledons and conifers (paratropical vegetation, estimated mean annual temperature 20°--25° C) (fig.
Collectively they reflect a seasonally dry, subtropical to warm temperate megathermal vegetation at the lower elevations, a deciduous broad-leaved mesothermal vegetation in the uplands, and locally at higher elevations a dominant coniferous element (D.I. Axelrod 1990), suggesting microthermal climates.
A comparable situation exists with the Miocene Mint Canyon flora of southern California and the Carmel flora near Monterey, California, both of which have been displaced 200--300 km from the south (D.I. Axelrod 1986), and late Cretaceous floras from western California and British Columbia that were transported at least 2000 km (N.O. Frederiksen 1987).
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