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The climate and ecology of different locations on the globe naturally separate into life zones, depending on elevation, latitude, and location.The generally strong dependency on elevation is known as altitudinal zonation: the average temperature of a location decreases as the elevation increases.
So can those ending in -ch / -tch (e.g. "the French", "the Dutch") provided they are pronounced with a 'ch' sound (e.g. the adjective Czech does not qualify). Many place-name adjectives and many demonyms are also used for various other things, sometimes with and sometimes without one or more additional words.
The life zone concept was developed by C. Hart Merriam in 1889 as a means of describing areas with similar plant and animal communities. Merriam observed that the changes in these communities with an increase in latitude at a constant elevation are similar to the changes seen with an increase in elevation at a constant latitude.
The two frigid zones, or polar regions, experience the midnight sun and the polar night for part of the year – at the edge of the zone there remains one day, the winter solstice, when the Sun is too low to rise, and one day at the summer solstice when the Sun remains above the horizon for 24 hours.
The climate is characterized by a great seasonal variation in temperatures, four distinct seasons, and a relatively small annual precipitation. [2] continental divide The line of high ground that separates the different oceanic drainage basins of a particular continent. The river systems of a continent on opposite sides of a continental divide ...
Continental climates are considered as temperate climate varieties due to their location in the temperate zones, [2] [3] but are classified separately from other temperate climates in the Köppen climate classification system where they are identified by their first letter, a capital D. In the Trewartha climate classification, they are ...
It’s one reason the global blue zones create the longest-living and healthiest people. After all, they are clusters of people who live, learn, and work alongside each other.
Heating of solids, sunlight and shade in different altitudinal zones (Northern hemisphere) [5] A variety of environmental factors determines the boundaries of altitudinal zones found on mountains, ranging from direct effects of temperature and precipitation to indirect characteristics of the mountain itself, as well as biological interactions of the species.