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Altitudinal zonation (or elevational zonation [1]) in mountainous regions describes the natural layering of ecosystems that occurs at distinct elevations due to varying environmental conditions. Temperature , humidity , soil composition, and solar radiation are important factors in determining altitudinal zones, which consequently support ...
Because of the altitudinal variation of the Mandakini (altitude ranging from 210 to 7,187 m [689 to 23,579 ft] a.s.l), climate conditions vary throughout the region. [ citation needed ] A general increase in temperatures, which scientists from the Department of Water Resources Development and Management, Indian Institute of Technology, Roorkee ...
Also amphidrome and tidal node. A geographical location where there is little or no tide, i.e. where the tidal amplitude is zero or nearly zero because the height of sea level does not change appreciably over time (meaning there is no high tide or low tide), and around which a tidal crest circulates once per tidal period (approximately every 12 hours). Tidal amplitude increases, though not ...
Hinglish (the name is a combination of the words "Hindi" and "English") is a macaronic language, a hybrid of British English and South Asian languages – it is a code-switching variety of these languages whereby they are freely interchanged within a sentence or between sentences.
Located in the Hindi Belt, the Central Zone includes the Dehlavi (Delhi) dialect (one of several called 'Khariboli') of the Hindustani language, the lingua franca of Northern India that is the basis of the Modern Standard Hindi and Standard Urdu literary standards. In regards to the Indo-Aryan language family, the coherence of this language ...
The variation in temperature that occurs from the highs of the day to the cool of nights is called diurnal temperature variation. Temperature ranges can also be based on periods of a month or a year. The size of ground-level atmospheric temperature ranges depends on several factors, such as: Average air temperature; Average humidity
The first recorded observation of the elevational diversity gradient was by Carl Linnaeus in his treatise On the growth of the habitable Earth.In this document, Linnaeus based his predictions on flood geology, assuming most of the world was at one point inundated, leaving only the highest elevations available for terrestrial life.
Countergradient variation, originally termed "contra-gradient variation", was coined by Richard Levins in his 1968 book Evolution in Changing Environments. [2] Levins first used the term when describing patterns of body size across an altitudinal gradient in populations of Drosophila , [ 4 ] and since then many other instances of ...