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The island generates wave motion in the wind passing over it, creating regularly spaced orographic clouds. The wave crests raise and cool the air to form clouds, while the troughs remain too low for cloud formation. Note that while the wave motion is generated by orographic lift, it is not required. In other words, one cloud often forms at the ...
An orographic map of Eastern Siberia from 1875 by Peter Kropotkin. Orography is the study of the topographic relief of mountains, [1] and can more broadly include hills, and any part of a region's elevated terrain. [2] Orography (also known as oreography, orology, or oreology) falls within the broader discipline of geomorphology. [3]
Marketing strategy refers to efforts undertaken by an organization to increase its sales and achieve competitive advantage. [1] In other words, it is the method of advertising a company's products to the public through an established plan through the meticulous planning and organization of ideas, data, and information.
Tectonic–climatic interaction is the interrelationship between tectonic processes and the climate system. The tectonic processes in question include orogenesis, volcanism, and erosion, while relevant climatic processes include atmospheric circulation, orographic lift, monsoon circulation and the rain shadow effect.
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Therefore, keeping tabs on industry competitors is vital for devising robust marketing plans. Marketing Strategy: Improving marketing effectiveness can be achieved by employing a superior marketing strategy. By positioning the product or brand correctly, the product/brand will be more successful in the market than competitors’ products/brands.
Marketing exposure is a major part that determines a company's success in their market. Although it is never directly identified or defined, it crucial for helping a company progress, creating competition for other companies, making the company more credible with consumers, and overall benefit both the company while satisfying consumers. [2]
Orographic or relief rainfall is caused when masses of air are forced up the side of elevated land formations, such as large mountains or plateaus (often referred to as an upslope effect). The lift of the air up the side of the mountain results in adiabatic cooling with altitude, and ultimately condensation and precipitation.