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- W1726579774 abstract "Publisher Summary This chapter discusses the topography of the Great Grand Sea. The Great Sand Sea consists of three units or landform generations in a vertical succession. These generations influence each other—the influence of the lower/older unit on the upper/younger being greater. The chapter also reviews the megadunes in the Great Sand Sea. The megadunes or draa are distinguished from the dunes by their dimensions and, particularly, by their wavelengths (>1 km). While dunes are formed by surface winds only, the entire planetary boundary layer of the atmosphere is involved in the modeling of draa, which explains their greater dimensions. Because of the completely different aeolian dynamics, dunes and draa are studied separately. Draa are found in all sand seas of the world and are of Pleistocene origin. They are distinguished from dunes by their larger dimensions (especially length and spacing)." @default.
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- W1726579774 date "2008-01-01" @default.
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- W1726579774 title "Chapter Three: Topography of the Great Sand Sea" @default.
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- W1726579774 doi "https://doi.org/10.1016/s0070-4571(07)10004-2" @default.
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