3.1.2.2, 3.1.2.3 - Episodic water and arid landforms
Explain how infrequent but energetic flows connect desert uplands to basin floors and distinguish depositional fans from erosional surfaces and residual hills.
Source, destination and duration of flow
Exogenous rivers receive much of their water from outside the desert, for example wetter headwaters, and can continue flowing through an arid region. Endoreic drainage, the specification's term commonly written endorheic, drains into an inland basin without a surface outlet to the sea. Water may infiltrate or evaporate from a terminal lake or playa. Ephemeral channels flow briefly in response to rainfall and are dry much of the time.
These categories describe different attributes. A river can receive external water and terminate in a closed basin; an ephemeral stream can also feed that basin. 'Exogenous', 'closed-basin' and 'ephemeral' are therefore not three mutually exclusive river sizes. Flow also varies seasonally and with water abstraction.
Episodic runoff and wadis
Short intense rain can exceed infiltration, especially on bare, crusted or rocky surfaces. Water first moves as relatively unconfined sheet flow, which can strip fine material, then concentrates into channels. A rapid rise in discharge creates a flash flood with enough energy to erode banks, entrain coarse debris and transport sediment. Rain upstream can flood a channel where no rain is falling locally; low annual rainfall does not mean low flood danger.
A wadi is a normally dry valley or channel shaped by intermittent flows. Weathering and slope failures supply debris to it between floods. During flow, channel gradient, roughness, water volume and load affect erosion and deposition. When water infiltrates into an alluvial bed, discharge can decline downstream; both loss of flow and reduced gradient favour sediment deposition.
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