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Area of occurrence: North America (particularly in central and southeastern regions of the United States colloquially known as Tornado Alley), South Africa, much of Europe (except most of the Alps), western and eastern Australia, New Zealand, Bangladesh and adjacent eastern India, Japan, the Philippines, and southeastern South America (Uruguay and Argentina)
Water tends to be stagnant or may flow slowly on a seasonal basis. [5] In North America, "slough" may refer to a side-channel from or feeding a river, or an inlet or natural channel only sporadically filled with water. [3] An example of this is Finn Slough on the Fraser River, whose lower reaches have dozens of notable sloughs.
A whirlwind A dust devil at school ground Whirlwind, 61 km northeast of Broome, Western Australia. A whirlwind is a phenomenon in which a vortex of wind (a vertically oriented rotating column of air) forms due to instabilities and turbulence created by heating and flow gradients.
Interfluve – Land between two converging, or confluent, rivers, mainly in the Punjab; Inverted relief – Landscape features that have reversed their elevation relative to other features; Island – Piece of subcontinental land completely surrounded by water; Islet – Very small island
A whirlpool is a body of rotating water produced by opposing currents or a current running into an obstacle. [1] [clarification needed] Small whirlpools form when a bath or a sink is draining. More powerful ones formed in seas or oceans may be called maelstroms (/ ˈ m eɪ l s t r ɒ m,-r ə m / MAYL-strom, -strəm).
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Oceanic eddies are also usually made of water masses that are different from those outside the eddy. That is, the water within an eddy usually has different temperature and salinity characteristics to the water outside the eddy. There is a direct link between the water mass properties of an eddy and its rotation.
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