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Which mechanism causes variations in Great Salt Lake brine streamflow due to atmospheric dynamics?

A)Localized precipitation intensity variation
B)Geothermal heating altering algal growth
C)Tectonic activity increasing stream bed slope
D)Salt precipitation altering channel roughness

💡 Explanation

When atmospheric circulation patterns shift, localized precipitation changes ensue because of altered moisture transport leading to variations in streamflow into the Great Salt Lake. Therefore localized precipitation is key, rather than geothermal heating,tectonics or salt precipiation, which don't have link to atmospheric dynamics.

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