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Which outcome occurs when prolonged atmospheric blocking disrupts zonal wind streams?

A)Intensified coastal upwelling
B)Amplified jet stream meandering
C)Increased stratospheric ozone depletion
D)Decreased thermohaline circulation

💡 Explanation

Jet stream meandering is amplified because Rossby waves, established via baroclinic instability, grow larger with stalled zonal flow. Stronger meanders cause extreme weather rather than predictable upwelling. Therefore, option B is best, rather than alternatives affecting ocean currents or the stratosphere.

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