Discussion
Which quantity does the Madden-Julian Oscillation index often use?
Answer: C
The eastward propagating envelope of enhanced and suppressed convection that constitutes the oscillation is most clearly seen in upper level velocity potential, which responds directly to the divergent circulation above the convection. Sea surface temperature indices and the Darwin Tahiti pressure difference measure the El Nino Southern Oscillation instead, on a much longer timescale.
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