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Observational evidence for an inertial oscillation in a particular situation is considered at Auckland, New Zealand. Cyclogenesis occurred in the Tasman Sea during the period, a low-level jet strengthened at Auckland, and the oscillation was detectable over a wide region of the South Pacific. The possible mechanisms of Blackadar and Uccellini are discussed in relation to the evidence.
Observational evidence for an inertial oscillation in a particular situation is considered at Auckland, New Zealand. Cyclogenesis occurred in the Tasman Sea during the period, a low-level jet strengthened at Auckland, and the oscillation was detectable over a wide region of the South Pacific. The possible mechanisms of Blackadar and Uccellini are discussed in relation to the evidence.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 68 | 28 | 4 |
| PDF Downloads | 20 | 14 | 1 |
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