The Bjerkens mechanism was proposed to explain this phenomenon, which causes the rising branch of the Walker circulation(*) to shift eastward.
The Bjerkens mechanism was proposed to explain this phenomenon, which causes the rising branch of the Walker circulation(*) to shift eastward. An index monitoring this phenomenon and its partner is based on measurements of the sea level pressure anomaly at Tahiti and Darwin. The warm phase of the Southern Oscillation, for ten points, identify this 12 to 18 month long warming of the central and easter Pacific Ocean.
The Bjerkens mechanism was proposed to explain this phenomenon, which causes the rising branch of the Walker circulation(*) to shift eastward.
El Nino