Shengyi Qian, Haibo Hu, Kevin I. Hodges, Yimin Zhu, Xiu-Qun Yang, Yuanheng Wang
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引用次数: 0
Abstract
This study investigates that the concurrent influence of El Niño-Southern Oscillation (ENSO) on the Arctic Oscillation (AO) mediated through the poleward translation of extra-tropical cyclones (ECs) over the North Atlantic is more significant than the one-year-lagged impact of ENSO through poleward propagating atmospheric angular momentum. Specific results show that during El Niño (La Niña) winter, the anomalous atmospheric horizontal heat advection from the Pacific to the Atlantic, which is caused by the southward (northward) displacement of the westerly jet stream, enhances (weakens) the atmospheric baroclinicity over the subtropical North Atlantic. Subsequently, the changed baroclinicity drives intensified (reduced) baroclinic energy conversion from the eddy available potential energy to the eddy kinetic energy, which shifts the genesis locations of ECs southward (northward) and suppresses (enhances) their poleward translation into the Arctic. Ultimately, through the combined thermodynamic and dynamical forcing associated with EC activity, the negative (positive) AO pattern is generated in the concurrent winter.
期刊介绍:
Geophysical Research Letters (GRL) publishes high-impact, innovative, and timely research on major scientific advances in all the major geoscience disciplines. Papers are communications-length articles and should have broad and immediate implications in their discipline or across the geosciences. GRLmaintains the fastest turn-around of all high-impact publications in the geosciences and works closely with authors to ensure broad visibility of top papers.