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Modulation of western North Pacific tropical cyclone activity by the Atlantic Meridional Mode
Journal article   Peer reviewed

Modulation of western North Pacific tropical cyclone activity by the Atlantic Meridional Mode

Wei Zhang, Gabriel Vecchi, Gabriele Villarini, Hiroyuki Murakami, Anthony Rosati, Xiaosong Yang, Liwei Jia and Fanrong Zeng
Climate dynamics, Vol.48(1), pp.631-647
01/2017
DOI: 10.1007/s00382-016-3099-2
url
https://repository.library.noaa.gov/view/noaa/66092/noaa_66092_DS1.pdfView
Open Access

Abstract

This study examines the year-to-year modulation of the western North Pacific (WNP) tropical cyclones (TC) activity by the Atlantic Meridional Mode (AMM) using both observations and the Geophysical Fluid Dynamics Laboratory Forecast-oriented Low Ocean Resolution Version of CM2.5 (FLOR) global coupled model. 1. The positive (negative) AMM phase suppresses (enhances) WNP TC activity in observations. The anomalous occurrence of WNP TCs results mainly from changes in TC genesis in the southeastern part of the WNP. 2. The observed responses of WNP TC activity to the AMM are connected to the anomalous zonal vertical wind shear (ZVWS) caused by AMM-induced changes to the Walker circulation. During the positive AMM phase, the warming in the North Atlantic induces strong descending flow in the tropical eastern and central Pacific, which intensifies the Walker cell in the WNP. The intensified Walker cell is responsible for the suppressed (enhanced) TC genesis in the eastern (western) part of the WNP by strengthening (weakening) ZVWS. 3. The observed WNPTC–AMM linkage is examined by the long-term control and idealized perturbations experiment with FLOR-FA. A suite of sensitivity experiments strongly corroborate the observed WNPTC–AMM linkage and underlying physical mechanisms.
Atlantic Meridional Mode Climatology Earth Sciences Geophysics/Geodesy Oceanography Tropical cyclone Western North Pacific

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