Links between Large-Scale Modes of Climate Variability and Synoptic Weather Patterns in the Southern Indian Ocean

Author:

Udy Danielle G.12,Vance Tessa R.3,Kiem Anthony S.4,Holbrook Neil J.12,Curran Mark A. J.53

Affiliation:

1. a Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Tasmania, Australia

2. b ARC Centre of Excellence for Climate Extremes, University of Tasmania, Hobart, Tasmania, Australia

3. c Australian Antarctic Program Partnership, Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Tasmania, Australia

4. d Centre for Water, Climate and Land, Faculty of Science, University of Newcastle, Callaghan, New South Wales, Australia

5. e Australian Antarctic Division, Kingston, Tasmania, Australia

Abstract

AbstractWeather systems in the southern Indian Ocean (SIO) drive synoptic-scale precipitation variability in East Antarctica and southern Australia. Improved understanding of these dynamical linkages is beneficial to diagnose long-term climate changes from climate proxy records as well as informing regional weather and climate forecasts. Self-organizing maps (SOMs) are used to group daily 500-hPa geopotential height (z500; ERA-Interim) anomalies into nine regional synoptic types based on their dominant patterns over the SIO (30°–75°S, 40°–180°E) from January 1979 to October 2018. The pattern anomalies represented include four meridional, three mixed meridional–zonal, one zonal, and one transitional node. The frequency of the meridional nodes shows limited association with the phase of the southern annular mode (SAM), especially during September–November. The zonal and mixed patterns were nevertheless strongly and significantly correlated with SAM, although the regional synoptic representation of SAM+ conditions was not zonally symmetric and was represented by three separate nodes. We recommend consideration of how different synoptic conditions vary the atmospheric representation of SAM+ in any given season in the SIO. These different types of SAM+ mean a hemispheric index fails to capture the regional variability in surface weather conditions that is primarily driven by the synoptic variability rather than the absolute polarity of the SAM.

Funder

Centre of Excellence for Climate Extremes, Australian Research Council

Australian Research Council Discovery Project

Antarctic Gateway Partnership, Australian Research Council

Antarctic Science Collaboration Initiative

Publisher

American Meteorological Society

Subject

Atmospheric Science

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