Search from over 60,000 research works

Advanced Search

Extreme rainfall variability in Australia: Patterns, drivers and predictability

[thumbnail of PDF of accepted version of manuscript, after peer review]
Preview
king_et_al_2014_eots.pdf - Accepted Version (1MB) | Preview
[thumbnail of jcli-d-13-00715%2E1.pdf]
Preview
jcli-d-13-00715%2E1.pdf - Published Version (5MB) | Preview
Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

King, A. D., Klingaman, N. P. orcid id iconORCID: https://orcid.org/0000-0002-2927-9303, Alexander, L. V., Donat, M. G., Jourdain, N. C. and Maher, P. (2014) Extreme rainfall variability in Australia: Patterns, drivers and predictability. Journal of Climate, 27 (15). pp. 6035-6050. ISSN 1520-0442 doi: 10.1175/JCLI-D-13-00715.1

Abstract/Summary

Leading patterns of observed monthly extreme rainfall variability in Australia are examined using an Empirical Orthogonal Teleconnection (EOT) method. Extreme rainfall variability is more closely related to mean rainfall variability during austral summer than in winter. The leading EOT patterns of extreme rainfall explain less variance in Australia-wide extreme rainfall than is the case for mean rainfall EOTs. We illustrate that, as with mean rainfall, the El Niño-Southern Oscillation (ENSO) has the strongest association with warm-season extreme rainfall variability, while in the cool-season the primary drivers are atmospheric blocking and the subtropical ridge. The Indian Ocean Dipole and Southern Annular Mode also have significant relationships with patterns of variability during austral winter and spring. Leading patterns of summer extreme rainfall variability have predictability several months ahead from Pacific sea surface temperatures (SSTs) and as much as a year in advance from Indian Ocean SSTs. Predictability from the Pacific is greater for wetter than average summer months than for months that are drier than average, whereas for the Indian Ocean the relationship has greater linearity. Several cool-season EOTs are associated with mid-latitude synoptic-scale patterns along the south and east coasts. These patterns have common atmospheric signatures denoting moist onshore flow and strong cyclonic anomalies often to the north of a blocking anti-cyclone. Tropical cyclone activity is observed to have significant relationships with some warm season EOTs. This analysis shows that extreme rainfall variability in Australia can be related to remote drivers and local synoptic-scale patterns throughout the year.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/36608
Item Type Article
Refereed Yes
Divisions Interdisciplinary Research Centres (IDRCs) > Walker Institute
Science > School of Mathematical, Physical and Computational Sciences > NCAS
Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Publisher American Meteorological Society
Download/View statistics View download statistics for this item

Downloads

Downloads per month over past year

University Staff: Request a correction | Centaur Editors: Update this record

Search Google Scholar