contributor author | Pepler, A. | |
contributor author | Timbal, B. | |
contributor author | Rakich, C. | |
contributor author | Coutts-Smith, A. | |
date accessioned | 2017-06-09T17:09:23Z | |
date available | 2017-06-09T17:09:23Z | |
date copyright | 2014/05/01 | |
date issued | 2014 | |
identifier issn | 0894-8755 | |
identifier other | ams-80259.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4223131 | |
description abstract | he strong relationship between eastern Australian winter?spring rainfall and tropical modes of variability such as the El Niño?Southern Oscillation (ENSO) does not extend to the heavily populated coastal strip east of the Great Dividing Range in southeast Australia, where correlations between rainfall and Niño-3.4 are insignificant during June?October. The Indian Ocean dipole (IOD) is found to have a strong influence on zonal wind flow during the winter and spring months, with positive IOD increasing both onshore winds and rainfall over the coastal strip, while decreasing rainfall elsewhere in southeast Australia. The IOD thus opposes the influence of ENSO over the coastal strip, and this is shown to be the primary cause of the breakdown of the ENSO?rainfall relationship in this region. | |
publisher | American Meteorological Society | |
title | Indian Ocean Dipole Overrides ENSO’s Influence on Cool Season Rainfall across the Eastern Seaboard of Australia | |
type | Journal Paper | |
journal volume | 27 | |
journal issue | 10 | |
journal title | Journal of Climate | |
identifier doi | 10.1175/JCLI-D-13-00554.1 | |
journal fristpage | 3816 | |
journal lastpage | 3826 | |
tree | Journal of Climate:;2014:;volume( 027 ):;issue: 010 | |
contenttype | Fulltext | |