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Tropical cyclone contribution to extreme rainfall over southwest Pacific Island nations

Citation

Deo, A and Chand, SS and Ramsay, H and Holbrook, NJ and McGree, S and Magee, A and Bell, S and Titimaea, M and Haruhiru, A and Malsale, P and Mulitalo, S and Daphne, A and Prakash, B and Vainikolo, V and Koshiba, S, Tropical cyclone contribution to extreme rainfall over southwest Pacific Island nations, Climate Dynamics, 56 pp. 3967-3993. ISSN 0930-7575 (2021) [Refereed Article]


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Copyright 2020 The Authors. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made.

DOI: doi:10.1007/s00382-021-05680-5

Abstract

Southwest Pacific nations are among some of the worst impacted and most vulnerable globally in terms of tropical cyclone (TC)-induced flooding and accompanying risks. This study objectively quantifies the fractional contribution of TCs to extreme rainfall (hereafter, TC contributions) in the context of climate variability and change. We show that TC contributions to extreme rainfall are substantially enhanced during active phases of the Madden–Julian Oscillation and by El Niño conditions (particularly over the eastern southwest Pacific region); this enhancement is primarily attributed to increased TC activity during these event periods. There are also indications of increasing intensities of TC-induced extreme rainfall events over the past few decades. A key part of this work involves development of sophisticated Bayesian regression models for individual island nations in order to better understand the synergistic relationships between TC-induced extreme rainfall and combinations of various climatic drivers that modulate the relationship. Such models are found to be very useful for not only assessing probabilities of TC- and non-TC induced extreme rainfall events but also evaluating probabilities of extreme rainfall for cases with different underlying climatic conditions. For example, TC-induced extreme rainfall probability over Samoa can vary from ~ 95 to ~ 75% during a La Niña period, if it coincides with an active or inactive phase of the MJO, and can be reduced to ~ 30% during a combination of El Niño period and inactive phase of the MJO. Several other such cases have been assessed for different island nations, providing information that have potentially important implications for planning and preparing for TC risks in vulnerable Pacific Island nations.

Item Details

Item Type:Refereed Article
Keywords:tropical cyclone, extreme rainfall, southwest Pacific Island nations, Madden Julian oscillation, El Nino Southern oscillation
Research Division:Earth Sciences
Research Group:Oceanography
Research Field:Physical oceanography
Objective Division:Environmental Policy, Climate Change and Natural Hazards
Objective Group:Natural hazards
Objective Field:Climatological hazards (e.g. extreme temperatures, drought and wildfires)
UTAS Author:Holbrook, NJ (Professor Neil Holbrook)
ID Code:143574
Year Published:2021
Web of Science® Times Cited:1
Deposited By:Oceans and Cryosphere
Deposited On:2021-03-24
Last Modified:2021-10-11
Downloads:4 View Download Statistics

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