On the relationship between Indian Ocean sea surface temperature variability and tropical cyclogenesis in the southwest Pacific

被引:18
|
作者
Magee, Andrew D. [1 ]
Verdon-Kidd, Danielle C. [1 ]
机构
[1] Univ Newcastle, Sch Environm & Life Sci, ECCRG, Fac Sci, Earth Sci Bldg,Univ Dr, Callaghan, NSW 2308, Australia
关键词
Climate < 2. Scale; Severe weather < 3. Physical phenomenon; ENSO; Tropical Cyclone; Climate Variability; Indian Ocean SST variability; Southwest Pacific; Tropical Cyclogenesis; MULTIDECADAL VARIABILITY; CYCLONE CLIMATOLOGY; AUSTRALIAN REGION; ISLAND COUNTRIES; ENSO; OSCILLATION; FIJI; SST; INTENSITY; RAINFALL;
D O I
10.1002/joc.5406
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In the southwest Pacific (SWP) tropical cyclones (TCs) account for 76% of the regions natural disasters and have substantial economic, physical and environmental impacts on people and places. Therefore, information is needed to better understand when and where TCs are likely to occur, as this can aid in preparedness and planning. While there is a well-established relationship between Pacific Ocean sea surface temperature (SST) variability and tropical cyclogenesis (TC genesis) in the SWP, it does not fully explain the historical spatial and temporal variability observed. Therefore, this study aims to look beyond the Pacific and establish a new relationship between Indian Ocean SST variability and SWP TC genesis. This is achieved by statistically relating indices of Indian Ocean SST variability to SWP TC genesis positions. The physical mechanisms driving these observed relationships are then established by studying changes in the environmental conditions conducive to TC genesis. This analysis shows that Indian Ocean SST variability significantly modulates the clustering of SWP TC genesis, where warmer (cooler) SSTs in the eastern and western regions of the Indian Ocean result in a statistically significant north/east (south/west) migration of TC genesis by up to 950 km. Importantly, this relationship is shown to be consistent when the El Nino/Southern Oscillation (ENSO, the dominant Pacific mode) is in an inactive phase (ENSO neutral). Favourable TC genesis parameters including warm SSTs, increased relative humidity, anomalously negative 700 hPa vorticity, anomalously negative and low absolute 200-850 hPa vertical wind shear account for the observed shift in clustering. Furthermore, we show that the combined effect of ENSO/Indian Ocean SST variability results in varying risk profiles for island nations of the region, with the two climate modes either enhancing or suppressing individual impacts. Significantly, the findings from this study provide an opportunity for meteorological agencies to improve seasonal SWP TC outlooks.
引用
收藏
页码:E774 / E795
页数:22
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