Increasing tropical cyclone intensity and potential intensity in the subtropical Atlantic around Bermuda from an ocean heat content perspective 1955-2019

被引:14
|
作者
Hallam, Samantha [1 ,2 ]
Guishard, Mark [3 ,4 ]
Josey, Simon A. [1 ]
Hyder, Pat [5 ]
Hirschi, Joel [1 ]
机构
[1] Natl Oceanog Ctr, European Way, Southampton SO14 3ZH, Hants, England
[2] Univ Southampton, Natl Oceanog Ctr, European Way, Southampton SO14 3ZH, Hants, England
[3] Bermuda Inst Ocean Sci, 17 Biol Stn, St Georges GE 01, Bermuda
[4] Bermuda Airport Author, Bermuda Weather Serv, St Georges DD03, Bermuda
[5] Met Off, Fitzroy Rd, Exeter EX1 3PB, Devon, England
关键词
tropical cyclone; ocean heat content; subtropical Atlantic; Bermuda; potential intensity; Hydrostation S time-series;
D O I
10.1088/1748-9326/abe493
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We investigate tropical cyclone (TC) activity and intensity within a 100 km radius of Bermuda between 1955 and 2019. The results show a more easterly genesis over time and significant increasing trends in TC intensity (maximum wind speed (Vmax)) with a decadal Vmax median value increase of 30 kts from 33 to 63 kts (r = 0.94, p = 0.02), together with significant increasing August, September, October sea surface temperature (SST) of 1.1 degrees C (0.17 degrees C per decade) r = 0.4 (p < 0.01) and increasing average ocean temperature between 0.5 degrees C and 0.7 degrees C (0.08 degrees C-0.1 degrees C per decade) r = 0.3(p < 0.01) in the depth range 0-300 m. The strongest correlation is found between TC intensity and ocean temperature averaged through the top 50 m ocean layer ((T-50 m) over bar) r = 0.37 (p < 0.01). We show how TC potential intensity (PI) estimates are closer to actual intensity by using <(T-50 m)over bar> as opposed to SST using the Hydrostation S time-series. We modify the widely used SST PI index by using (T-50 m) over bar to provide a closer estimate of the observed minimum sea level pressure (MSLP), and associated Vmax than by using SST, creating a (T-50 m) over bar PI ((T-50 m) over bar _PI) index. The average MSLP difference is reduced by 12 mb and proportional (r = 0.74, p < 0.01) to the SST/<(T-50 m)over bar> temperature difference. We also suggest the index could be used over a wider area of the subtropical/tropical Atlantic where there is a shallow mixed layer depth.
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页数:10
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