Increasing tropical cyclone intensity and potential intensity in the subtropical Atlantic around Bermuda from an ocean heat content perspective 1955- 2019
Hallam, Samantha; Guishard, Mark; Josey, Simon A. ORCID: https://orcid.org/0000-0002-1683-8831; Hyder, Pat; Hirschi, Joel J.-M.. 2021 Increasing tropical cyclone intensity and potential intensity in the subtropical Atlantic around Bermuda from an ocean heat content perspective 1955- 2019. Environmental Research Letters, 16 (3), 034052. https://doi.org/10.1088/1748-9326/abe493
Before downloading, please read NORA policies.
|
Text
Hallam+et+al_2021_Environ._Res._Lett._10.1088_1748-9326_abe493.pdf - Accepted Version Available under License Creative Commons Attribution. Download (8MB) | Preview |
|
|
Text
Hallam_2021_Environ._Res._Lett._16_034052.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (5MB) | Preview |
Abstract/Summary
We investigate tropical cyclone (TC) activity and intensity within a 100km radius of Bermuda between 1955 and 2019. The results show a more easterly genesis over time and significant increasing trends in tropical cyclone intensity (maximum wind speed (Vmax)) with a decadal Vmax median value increase of 30kts from 33 to 63kts (r=0.94, p=0.02), together with significant increasing August, September, October (ASO) sea surface temperature (SST) of 1.1°C (0.17°C per decade) r= 0.4 (p<0.01) and increasing average ocean temperature between 0.5–0.7°C (0.08-0.1°C per decade) r=0.3(p<0.01) in the depth range 0-300m. The strongest correlation is found between TC intensity and ocean temperature averaged through the top 50m ocean layer (T50m ) r=0.37 (p<0.01). We show how tropical cyclone potential intensity estimates are closer to actual intensity by using T50m as opposed to SST using the Bermuda Atlantic Timeseries Hydrostation S dataset. We modify the widely used sea surface temperature potential intensity index by using T50m to provide a closer estimate of the observed minimum sea level pressure (MSLP), and associated Vmax than by using SST, creating a T50m potential intensity (T50m_PI) index. The average MSLP difference is reduced by 12mb and proportional (r=0.74, p<0.01) to the SST/(T50m ) 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.
Item Type: | Publication - Article |
---|---|
Digital Object Identifier (DOI): | https://doi.org/10.1088/1748-9326/abe493 |
ISSN: | 1748-9326 |
Date made live: | 01 Mar 2021 14:04 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/529771 |
Actions (login required)
View Item |
Document Downloads
Downloads for past 30 days
Downloads per month over past year