Late Holocene temperature variability in Tasmania inferred from borehole temperature data

Suman, Asadusjjaman; Dyer, Fiona; White, Duanne

doi:https://doi.org/10.5194/cp-13-559-2017

Articles | Volume 13, issue 6

https://doi.org/10.5194/cp-13-559-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue:

Southern perspectives on climate and the environment from...

https://doi.org/10.5194/cp-13-559-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 13, issue 6

Research article

|

02 Jun 2017

Research article |

| 02 Jun 2017

Late Holocene temperature variability in Tasmania inferred from borehole temperature data

Asadusjjaman Suman, Fiona Dyer, and Duanne White

Download

Final revised paper (published on 02 Jun 2017)
Supplement to the final revised paper
Preprint (discussion started on 15 Dec 2016)
Supplement to the preprint

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

- Printer-friendly version

- Supplement

RC1: 'Review of Suman et al', Anonymous Referee #1, 10 Jan 2017
RC2: 'Review of Suman et al.', Anonymous Referee #2, 12 Jan 2017
AC1: 'Response to the reviewers comments', Asadusjjaman Suman, 15 Mar 2017

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish as is (25 Apr 2017) by Andrew Lorrey

Short summary

Thirty-six borehole temperature–depth profiles were analysed to reconstruct the ground surface temperature history (GSTH) of eastern Tasmania for the past 5 centuries. Temperature changes were greatest around the north-east coast and decreased towards midland Tasmania. Average GSTH reconstructed from Tasmanian boreholes shows temperature increases of about 1.2 ± 0.2 °C during the past 5 centuries.