Articles | Volume 9, issue 4
https://doi.org/10.5194/cp-9-1807-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.Special issue:
A model–data comparison of the Holocene global sea surface temperature evolution
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- Final revised paper (published on 06 Aug 2013)
- Supplement to the final revised paper
- Preprint (discussion started on 29 Mar 2012)
Interactive discussion
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
- Printer-friendly version
- Supplement
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SC C273: 'Paper addresses a question that is not a scientific question', Terry Oldberg, 16 Apr 2012
- AC C343: 'clarification', Gerrit Lohmann, 04 May 2012
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SC C320: 'Why is there no discussion of a higher radiative forcing value for insolation?', Sebastian Luening, 27 Apr 2012
- AC C379: 'no evidence for "a higher radiative forcing for insolation also means a higher radiative forcing for solar activity"', Gerrit Lohmann, 11 May 2012
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RC C447: 'Review', Anonymous Referee #1, 25 May 2012
- AC C2952: 'reply to referee #1', Gerrit Lohmann, 24 Dec 2012
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SC C710: 'All models mismatch Holocene proxies', Joachim Seifert, 29 Jun 2012
- SC C711: 'Holocene sea surface temperature trends', Gerrit Lohmann, 29 Jun 2012
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RC C1750: 'Review of “A model-data comparison of the Holocene global sea surface temperature evolution”, CPD-8-1005-2012', Anonymous Referee #2, 28 Sep 2012
- AC C2958: 'reply to referee #2', Gerrit Lohmann, 24 Dec 2012