Surface energy budget responses to radiative forcing at Summit, Greenland

Miller, Nathaniel B.; Shupe, Matthew D.; Cox, Christopher J.; Noone, David; Persson, P. Ola G.; Steffen, Konrad

doi:https://doi.org/10.5194/tc-11-497-2017

Articles | Volume 11, issue 1

https://doi.org/10.5194/tc-11-497-2017

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

https://doi.org/10.5194/tc-11-497-2017

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

Articles | Volume 11, issue 1

Research article

|

13 Feb 2017

Research article |

| 13 Feb 2017

Surface energy budget responses to radiative forcing at Summit, Greenland

Nathaniel B. Miller, Matthew D. Shupe, Christopher J. Cox, David Noone, P. Ola G. Persson, and Konrad Steffen

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Final revised paper (published on 13 Feb 2017)
Preprint (discussion started on 23 Sep 2016)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Review', Peter Kuipers Munneke, 03 Nov 2016
- AC1: 'Response to Dr. Kuipers Munneke (Referee 1)', Nathaniel Miller, 17 Dec 2016
RC2: 'Review', Anonymous Referee #2, 21 Nov 2016
- AC2: 'Response to Referee 2', Nathaniel Miller, 17 Dec 2016

Peer-review completion

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

AR by Nathaniel Miller on behalf of the Authors (17 Dec 2016) Author's response Manuscript

ED: Reconsider after major revisions (21 Dec 2016) by Xavier Fettweis

AR by Nathaniel Miller on behalf of the Authors (22 Dec 2016) Author's response Manuscript

ED: Publish as is (02 Jan 2017) by Xavier Fettweis

ED: Referee Nomination & Report Request started (02 Jan 2017) by Xavier Fettweis

RR by Peter Kuipers Munneke (04 Jan 2017)

ED: Publish as is (19 Jan 2017) by Xavier Fettweis

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Short summary

A comprehensive observational dataset is assembled to investigate atmosphere–Greenland ice sheet interactions and characterize surface temperature variability. The amount the surface temperature warms, due to increases in cloud presence and/or elevated sun angle, varies throughout the annual cycle and is modulated by the responses of latent, sensible and ground heat fluxes. This observationally based study provides process-based relationships, which are useful for evaluation of climate models.