Articles | Volume 15, issue 4
Research article
13 Apr 2021
Research article |  | 13 Apr 2021

Impact of updated radiative transfer scheme in snow and ice in RACMO2.3p3 on the surface mass and energy budget of the Greenland ice sheet

Christiaan T. van Dalum, Willem Jan van de Berg, and Michiel R. van den Broeke


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (04 Feb 2021) by Masashi Niwano
AR by Christiaan van Dalum on behalf of the Authors (04 Feb 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (05 Feb 2021) by Masashi Niwano
RR by Anonymous Referee #2 (15 Feb 2021)
RR by Anonymous Referee #1 (01 Mar 2021)
ED: Publish as is (02 Mar 2021) by Masashi Niwano
Short summary
Absorption of solar radiation is often limited to the surface in regional climate models. Therefore, we have implemented a new radiative transfer scheme in the model RACMO2, which allows for internal heating and improves the surface reflectivity. Here, we evaluate its impact on the surface mass and energy budget and (sub)surface temperature, by using observations and the previous model version for the Greenland ice sheet. New results match better with observations and introduce subsurface melt.