Articles | Volume 18, issue 5
https://doi.org/10.5194/bg-18-1577-2021
https://doi.org/10.5194/bg-18-1577-2021
Research article
 | 
04 Mar 2021
Research article |  | 04 Mar 2021

Microclimatic comparison of lichen heaths and shrubs: shrubification generates atmospheric heating but subsurface cooling during the growing season

Peter Aartsma, Johan Asplund, Arvid Odland, Stefanie Reinhardt, and Hans Renssen

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (19 Dec 2020) by Paul Stoy
AR by Peter Aartsma on behalf of the Authors (06 Jan 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (07 Jan 2021) by Paul Stoy
RR by Anonymous Referee #1 (21 Jan 2021)
RR by Anonymous Referee #2 (25 Jan 2021)
ED: Publish subject to technical corrections (25 Jan 2021) by Paul Stoy
AR by Peter Aartsma on behalf of the Authors (28 Jan 2021)  Author's response    Manuscript
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Short summary
In the literature, it is generally assumed that alpine lichen heaths keep their direct environment cool due to their relatively high albedo. However, we reveal that the soil temperature and soil heat flux are higher below lichens than below shrubs during the growing season, despite a lower net radiation for lichens. We also show that the differences in microclimatic conditions between these two vegetation types are more pronounced during warm and sunny days than during cold and cloudy days.
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