Articles | Volume 24, issue 10
Hydrol. Earth Syst. Sci., 24, 4923–4942, 2020
https://doi.org/10.5194/hess-24-4923-2020
Hydrol. Earth Syst. Sci., 24, 4923–4942, 2020
https://doi.org/10.5194/hess-24-4923-2020

Research article 20 Oct 2020

Research article | 20 Oct 2020

Imprints of evaporative conditions and vegetation type in diurnal temperature variations

Annu Panwar et al.

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ED: Publish subject to revisions (further review by editor and referees) (21 Jun 2020) by Dominic Mazvimavi
AR by Annu Panwar on behalf of the Authors (30 Jul 2020)  Author's response    Manuscript
ED: Publish as is (03 Sep 2020) by Dominic Mazvimavi
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Short summary
Here we examine the effect of evaporative cooling across different vegetation types. Evaporation cools surface temperature significantly in short vegetation. In the forest, the high aerodynamic conductance explains 56 % of the reduced surface temperature. Therefore, the main cooling agent in the forest is the high aerodynamic conductance and not evaporation. Additionally, we propose the diurnal variation in surface temperature as being a potential indicator of evaporation in short vegetation.