Imprints of evaporative conditions and vegetation type  in diurnal temperature variations

Panwar, Annu; Renner, Maik; Kleidon, Axel

doi:https://doi.org/10.5194/hess-24-4923-2020

Articles | Volume 24, issue 10

Hydrol. Earth Syst. Sci., 24, 4923–4942, 2020

https://doi.org/10.5194/hess-24-4923-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Hydrol. Earth Syst. Sci., 24, 4923–4942, 2020

https://doi.org/10.5194/hess-24-4923-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 24, issue 10

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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Aug 2020	10	10	2	22
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Nov 2020	76	49	3	128
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Mar 2021	52	9	0	61
Apr 2021	63	10	0	73
May 2021	37	19	2	58
Jun 2021	29	20	3	52
Jul 2021	39	20	0	59
Aug 2021	23	12	0	35
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Dec 2021	36	12	0	48
Jan 2022	40	15	0	55
Feb 2022	37	14	1	52
Mar 2022	27	12	0	39
Apr 2022	18	52	0	70
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Cumulative views and downloads (calculated since 16 Mar 2020)

Month	HTML	PDF	XML	Total
Mar 2020	169	47	2	218
Apr 2020	78	34	1	113
May 2020	33	30	0	63
Jun 2020	40	12	1	53
Jul 2020	24	18	6	48
Aug 2020	10	10	2	22
Sep 2020	21	17	0	38
Oct 2020	332	76	8	416
Nov 2020	76	49	3	128
Dec 2020	45	29	0	74
Jan 2021	57	23	1	81
Feb 2021	47	18	0	65
Mar 2021	52	9	0	61
Apr 2021	63	10	0	73
May 2021	37	19	2	58
Jun 2021	29	20	3	52
Jul 2021	39	20	0	59
Aug 2021	23	12	0	35
Sep 2021	29	9	1	39
Oct 2021	27	40	0	67
Nov 2021	31	28	1	60
Dec 2021	36	12	0	48
Jan 2022	40	15	0	55
Feb 2022	37	14	1	52
Mar 2022	27	12	0	39
Apr 2022	18	52	0	70
May 2022	18	5	1	24
Jun 2022	16	8	2	26

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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.

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