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HESS | Articles | Volume 24, issue 3
Hydrol. Earth Syst. Sci., 24, 1055–1072, 2020
https://doi.org/10.5194/hess-24-1055-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Hydrol. Earth Syst. Sci., 24, 1055–1072, 2020
https://doi.org/10.5194/hess-24-1055-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 04 Mar 2020

Research article | 04 Mar 2020

Evaporation from a large lowland reservoir – (dis)agreement between evaporation models from hourly to decadal timescales

Femke A. Jansen and Adriaan J. Teuling

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Cited articles

Aalbers, E. E., Lenderink, G., van Meijgaard, E., and van den Hurk, B. J. J. M.: Local-Scale Changes in Mean and Heavy Precipitation in Western Europe, Climate Change or Internal Variability?, Clim. Dynam., 50, 4745–4766, https://doi.org/10.1007/s00382-017-3901-9, 2017. a
Abdelrady, A. R., Timmermans, J., Vekerdy, Z., and Salama, M. S.: Surface Energy Balance of Fresh and Saline Waters: AquaSEBS, Remote Sens., 8, 583, https://doi.org/10.3390/rs8070583, 2016. a
Abtew, W. and Melesse, A. M.: Evaporation and Evapotranspiration: Measurements and Estimations, Springer Netherlands, 2013. a
Arnell, N. W.: Climate Change and Global Water Resources, Global Environ. Change, 9, S31–S49, https://doi.org/10.1016/S0959-3780(99)00017-5, 1999. a
Beer, T., Li, J., and Alverson, K.: Global Change and Future Earth: The Geoscience Perspective, Cambridge University Press, Cambridge, 2018. a
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We characterized the (dis)agreement between six evaporation methods from hourly to decadal timescales, focussing on the IJsselmeer region in the Netherlands. The projected changes in mean yearly water losses through evaporation between the years 2000 and 2100 range from 4 mm to 94 mm among the methods. We therefore stress that the choice of method is of great importance for water managers in their decision making.
We characterized the (dis)agreement between six evaporation methods from hourly to decadal...
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