Articles | Volume 23, issue 1
https://doi.org/10.5194/hess-23-515-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-23-515-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Using phase lags to evaluate model biases in simulating the diurnal cycle of evapotranspiration: a case study in Luxembourg
Max Planck Institute for Biogeochemistry, 07745 Jena, Germany
Claire Brenner
Institut für Wasserwirtschaft, Hydrologie und konstruktiven Wasserbau, Universität für Bodenkultur (BOKU), 1190 Vienna, Austria
Kaniska Mallick
Department of Environmental Research and Innovation, Luxembourg Institute of Science and Technology (LIST), 4422 Belvaux, Grand Duchy of Luxembourg
Hans-Dieter Wizemann
Institut für Physik und Meteorologie, Universität Hohenheim, 70599 Stuttgart, Germany
Luigi Conte
Max Planck Institute for Biogeochemistry, 07745 Jena, Germany
Ivonne Trebs
Department of Environmental Research and Innovation, Luxembourg Institute of Science and Technology (LIST), 4422 Belvaux, Grand Duchy of Luxembourg
Jianhui Wei
Institut für Physik und Meteorologie, Universität Hohenheim, 70599 Stuttgart, Germany
Volker Wulfmeyer
Institut für Physik und Meteorologie, Universität Hohenheim, 70599 Stuttgart, Germany
Karsten Schulz
Institut für Wasserwirtschaft, Hydrologie und konstruktiven Wasserbau, Universität für Bodenkultur (BOKU), 1190 Vienna, Austria
Axel Kleidon
Max Planck Institute for Biogeochemistry, 07745 Jena, Germany
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- Temporal patterns of carbon-water coupling of a subalpine peatland in subtropics: Insights from a seven-year eddy covariance monitoring Z. Liu et al. 10.1016/j.ejrh.2024.101903
- An assessment of phase relationships between heat fluxes and ground surface temperatures in a diurnal cycle based on monitoring studies at the Verkhnee Dubrovo meteorological station D. Demezhko et al. 10.24930/1681-9004-2022-22-2-239-250
- Ozone deposition impact assessments for forest canopies require accurate ozone flux partitioning on diurnal timescales A. Visser et al. 10.5194/acp-21-18393-2021
- Comparison of Empirical Methods to Estimated Reference Evapotranspiration L. Gandri et al. 10.29303/jrpb.v12i2.629
- Do Surface and Air Temperatures Contain Similar Imprints of Evaporative Conditions? A. Panwar et al. 10.1029/2019GL082248
- Challenges and Future Perspectives of Multi-/Hyperspectral Thermal Infrared Remote Sensing for Crop Water-Stress Detection: A Review M. Gerhards et al. 10.3390/rs11101240
- Energy Imbalance and Evapotranspiration Hysteresis Under an Advective Environment: Evidence From Lysimeter, Eddy Covariance, and Energy Balance Modeling R. Dhungel et al. 10.1029/2020GL091203
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- Hysteresis Behavior of Surface Water Fluxes in a Hydrologic Transition of an Ephemeral Lake Y. Cui et al. 10.1029/2019JD032364
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- Summarizing the state of the terrestrial biosphere in few dimensions G. Kraemer et al. 10.5194/bg-17-2397-2020
- Energy balance closure and evapotranspiration hysteresis in central Amazon under contrasting conditions during the GoAmazon project in 2014 and 2015 R. Carneiro et al. 10.1016/j.jsames.2023.104686
Latest update: 08 Dec 2024
Short summary
We estimate the phase lag of surface states and heat fluxes to incoming solar radiation at the sub-daily timescale. While evapotranspiration reveals a minor phase lag, the vapor pressure deficit used as input by Penman–Monteith approaches shows a large phase lag. The surface-to-air temperature gradient used by energy balance residual approaches shows a small phase shift in agreement with the sensible heat flux and thus explains the better correlation of these models at the sub-daily timescale.
We estimate the phase lag of surface states and heat fluxes to incoming solar radiation at the...