Articles | Volume 17, issue 24
https://doi.org/10.5194/bg-17-6423-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-6423-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Decoupling of a Douglas fir canopy: a look into the subcanopy with continuous vertical temperature profiles
Bart Schilperoort
CORRESPONDING AUTHOR
Water Management, Delft University of Technology, Stevinweg 1, 2628 CN Delft, the Netherlands
Miriam Coenders-Gerrits
Water Management, Delft University of Technology, Stevinweg 1, 2628 CN Delft, the Netherlands
César Jiménez Rodríguez
Water Management, Delft University of Technology, Stevinweg 1, 2628 CN Delft, the Netherlands
Escuela de Ingeniería Forestal, Tecnológico de Costa Rica, 159-7050, Cartago, Costa Rica
Christiaan van der Tol
Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Hengelosestraat 99, 7514 AE Enschede, the Netherlands
Bas van de Wiel
Geoscience & Remote Sensing, Delft University of Technology, Stevinweg 1, 2628 CN Delft, the Netherlands
Hubert Savenije
Water Management, Delft University of Technology, Stevinweg 1, 2628 CN Delft, the Netherlands
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Latest update: 23 Nov 2024
Short summary
With distributed temperature sensing (DTS) we measured a vertical temperature profile in a forest, from the forest floor to above the treetops. Using this temperature profile we can see which parts of the forest canopy are colder (thus more dense) or warmer (and less dense) and study the effect this has on the suppression of turbulent mixing. This can be used to improve our knowledge of the interaction between the atmosphere and forests and improve carbon dioxide flux measurements over forests.
With distributed temperature sensing (DTS) we measured a vertical temperature profile in a...
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