CATchment and ecohydrology research group, Environmental sensing and modelling unit, Luxembourg Institute of Science and Technology, Belvaux, Luxembourg
Faculty of Science, Technology and Medicine, University of Luxembourg, Belval, Luxembourg
Christoph J. Gey
Institute of Geosciences, University of Mainz, Mainz, Germany
Bernd R. Schöne
Institute of Geosciences, University of Mainz, Mainz, Germany
Dept. of Environmental Systems Science, 5 ETH Zürich, Zürich, Switzerland
Swiss Federal Research Institute WSL, Birmensdorf, Switzerland
Dept. of Earth and Planetary Science, University of California, Berkeley, CA, USA
Loic Leonard
CATchment and ecohydrology research group, Environmental sensing and modelling unit, Luxembourg Institute of Science and Technology, Belvaux, Luxembourg
CATchment and ecohydrology research group, Environmental sensing and modelling unit, Luxembourg Institute of Science and Technology, Belvaux, Luxembourg
CATchment and ecohydrology research group, Environmental sensing and modelling unit, Luxembourg Institute of Science and Technology, Belvaux, Luxembourg
CATchment and ecohydrology research group, Environmental sensing and modelling unit, Luxembourg Institute of Science and Technology, Belvaux, Luxembourg
Faculty of Science, Technology and Medicine, University of Luxembourg, Belval, Luxembourg
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Total article views: 4,864 (including HTML, PDF, and XML)
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4,864
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285
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EndNote: 285
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Total article views: 1,486 (including HTML, PDF, and XML)
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HTML: 929
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BibTeX: 95
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2,670
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HTML: 2,670
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Viewed (geographical distribution)
Total article views: 4,864 (including HTML, PDF, and XML)
Thereof 4,760 with geography defined
and 104 with unknown origin.
Total article views: 1,486 (including HTML, PDF, and XML)
Thereof 1,396 with geography defined
and 90 with unknown origin.
Total article views: 3,378 (including HTML, PDF, and XML)
Thereof 3,364 with geography defined
and 14 with unknown origin.
How landscape features affect water storage and release in catchments remains poorly understood. Here we used water stable isotopes in 12 streams to assess the fraction of precipitation reaching streamflow in less than 2 weeks. More recent precipitation was found when streamflow was high and the fraction was linked to the geology (i.e. high when impermeable, low when permeable). Such information is key for better anticipating streamflow responses to a changing climate.
How landscape features affect water storage and release in catchments remains poorly understood....