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Jasechko et al. reply
replying to A. M. J. Coenders-Gerrits et al. Nature506,http://dx.doi.org/10.1038/nature12925(2014) In their Comment, Coenders-Gerrits et al. 1 suggest that our conclusion that transpiration dominates the terrestrial water cycle 2 is biased by unrepresentative input data and optimistic uncertainty ra...
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| Published in: | Nature (London) 2014-02, Vol.506 (7487), p.E2-E3 |
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| Main Authors: | , , , , , |
| Format: | Article |
| Language: | English |
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| container_end_page | E3 |
| container_issue | 7487 |
| container_start_page | E2 |
| container_title | Nature (London) |
| container_volume | 506 |
| creator | Jasechko, Scott Sharp, Zachary D. Gibson, John J. Birks, S. Jean Yi, Yi Fawcett, Peter J. |
| description | replying to
A. M. J. Coenders-Gerrits
et al.
Nature506,http://dx.doi.org/10.1038/nature12925(2014)
In their Comment, Coenders-Gerrits
et al.
1
suggest that our conclusion that transpiration dominates the terrestrial water cycle
2
is biased by unrepresentative input data and optimistic uncertainty ranges related to runoff, interception and the isotopic compositions of transpired and evaporated moisture. We clearly presented the uncertainties applied in our Monte-Carlo sensitivity analysis, we reported percentile ranges of results rather than standard deviations to best communicate the nonlinear nature of the isotopic evaporation model, and we highlighted that the uncertainty in our calculation remains large, particularly in humid catchments (for example, figure 2 in our paper
2
). |
| doi_str_mv | 10.1038/nature12926 |
| format | article |
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A. M. J. Coenders-Gerrits
et al.
Nature506,http://dx.doi.org/10.1038/nature12925(2014)
In their Comment, Coenders-Gerrits
et al.
1
suggest that our conclusion that transpiration dominates the terrestrial water cycle
2
is biased by unrepresentative input data and optimistic uncertainty ranges related to runoff, interception and the isotopic compositions of transpired and evaporated moisture. We clearly presented the uncertainties applied in our Monte-Carlo sensitivity analysis, we reported percentile ranges of results rather than standard deviations to best communicate the nonlinear nature of the isotopic evaporation model, and we highlighted that the uncertainty in our calculation remains large, particularly in humid catchments (for example, figure 2 in our paper
2
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A. M. J. Coenders-Gerrits
et al.
Nature506,http://dx.doi.org/10.1038/nature12925(2014)
In their Comment, Coenders-Gerrits
et al.
1
suggest that our conclusion that transpiration dominates the terrestrial water cycle
2
is biased by unrepresentative input data and optimistic uncertainty ranges related to runoff, interception and the isotopic compositions of transpired and evaporated moisture. We clearly presented the uncertainties applied in our Monte-Carlo sensitivity analysis, we reported percentile ranges of results rather than standard deviations to best communicate the nonlinear nature of the isotopic evaporation model, and we highlighted that the uncertainty in our calculation remains large, particularly in humid catchments (for example, figure 2 in our paper
2
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A. M. J. Coenders-Gerrits
et al.
Nature506,http://dx.doi.org/10.1038/nature12925(2014)
In their Comment, Coenders-Gerrits
et al.
1
suggest that our conclusion that transpiration dominates the terrestrial water cycle
2
is biased by unrepresentative input data and optimistic uncertainty ranges related to runoff, interception and the isotopic compositions of transpired and evaporated moisture. We clearly presented the uncertainties applied in our Monte-Carlo sensitivity analysis, we reported percentile ranges of results rather than standard deviations to best communicate the nonlinear nature of the isotopic evaporation model, and we highlighted that the uncertainty in our calculation remains large, particularly in humid catchments (for example, figure 2 in our paper
2
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| ispartof | Nature (London), 2014-02, Vol.506 (7487), p.E2-E3 |
| issn | 0028-0836 1476-4687 |
| language | eng |
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| source | Nature |
| subjects | 704/106/242 704/172/169/895 brief-communications-arising Climate models Environmental aspects Forecasts and trends Fresh Water - analysis Humanities and Social Sciences multidisciplinary Plant Transpiration - physiology Plants Plants - metabolism Runoff Science Transpiration Water Movements |
| title | Jasechko et al. reply |
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