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231225s2020 xx |||||o 00| ||eng c |
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|a 10.1111/gcb.15007
|2 doi
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|a pubmed24n1018.xml
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|a (NLM)31957162
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|a DE-627
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|c DE-627
|e rakwb
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|a eng
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| 100 |
1 |
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|a Damm, Alexander
|e verfasserin
|4 aut
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| 245 |
1 |
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|a Remote sensing of forest gas exchange
|b Considerations derived from a tomographic perspective
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|c 2020
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| 336 |
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|a Text
|b txt
|2 rdacontent
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|a ƒaComputermedien
|b c
|2 rdamedia
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| 338 |
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|a ƒa Online-Ressource
|b cr
|2 rdacarrier
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|a Date Revised 29.11.2023
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|a published: Print-Electronic
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|a Citation Status PubMed-not-MEDLINE
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| 520 |
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|a © 2020 John Wiley & Sons Ltd.
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|a The global exchange of gas (CO2 , H2 O) and energy (sensible and latent heat) between forest ecosystems and the atmosphere is often assessed using remote sensing (RS) products. Although these products are essential in quantifying the spatial variability of forest-atmosphere exchanges, large uncertainties remain from a measurement bias towards top of canopy fluxes since optical RS data are not sensitive for the vertically integrated forest canopy. We hypothesize that a tomographic perspective opens new pathways to advance upscaling gas exchange processes from leaf to forest stands and larger scales. We suggest a 3D modelling environment comprising principles of ecohydrology and radiative transfer modelling with measurements of micrometeorological variables, leaf optical properties and forest structure, and assess 3D fields of net CO2 assimilation (An ) and transpiration (T) in a Swiss temperate forest canopy. 3D simulations were used to quantify uncertainties in gas exchange estimates inherent to RS approaches and model assumptions (i.e. a big-leaf approximation in modelling approaches). Our results reveal substantial 3D heterogeneity of forest gas exchange with top of canopy An and T being reduced by up to 98% at the bottom of the canopy. We show that a simplified use of RS causes uncertainties in estimated vertical gas exchange of up to 300% and that the spatial variation of gas exchange in the footprint of flux towers can exceed diurnal dynamics. We also demonstrate that big-leaf assumptions can cause uncertainties up to a factor of 10 for estimates of An and T. Concluding, we acknowledge the large potential of 3D assessments of gas exchange to unravelling the role of vertical variability and canopy structure in regulating forest-atmosphere gas and energy exchange. Such information allows to systematically link canopy with global scale controls on forest functioning and eventually enables advanced understanding of forest responses to environmental change
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|a Journal Article
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| 650 |
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|a 3D radiative transfer modelling
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| 650 |
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4 |
|a DART
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| 650 |
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4 |
|a LiDAR
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| 650 |
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4 |
|a eddy covariance
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| 650 |
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4 |
|a net CO2 assimilation
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| 650 |
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4 |
|a soil-plant-atmosphere continuum model
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| 650 |
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4 |
|a temperate forest ecosystems
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| 650 |
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4 |
|a transpiration
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| 700 |
1 |
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|a Paul-Limoges, Eugenie
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Kükenbrink, Daniel
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Bachofen, Christoph
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Morsdorf, Felix
|e verfasserin
|4 aut
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| 773 |
0 |
8 |
|i Enthalten in
|t Global change biology
|d 1999
|g 26(2020), 4 vom: 18. Apr., Seite 2717-2727
|w (DE-627)NLM098239996
|x 1365-2486
|7 nnns
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| 773 |
1 |
8 |
|g volume:26
|g year:2020
|g number:4
|g day:18
|g month:04
|g pages:2717-2727
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| 856 |
4 |
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|u http://dx.doi.org/10.1111/gcb.15007
|3 Volltext
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