2020
DOI: 10.5194/gmd-13-905-2020
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HETEROFOR 1.0: a spatially explicit model for exploring the response of structurally complex forests to uncertain future conditions – Part 1: Carbon fluxes and tree dimensional growth

Abstract: Given the multiple abiotic and biotic stressors resulting from global changes, management systems and practices must be adapted in order to maintain and reinforce the resilience of forests. Among others, the transformation of monocultures into uneven-aged and mixed stands is an avenue to improve forest resilience. To explore the forest response to these new silvicultural practices under a changing environment, one needs models combining a processbased approach with a detailed spatial representation, which is q… Show more

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Cited by 22 publications
(37 citation statements)
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“…The option phenology at tree level was used to test if the agreement between predicted and observed basal area increment could be improved. With the default phenology option, HETEROFOR tended to overestimate the growth of dominant trees and underestimate that of suppressed trees (Jonard et al, 2020a). With the option phenology at tree level, this bias was partially resorbed.…”
Section: Phenologymentioning
confidence: 99%
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“…The option phenology at tree level was used to test if the agreement between predicted and observed basal area increment could be improved. With the default phenology option, HETEROFOR tended to overestimate the growth of dominant trees and underestimate that of suppressed trees (Jonard et al, 2020a). With the option phenology at tree level, this bias was partially resorbed.…”
Section: Phenologymentioning
confidence: 99%
“…with T surf (in degrees Celsius), the temperature at the soil surface, considered as equal to air temperature (T ), T int (in degrees Celsius), the temperature at the interface between the organic layers and the mineral soil (see Jonard et al, 2020a, for more information on the way T int is obtained), and th org (in metres), the thickness of the organic layer. For ground vegetation transpiration and soil evaporation, the aerodynamic resistance is computed by applying Eqs.…”
Section: Ground Vegetation Transpiration and Soil Evaporationmentioning
confidence: 99%
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