2021
DOI: 10.1016/j.agrformet.2020.108243
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Differential response of oak and beech to late frost damage: an integrated analysis from organ to forest

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Cited by 21 publications
(20 citation statements)
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“…The NDVI dataset shows another legacy of the spring frost, a delay in autumn leaf senescence in the frost year and also but less markedly in the following year (Figure 7). This trend is consistent with a previous study conducted in the same forest about the consequences of the 2017 frost on stem, shoot and leaf functional traits, including leaf phenology using shorter NDVI time series, but with higher temporal and spatial resolution (Rubio-Cuadrado et al 2021). Here, we found no significant differences in NDVI between years, but this is partly because of the low number of springfrost years with NDVI data (1995, 2010 and 2013) and the low spatial resolution of the dataset analyzed.…”
Section: Frost Legacies: Decreasing Resistance Index and Delayed Sene...supporting
confidence: 92%
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“…The NDVI dataset shows another legacy of the spring frost, a delay in autumn leaf senescence in the frost year and also but less markedly in the following year (Figure 7). This trend is consistent with a previous study conducted in the same forest about the consequences of the 2017 frost on stem, shoot and leaf functional traits, including leaf phenology using shorter NDVI time series, but with higher temporal and spatial resolution (Rubio-Cuadrado et al 2021). Here, we found no significant differences in NDVI between years, but this is partly because of the low number of springfrost years with NDVI data (1995, 2010 and 2013) and the low spatial resolution of the dataset analyzed.…”
Section: Frost Legacies: Decreasing Resistance Index and Delayed Sene...supporting
confidence: 92%
“…The lower impact of spring frosts on Q. petraea growth is partly explained by the lower damage suffered by the leaves, which would be in turn related to its later leaf phenology (Figure 2), but it is also explained by the differences between tree species when faced with the same damage. In this sense, the loss of a cohort of leaves caused by a spring frost seems to produce a decrease in growth in F. sylvatica but not in Q. petraea (Rubio-Cuadrado et al 2021). The lower Q. petraea growth produced in frost years (Figure 5) seems to be due mostly to a delay in phenology, possibly caused by the freeze-thaw events (Tedla et al 2020), rather than to a direct effect of the damage suffered by the frozen leaves.…”
Section: Discussionmentioning
confidence: 92%
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“…The EFCM is based on 16-day maximum value composites derived from daily Terra MODIS NDVI observations spanning the period of 2001 to current at a spatial resolution of 231.25 × 231.25 m and covering the area of Europe. We based the EFCM on NDVI since it represents vegetation greenness which reflects tree-species phenology (Misra et al, 2016 , 2018 ) and responds sensitively to drought-stress in trees (Anyamba and Tucker, 2012 ; Orth et al, 2016 ; Buras et al, 2018 , 2020 ; Brun et al, 2020 ; Rita et al, 2020 ), late-frost damage (Rubio-Cuadrado et al, 2021 ), tree die-back (Rogers et al, 2018 ; Liu et al, 2019 ; Spruce et al, 2019 ), and has been used to compute vegetation condition indices (e.g., Kogan, 1995 ). Given its wide application within a forest-decline context, we consider NDVI as a meaningful proxy for actual forest condition which, in case of extreme values, may represent extraordinary phenology (early start of the season and early senescence, e.g., Misra et al, 2016 ; Brun et al, 2020 ) or canopy greenness due to atypical environmental conditions such as drought, late-frost, water-logged soils succeeding long-lasting precipitation events, ice storms, and windthrow (e.g., Bascietto et al, 2018 ; Buras et al, 2020 ; Rita et al, 2020 ).…”
Section: Methodsmentioning
confidence: 99%