1926
DOI: 10.3406/bagf.1926.6321
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L'indice d'aridité

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Cited by 158 publications
(70 citation statements)
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“…We specified the mean of the gamma distribution (a × n) as a function of initial size (S , as the basal area in 2-SFI), competition (C, as the value of a competition index), mean annual temperature (T ) and mean annual precipitation (P). Other climatic predictors such as aridity indices (Dantin and Revenga, 1940;De Martonne, 1926) were first considered but they systematically rendered poorer fits to the growth models and were therefore not included in the final model. We tested different functional forms that covered a wide range of possible responses: linear, Michaelis Menten-type, power, exponential and hyperbolic.…”
Section: Model Formulation and Comparisonmentioning
confidence: 99%
“…We specified the mean of the gamma distribution (a × n) as a function of initial size (S , as the basal area in 2-SFI), competition (C, as the value of a competition index), mean annual temperature (T ) and mean annual precipitation (P). Other climatic predictors such as aridity indices (Dantin and Revenga, 1940;De Martonne, 1926) were first considered but they systematically rendered poorer fits to the growth models and were therefore not included in the final model. We tested different functional forms that covered a wide range of possible responses: linear, Michaelis Menten-type, power, exponential and hyperbolic.…”
Section: Model Formulation and Comparisonmentioning
confidence: 99%
“…Also, due to the diversity and heterogeneity of the climatic descriptions made by the various authors, and to be able to compare different fir species, it seemed interesting to use De Martonne's [29] aridity index: IA = P/T + 10 where P is annual precipitation in mm and T is mean annual temperature in o C. The lower the index value, the greater the degree of drought.…”
Section: Simulation Of Climatic Changesmentioning
confidence: 99%
“…The precipitation on the 25 triplets ranged from 520 to 1175 mm, and the mean annual temperature varied from 6 to 10.5°C. Therefore, the aridity index according to de Martonne (1926), calculated as ratio of precipitation and mean temperature plus 10°, was determined to be within a range of 28-61 mm°C -1 . Stand age, soil characteristics, climate data, and site information can be found in the online supplement material of Pretzsch et al (2015).…”
Section: Experimental Sitesmentioning
confidence: 99%
“…Several studies developed such models, e.g. Schnedl (2003) for European beech and Scots pine (Pinus sylvestris L.) in Austria, or Döbbeler (2004) for several tree species in Germany, and Condés et al (2016) for Scots pine and European beech stands in Europe depending on the aridity index according to de Martonne (1926). These models showed considerable differences for this relationship between tree species and between mixed and monospecific stands at the same sites (Pretzsch and Biber 2016).…”
Section: Introductionmentioning
confidence: 99%