1987
DOI: 10.1016/s0022-5193(87)80237-0
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The temperature dependence of dormancy breaking in plants: Computer simulation of processes studied under controlled temperatures

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Cited by 262 publications
(190 citation statements)
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“…The chilling requirement until LF (24 CP, beginning of endodormancy) and t 1 (41 CP, end of endodormancy) were relatively constant in all years (Table 4), which allows to calculate the endodormancy phase in phenological models by the dynamic approach [55,56]. Our results confirm the fact that in temperate climates a distinct time lag between t 1 and t 1 * can exist [17,37].…”
Section: Relevance For Phenological Modellingsupporting
confidence: 76%
“…The chilling requirement until LF (24 CP, beginning of endodormancy) and t 1 (41 CP, end of endodormancy) were relatively constant in all years (Table 4), which allows to calculate the endodormancy phase in phenological models by the dynamic approach [55,56]. Our results confirm the fact that in temperate climates a distinct time lag between t 1 and t 1 * can exist [17,37].…”
Section: Relevance For Phenological Modellingsupporting
confidence: 76%
“…23 Chill unit models provide information on how cultivars fare under the current and future climate conditions, inform producers of the stage of phenological development during the growing season and prediction of maturity dates which improve market delivery of fruits. Three important monitoring systems for chill units have been commonly applied: the Utah (Richardson) model 24 measuring RCU, the Infruitec model (daily positive Utah model) measuring Infruitec chill units and the dynamic chill model 25,26 measuring dynamic chill portion (DCP). Studies on winter chill and chilling requirements often implicitly assume that all models can be used interchangeably because the choice of model is not important.…”
Section: Impact Of Climate Change On Chill Unit Accumulationmentioning
confidence: 99%
“…This model has been established to give a more precise estimate of winter chilling in regions with mild winters, as well as in areas suffering from very cold winters. 32 The dynamic model 25,26 was introduced in the 1980s as a new concept for the negation process 32 . This model is based on the premise that winter chill accumulates as a result of a two-step process.…”
Section: Impact Of Climate Change On Chill Unit Accumulationmentioning
confidence: 99%
“…However, it is rather very difficult to express the agriculture related effects of the climate change in numbers and figures as the soil-plant-atmosphere system is very complex. Different simulation models of winter chill accumulation have been developed which are purely empirical and based on either field observations [14] or controlled temperature experiments [15] rather than on a functional understanding of tree physiology. The most widely used models to calculate chill units are as follows-…”
Section: Calculation Of Chill Unitsmentioning
confidence: 99%