The chill accumulation model is used to estimate the number of days from harvest (or leaf fall) in the previous season until bud break in the current season. It is well known that tree crops and natural tree species have specific chill requirements, which are related to the number of accumulated hours within a known temperature range. In this model, we use chill days (CD), which are defined as the cumulative number of hours below a pre-selected threshold temperature divided by 24 hours per day (to express as accumulated days rather than hours). We also use "anti-Chill days" (CA), which are defined as the cumulative number of hours above the same pre-selected threshold temperature divided by 24 hours per day. The CD values are given a negative sign and the CA values are given a positive sign. In the model, the CD values are accumulated until they reach a pre-selected value that is identified as the chill requirement (CR). Because the CD values are negative, the CR is also negative. The chill requirement is met on the day when the SCD is less or equal to CR. On the following day, the model no longer adds CD, but begins to add daily anti-chill days to CR. On the date that CR + SCA is equal or greater than 0, that date is selected for bud break. The optimal value for the chill temperature threshold and for CR are determined using trial and error until the root mean square error between predicted and observed days between harvest or leaf drop and bud break is minimized.

A new model for estimating chill accumulation requirements for crop and natural tree species

Cesaraccio C;Duce P
2002

Abstract

The chill accumulation model is used to estimate the number of days from harvest (or leaf fall) in the previous season until bud break in the current season. It is well known that tree crops and natural tree species have specific chill requirements, which are related to the number of accumulated hours within a known temperature range. In this model, we use chill days (CD), which are defined as the cumulative number of hours below a pre-selected threshold temperature divided by 24 hours per day (to express as accumulated days rather than hours). We also use "anti-Chill days" (CA), which are defined as the cumulative number of hours above the same pre-selected threshold temperature divided by 24 hours per day. The CD values are given a negative sign and the CA values are given a positive sign. In the model, the CD values are accumulated until they reach a pre-selected value that is identified as the chill requirement (CR). Because the CD values are negative, the CR is also negative. The chill requirement is met on the day when the SCD is less or equal to CR. On the following day, the model no longer adds CD, but begins to add daily anti-chill days to CR. On the date that CR + SCA is equal or greater than 0, that date is selected for bud break. The optimal value for the chill temperature threshold and for CR are determined using trial and error until the root mean square error between predicted and observed days between harvest or leaf drop and bud break is minimized.
2002
Istituto di Biometeorologia - IBIMET - Sede Firenze
Bud break
tree crops
natural tree species
chill accumulation models
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/60220
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