Tracking Winter Chill in Fruit Growing Regions
Written by Franz Niederholzer1 and Kitren Glozer2 1UC Farm Advisor, Sutter/Yuba Counties, 2Associate Project Scientist, Department of Plant Sciences, UC Davis “Is it a good chilling year?” That’s a common coffee house question this time of year in fruit and nut growing regions. The amount of chilling a perennial crop accumulates in a given winter will influence bloom conditions – the most crucial time in a crop season. Less chilling than a certain tree crop requires can lead to an extended bloom; too little altogether can result in bud death and drop in some crops like apricot and sweet cherry. ‘Good chilling’ (more chilling than the minimum required) can produce a very short bloom season, or ‘snowball bloom’. Chilling models can provide growers and their advisors with key information to time dormancy-breaking materials (hydrogen cyanamide, oil, etc.) to manipulate bloom to improve or maintain yield and quality in regions where local chilling is marginal for a certain crop. Climate change may make achieving critical chilling more important in years to come. In this article, we’ll briefly review chilling and chilling models. Deciduous perennial crops break bud in the late winter or spring after a certain amount of cold weather (chilling) followed by a certain amount of warmer weather. Think of this process as a relay race. The chilling is the first leg of the race, and the heat accumulation is the second leg. Bud break is the finish line. The length of each leg of the race depends on crop and variety. The weather during the race influences the runner’s speed. Good chilling weather speeds up the chilling leg, warmer weather can slow it down or even stop it. Cool weather on the warming leg slows the progress towards bloom. Since most perennial crops are not native to North America,
Recent Comments