Climatic Changes Lead to Declining Winter Chill for Fruit and Nut Trees in California during 1950–2099

Background

Winter chill is one of the defining characteristics of a location's suitability for the production of many tree crops. We mapped and investigated observed historic and projected future changes in winter chill in California, quantified with two different chilling models (Chilling Hours, Dynamic Model).

Methodology/Principal Findings

Based on hourly and daily temperature records, winter chill was modeled for two past temperature scenarios (1950 and 2000), and 18 future scenarios (average conditions during 2041–2060 and 2080–2099 under each of the B1, A1B and A2 IPCC greenhouse gas emissions scenarios, for the CSIRO-MK3, HadCM3 and MIROC climate models). For each scenario, 100 replications of the yearly temperature record were produced, using a stochastic weather generator. We then introduced and mapped a novel climatic statistic, “safe winter chill”, the 10% quantile of the resulting chilling distributions. This metric can be interpreted as the amount of chilling that growers can safely expect under each scenario. Winter chill declined substantially for all emissions scenarios, with the area of safe winter chill for many tree species or cultivars decreasing 50–75% by mid-21st century, and 90–100% by late century.

Conclusions/Significance

Both chilling models consistently projected climatic conditions by the middle to end of the 21st century that will no longer support some of the main tree crops currently grown in California, with the Chilling Hours Model projecting greater changes than the Dynamic Model. The tree crop industry in California will likely need to develop agricultural adaptation measures (e.g. low-chill varieties and dormancy-breaking chemicals) to cope with these projected changes. For some crops, production might no longer be possible.


Similar entries

  • (Helmholtz Association of German Research Centres) Climatic fluctuations close to the equator show a different pattern toclimate change in the Arctic and Antarctic. In the tropics, distinct11,500-year fluctuations between wet and dry periods can be clearlyidentified which do not occur in temperature reconstructions of polarice cores.

  • mvdwege writes "After being cleared of charges of misconduct by a parliamentary committee, now the CRU has the results of the inquiry (PDF) by a panel of scientists into their scientific methods. Here is the CRU press release. Criticisms: The statistical methods used, though arriving at correct results, are not optimal, and it is recommended future studies involve professional statisticians if possible; and the CRU scientists are lacking somewhat in organization. A very far cry from the widespread allegations of fraud.

  • The largest known mass extinction in Earth's history, about 252 million years ago at the end of the Permian Period, may have been caused by global warming. A new fossil species suggests that some land animals may have survived the end-Permian extinction by living in cooler climates in Antarctica. Jörg Fröbisch and Kenneth D. Angielczyk of The Field Museum together with Christian A. Sidor from the University of Washington have identified a distant relative of mammals, Kombuisia antarctica, that apparently survived the mass extinction by living in Antarctica.
    read more

  • Communities have been shaped in numerous ways by past climatic change; this process continues today. At the end of the Pleistocene epoch about 11,700 years ago, North American communities were substantially altered by the interplay of two events. The climate shifted from the cold, arid Last Glacial Maximum to the warm, mesic Holocene interglacial, causing many mammal species to shift their geographic distributions substantially. Populations were further stressed as humans arrived on the continent.

  • Background

    Winter chill is one of the defining characteristics of a location's suitability for the production of many tree crops. We mapped and investigated observed historic and projected future changes in winter chill in California, quantified with two different chilling models (Chilling Hours, Dynamic Model).

  • Long-term climate fluctuations were probably the main reason for the extinction of the dinosaurs and other creatures 65 million years ago, according to new research from a German paleontologist. The results challenge the almost 30-year-old theory that a meteorite impact at the Mexican Yucatan peninsula was the single cause for one of the five largest mass extinctions in Earth history.

  • Long-term climate fluctuations were probably the main reason for the extinction of the dinosaurs and other creatures 65 million years ago, according to new research from a German paleontologist. The results challenge the almost 30-year-old theory that a meteorite impact at the Mexican Yucatan peninsula was the single cause for one of the five largest mass extinctions in Earth history.