Skip to main content

Advertisement

Log in

Accumulated winter chill is decreasing in the fruit growing regions of California

  • Published:
Climatic Change Aims and scope Submit manuscript

Abstract

We examined trends in accumulated winter chill across the fruit growing region of central California and its internal coastal valleys. We tested the hypothesis that global warming is in motion in California and is causing accumulated winter chill to decrease across the fruit and nut growing regions of California. The detection of potential trends in accumulated winter chill (between 0 and 7.2°C) was determined using two complementary climate datasets. The California Irrigation Management Information System (CIMIS) contains hourly climate data and is suitable for computing accumulated chill hours and chill degree-hours. But, its longest data records extend back only to the 1980s. The National Weather Service Coop climate record is longer, extending beyond the 1950s at many sites. But its datasets only contain information on daily maximum and minimum temperatures. To assess long term trends in winter chill accumulation, we developed an algorithm that converted information from daily maximum and minimum temperature into accumulated hours of winter chill and summations of chill-degree hours. These inferred calculations of chill hour accumulation were tested with and validated by direct measurements from hourly-based data from the CIMIS network. With the combined climate datasets, we found that the annual accumulation of winter chill hours and chill degree hours is diminishing across the fruit and nut growing regions of California. Observed trends in winter chill range between -50 and -260 chill hours per decade. We also applied our analytical algorithm to project changes in winter chill using regional climate projections of temperature for three regions in the Central Valley. Predicted rates of reduced winter chill, for the period between 1950 and 2100, are on the order of -40 h per decade. By the end of the 21st century, orchards in California are expected to experience less than 500 chill hours per winter. This chronic and steady reduction in winter chill is expected to have deleterious economic and culinary impact on fruit and nut production in California by the end of the 21st Century.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Anonymous (2003) California Agriculture Overview. California Agricultural Statistics Service, Sacramento, p 10

  • Aron R (1983) Availability of chilling temperatures in California. Agric Meteorol 28:351–363

    Article  Google Scholar 

  • Aron RH (1975) A method for estimating the number of hours below a selected temperature threshold. J Appl Meteorol 14:1415–1418

    Article  Google Scholar 

  • Cayan D, Kammerdiener S, Dettinger M, Caprio J, Peterson D (2001) Changes in the onset of spring in the western United States. B Am Meteorol Soc 82:399–415

    Article  Google Scholar 

  • Cayan DR, Maurer EP, Dettinger M, Tyree M, Hayhoe K, Bonfils C, Duffy P, Santer BD (2005) Climate scenarios for California. CEC-500–2005–203-SD. California Climate Change Center, Sacramento, p 47

    Google Scholar 

  • Chmielewski F-M, Muller A, Bruns E (2004) Climate changes and trends in phenology of fruit trees and field crops in Germany, 1961–2000. Agric Forest Meteorol 121:69–78

    Article  Google Scholar 

  • Christy JR, Norris WB, Redmond K, Gallo KP (2006) Methodology and results of calculating central California surface temperature trends: evidence of human-induced climate change? J Clim 19:548–563

    Article  Google Scholar 

  • Egea J, Ortega E, Martinez-Gomez P, Dicenta F (2003) Chilling and heat requirements of almond cultivars for flowering. Environ Exp Bot 50:79–85

    Google Scholar 

  • Feng S, Hu Q (2004) Changes in agro-meteorological indicators in the contiguous United States: 1951–2000. Theor Appl Climatol 78:247–264

    Article  Google Scholar 

  • Friedlingstein P, Dufresne J-L, Cox PM, Rayner P (2003) How positive is the feedback between climate change and the carbon cycle? Tellus B 55:692–700

    Article  Google Scholar 

  • Fung IY, Doney SC, Lindsay K, John J (2005) Evolution of carbon sinks in a changing climate. Proc Natl Acad Sci U S A 102:11201–11206

    Article  Google Scholar 

  • Gutierrez AP, Ponti L, Ellis CK, d'Oultremont T (2006) Analysis of climate effects on agricultural systems. CEC-500–2005–188-SF. California Climate Change Center, Sacramento

    Google Scholar 

  • Hayhoe K, Cayan D, Field C, Frumhoff PC, Maurer EP, Miller NL, Moser S, Schneider SH, Cahill K, Cleland EE, Dale L, Drapek R, Hanemann RM, Lalkstein L, Lenihan JM, Lunch CK, Neilson RP, Sheridan SC, Verville JH (2004) Emissions pathways, climate change and impacts on California. Proc Natl Acad Sci U S A 101:12422–12427

    Article  Google Scholar 

  • Holets S, Swanson RN (1981) High-inversion fog episodes in Central California. J Appl Meteorol 20:890–899

    Article  Google Scholar 

  • Izaurralde RC, Rosenberg NJ, Brown RA, Thomson AM (2003) Integrated assessment of Hadley Center (HadCM2) climate-change impacts on agricultural productivity and irrigation water supply in the conterminous United States: Part II. Regional agricultural production in 2030 and 2095. Agric Forest Meteorol 117:97–122

    Article  Google Scholar 

  • Maurer EP, Duffy PB (2005) Uncertainty in projections of streamflow changes due to climate change in California. Geophys Res Lett 32:L03704 DOI 10.1029/2004GL021462

  • McKenney DW, Pedlar JH, Papadopol P, Hutchinson MF (2006) The development of 1901–2000 historical monthly climate models for Canada and the United States. Agric Forest Meteorol 138:69–81

    Article  Google Scholar 

  • McNaughton KG, Spriggs TW (1986) A mixed-layer model for regional evaporation. Bound-Lay Meteorol 34:243–262

    Article  Google Scholar 

  • Monteith JL, Unsworth MH (1990) Principles of environmental physics. Arnold, London

    Google Scholar 

  • Nakicenovic N, Alcamo J, Davis G, Vries BD, Fenhann J, Gaffin S, Gregory K, Grübler A, Jung TY, Kram T, Rovere ELL, Michaelis L, Mori S, Morita T, Pepper W, Pitcher H, Price L, Riahi K, Roehrl A, Rogner H-H, Sankovski A, Schlesinger M, Shukla P, Smith S, Swart R, Rooijen SV, Victor N, Dadi Z (2000) Special report on emission scenarios. Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge

    Google Scholar 

  • Nemani RR, White MA, Cayan DR, Jones GV, Running SW, Coughlan JC, Peterson DL (2001) Asymmetric warming over coastal California and its impact on the premium wine industry. Clim Res 19:25–34

    Article  Google Scholar 

  • Porter JR, Semenov MA (2005) Crop responses to climatic variation. Philos Trans R Soc Lond B Biol Sci 360:2021–2035

    Article  Google Scholar 

  • Rattigan K, Hill SJ (1986) Relationship between temperature and flowering in almond. Aust J Exp Agric 26:399–404

    Article  Google Scholar 

  • Richardson EA, Seeley SD, Walker DR (1974) A model for estimating the completion of rest for ‘Redhaven’ and ‘Elberta’ peach trees. HortScience 9:331–332

    Google Scholar 

  • Rosenweig C, Hillell D (1998) Climate change and the global harvest. Oxford, Oxford

    Google Scholar 

  • Samish RM (1954) Dormancy in woody plants. Annu Rev Plant Physiol 5:183–204

    Article  Google Scholar 

  • Snyder MA, Bell JA, Sloan L, Duffy PB, Govindasamy B (2002) Climate responses to a doubling of atmospheric carbon dioxide for a climatically vulnerable region. Geophys Res Lett 29 DOI 10.1029/2001GL014431

  • Snyder RL, Spano D, Cesaraccio C, Duce P (1999) Determining degree-day thresholds from field observations. Int J Biometeorol V42:177–182

    Article  Google Scholar 

  • Suckling PW, Mitchell MD (1988) Fog climatology of the Sacramento urban area. Prof Geogr 40:186–194

    Article  Google Scholar 

  • Underwood SJ, Ellrod GP, Kuhnert AL (2004) A multiple-case analysis of nocturnal radiation-fog development in the Central Valley of California utilizing the GOES Nighttime Fog Product. J Appl Meteorol 43:297–311

    Article  Google Scholar 

  • VanRheenan NT, Wood AW, Palmer RN, Lettenmaier DP (2004) Potential implications of PCM climate change scenarios for Sacramento-San Joaquin River basin hydrology and water resources. Clim Change 62:257–281

    Article  Google Scholar 

  • Wood AW, Maurer EP, Kumar A, Lettenmaier DP (2002) Long range experimental hydrologic forecasting for the eastern U.S. J Geophys Res 107:4429

    Article  Google Scholar 

  • Zalom F, Goodell P, Wilson LT, Barnett WW, Bentley WJ (1983) Degree days: the calculation and use of heat units in pest management. University of California DANR Leaflet. 21373. pg

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Dennis Baldocchi.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Baldocchi, D., Wong, S. Accumulated winter chill is decreasing in the fruit growing regions of California. Climatic Change 87 (Suppl 1), 153–166 (2008). https://doi.org/10.1007/s10584-007-9367-8

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10584-007-9367-8

Keywords

Navigation