1 Documentation for gridded climate data for 1961-90 and scenarios for 2010-39 and 2040-69 periods 1961-1990 baseline climate The file ‘Normals61.txt’ contains gridded monthly mean values for daily maximum and minimum air temperature and total precipitation for the 1961-1990 period. These data were constructed by interpolating monthly climate data as a function of latitude, longitude and elevation using ANUSPLIN (Hutchinson, 2000). ANUSPLIN uses thin plate smoothing splines as the interpolation technique (Hutchinson, 1995). Any stations with 5 or more years of record were used (Environment Canada, 1994). The grid is 500 arc seconds and was developed using a Digital Elevation Model (DEM) data, based on the National Topographic Series 1:250,000 topographic data. For details of these particular Canadian applications see McKenney et al. (2001) (see also Price et al. 2000). File Name: Normals61.ZIP File Structure: Comma-delimited text file, compressed using WinZip. Variables on the file are as follows: Latitude and Longitude (decimal degrees) 12 monthly values (Jan. – Dec.) for average maximum temperature, ºC 12 monthly values (Jan. – Dec.) for average minimum temperature, ºC 12 monthly values (Jan. – Dec.) for total precipitation, mm File Size: Zipped: 4.4 Mb; decompressed 12.7 Mb Climate scenarios – 2010-2039 and 2040-2069 Climate change scenarios were based on the first generation coupled Canadian General Circulation Model, greenhouse gas with aerosols simulation 1 (CGCMI GA1). Mean monthly changes in temperature and in precipitation ratios from 1961-1990 values were interpolated to the same 500 arc second grid as above using ANUSPLIN with only latitude and longitude as predictor variables. The interpolated change values were then applied to the gridded 1961-1990 normals in ‘Normals61.txt’. File Names: Normals10.ZIP (Monthly climate normals for 2010-2039 period) Normals40.ZIP (Monthly climate normals for 2040-2069 period) File Structure: Same as ‘Normals61.ZIP’ File Size: Similar to ‘Normals61.ZIP’ Calculation of agro-climatic indices Agroclimatic indices were computed using the gridded monthly values as input data. Initially, 365 daily values of average maximum temperature and of average minimum temperature were generated from monthly average values using the Brooks sine wave interpolation procedure (Brooks, 1943). Average daily values for precipitation were generated by dividing the monthly values by the number of days in the month. The average daily values were then used to compute the following indices: 2 Growing degree-days above 5ºC (GDD): GDD were computed by calculating the amount by which average daily mean temperature (Tmean) exceeded 5.0C and summing these values from the time when Tmean first exceeded 5.0C in spring until the last date of Tmean exceeded 5.0C in fall. While this procedure will result in some differences from GDD computed from daily values rather than averages (since averages may include days when temperatures were below the base value in the spring and fall periods), it has been commonly accepted as being of sufficient accuracy (Chapman and Brown 1978) Effective Growing Degree-Days (EGDD): EGDD are used as a primary climate classifier in the suitability rating system for spring-seeded small grains and are determined based on the method described in the Working Group report (Agronomics Interpretations Working Group, 1995). GDD were summed from 10 days after Tmean 5.0C in spring to the average date of the first fall frost (0C), and a daylength factor was applied to compensate for increased effectiveness of GDD in maturing cereal crops in northern latitudes. Average fall frost dates were estimated from monthly temperature normals, elevation and astronomical data as described by Sly et al. (1971). Daylength (N) and solar radiation at the top of the atmosphere (Qo) were estimated from latitude and time of year using procedures described by Robertson and Russelo (1968). Potential Evapotranspiration (PE) and Precipitation Deficit (DEFICIT): Average daily PE was determined by calculating Latent evaporation (LE) from daily temperatures and solar radiation at the top of the atmosphere, using Baier and Robertson (1965) Formula I and converting LE to PE by using the conversion factor of 0.086. Average daily DEFICIT was calculated by subtracting average daily precipitation (P) from PE. Daily DEFICIT and PE values were accumulated over periods shown below. File Names: Indices61.ZIP, Indices10.ZIP and Indices40.ZIP. These files contain the gridded indices for the 1961-90, 2010-39 and 2040-69 periods, respectively. File Structure: Comma-delimited text file, compressed using WinZip. Variables on the file are as follows: Latitude (decimal degrees) Longitude (decimal degrees) GDD (Celsius) StartGDD (Starting date for accumulating GDD, calendar day) StopGDD (Ending date for accumulating GDD, calendar day) EGDD (Celsius) StartEGDD (Starting date for accumulating EGDD, calendar day) StopEGDD (Ending date for accumulating EGDD, calendar day) DEFICIT1 (Accumulated over same period as GDD, mm) PE1 (Accumulated over same period as GDD, mm) DEFICIT2 (Positive values only of PE – P accumulated over same period as EGDD, mm) PE2 (Accumulated over same period as EGDD, mm) 3 File Size: Zipped: 0.9 Mb; decompressed: 3.3 Mb Questions about the data or feedback should be directed to: Andrew Bootsma, Agro-climatologist Agriculture and Agri-Food Canada Eastern Cereal and Oilseed Research Centre K.W. Neatby Bldg., Rm. 4129B 960 Carling Ave. Ottawa ON CANADA K1A 0C6 Tel: (613) 759-1526 Fax: (613) 759-1924 E-mail: BootsmaA@agr.gc.ca or Dan McKenney (PhD) Chief, Landscape Analysis and Applications Canadian Forest Service 1219 Queen Street East Sault Ste. Marie, Ontario CANADA P6A 2E5 Ph 705-759-5740 ext 2316 Fax 705-759-5700 Email dmckenne@nrcan.gc.ca Disclaimer: These data are available free for public use but remain copyright of Agriculture and AgriFood Canada (AAFC) and Natural Resources Canada (NRCan). The information has been obtained from a variety of sources and while efforts have been undertaken to assure its accuracy, it is provided without warranty as a public service. Any decision taken based on the information contained within these data files is the sole responsibility of the person taking the decision. REFERENCES Agronomics Interpretations Working Group. 1995. Land Suitability Rating System for Agricultural Crops: 1. Spring-seeded small grains. Edited by W.W. Pettapiece. Tech. Bull. 1995-6E. Centre for Land and Biological Resources Research, Agriculture and Agri-Food Canada, Ottawa, 90 pp., 2 maps. Baier, W. and Robertson, G.W. 1965. Estimation of latent evaporation from simple weather observations. Can. J. Plant Sci. 45: 276-284. Brooks, C.E.P. 1943. Interpolation tables for daily values of meteorological elements. 4 Quart. J. Royal Meteorol. Soc. 69: 160-162. Chapman, L.J. and Brown, D.M. 1978. The Climates of Canada for Agriculture. Canada Land Inventory Report No. 3. Revised 1978. Environment Canada, Lands Directorate, 24 pp. Environment Canada 1994. Canadian Monthly Climate Data and 1961-1990 Normals on CD-ROM, Version 3.0E. Environment Canada, Atmospheric Environment Service, Downsview, Ontario. Hutchinson, M.F. 1995. Interpolating mean rainfall using thin plate smoothing splines. Int. J. Geographical Information Systems 9: 385-403 Hutchinson, M.F. 2000. ANUSPLIN Version 4.1 User Guide. Centre for Resource and Environmental Studies, Australian National University, Canberra ACT 0200, Australia. McKenney, D.W., Hutchinson, M.F., Kesteven, J. and Venier, L. 2001. Canada's plant hardiness zones revisited using modern climate interpolation techniques. Can J. Plant Science 81:129-143 Price, D., McKenney, D.W., Nalder, I., Hutchinson, M.F. and Kestevan, J. 2000. A comparison of two statistical methods for interpolating monthly mean climate. Ag. And Forest. Met. 101:81-94. Robertson, G.W. and Russelo, D.A. 1968. Astrometeorological estimator for estimating time when sun is at any elevation, elapsed time between the same elevations in the morning and afternoon, and hourly and daily values of solar energy, Qo. Tech. Bull. 14, Agrometeor. Section, Plant Research Inst., Canada Dept. Agriculture, 22 pp. Sly, W., Robertson, G.W. and Coligado, M.C. 1971. Estimation of probable dates of temperatures near freezing from monthly temperature normals, station elevation, and astronomical data. Canada Department of Agriculture, Research Branch, Plant Research Institute, Agrometeorology Section, Ottawa, Tech. Bull. 79, 21 pp.