Mapping monthly precipitation, temperature, and solar radiation for Ireland with polynomial regression and a digital elevation model

A 1 km 2 resolution digital elevation model (DEM) of Ireland was constructed and used as the basis for generating digital maps of the climate parameters required to run a model of ecosystem carbon and water cycling. The DEM had mean absolute errors of 30 m or less for most of Ireland. The ecosystem model requires inputs of monthly precipitation, monthly averaged maximum and minimum daily temperature, and monthly averaged daily solar radiation. Long-term (1951 to 1980) averaged monthly data were obtained from sites measuring precipitation (618 sites), temperature (62 sites), and the number of hours of bright sunshine per day ('sunshine hours') (61 sites). Polynomial regression was used to derive a simple model for each monthly climate variable to relate climate to position and ele- vation on the DEM. Accuracy assessments with subsets of each climate data set determined that poly- nomial regression can predict average monthly climate in Ireland with mean absolute errors of 5 to 15 mm for monthly precipitation, 0.2 to 0.5°C for monthly averaged maximum and minimum tempera- ture, and 6 to 15 min for monthly averaged sunshine hours. The polynomial regression estimates of cli- mate were compared with estimates from a modified inverse-distance-squared interpolation. Predic- tion accuracy did not differ between the 2 methods, but the polynomial regression models demanded less time to generate and less computer storage space, greatly decreasing the time required for regional modeling runs.

[1]  Alfred J. Henry INCREASE OF PRECIPITATION WITH ALTITUDE1 , 1919 .

[2]  MONTHLY VARIATIONS OF THE PRECIPITATION-ALTITUDE RELATION IN THE CENTRAL SIERRA NEVADA OF CALIFORNIA , 1920 .

[3]  Vail P. Schermerhorn Relations between topography and annual precipitation in western Oregon and Washington , 1967 .

[4]  L. Swift,et al.  Algorithm for solar radiation on mountain slopes , 1976 .

[5]  J. Logue,et al.  Monthly and annual averages of rainfall for Ireland 1941-1970 , 1977 .

[6]  D. K. Butt Solar and Terrestrial Radiation , 1978 .

[7]  Frederick K. Lutgens The atmosphere , 2018, Physics to a Degree.

[9]  Lawrence Dingman,et al.  Elevation: a major influence on the hydrology of New Hampshire and Vermont, USA / L'altitude exerce une influence importante sur l'hydrologie du New Hampshire et du Vermont, Etats-Unis , 1981 .

[10]  Thomas D. Brock,et al.  Calculating solar radiation for ecological studies , 1981 .

[11]  C. Obled,et al.  Objective analyses and mapping techniques for rainfall fields: An objective comparison , 1982 .

[12]  M. Iqbal An introduction to solar radiation , 1983 .

[13]  G. Campbell,et al.  On the relationship between incoming solar radiation and daily maximum and minimum temperature , 1984 .

[14]  F. Forrestal,et al.  Monthly and annual averages of rainfall for Ireland 1961-1990 , 1984 .

[15]  J. Salas,et al.  A COMPARATIVE ANALYSIS OF TECHNIQUES FOR SPATIAL INTERPOLATION OF PRECIPITATION , 1985 .

[16]  P. Burrough Principles of Geographical Information Systems for Land Resources Assessment , 1986 .

[17]  Ramakrishna R. Nemani,et al.  Extrapolation of synoptic meteorological data in mountainous terrain and its use for simulating forest evapotranspiration and photosynthesis , 1987 .

[18]  J. Hamilton,et al.  Objective analysis of monthly climatological fields of temperature, sunshine, rainfall percentage and rainfall amount , 1988 .

[19]  S. Running,et al.  A general model of forest ecosystem processes for regional applications I. Hydrologic balance, canopy gas exchange and primary production processes , 1988 .

[20]  S. Dingman,et al.  Application of kriging to estimating mean annual precipitation in a region of orographic influence , 1988 .

[21]  Gordon B. Bonan,et al.  A computer model of the solar radiation, soil moisture, and soil thermal regimes in boreal forests , 1989 .

[22]  Jeff Dozier,et al.  Topographic distribution of clear‐sky radiation over the Konza Prairie, Kansas , 1990 .

[23]  E. Rastetter,et al.  Potential Net Primary Productivity in South America: Application of a Global Model. , 1991, Ecological applications : a publication of the Ecological Society of America.

[24]  L. Hamilton 217-249 inRegression with Graphics: A Second Course in Applied Statistics , 1991 .

[25]  A. Flint,et al.  Precipitation Estimation in Mountainous Terrain Using Multivariate Geostatistics. Part I: Structural Analysis , 1992 .

[26]  J. Aber,et al.  A strategy for the regional analysis of the effects of physical and chemical climate change on biogeochemical cycles in northeastern (U.S.) forests , 1993 .

[27]  J. M. Ellis,et al.  A Spatial Model of Atmospheric Deposition for the Northeastern U.S. , 1993, Ecological applications : a publication of the Ecological Society of America.

[28]  S. Running,et al.  Validating Diurnal Climatology Logic of the MT-CLIM Model Across a Climatic Gradient in Oregon , 1994 .

[29]  C. Daly,et al.  A Statistical-Topographic Model for Mapping Climatological Precipitation over Mountainous Terrain , 1994 .

[30]  P. Reich,et al.  Predicting the effects of climate change on water yield and forest production in the northeastern United States , 1995 .

[31]  N. T. Kottegoda,et al.  Identification and calibration of spatial correlation patterns of rainfall , 1995 .

[32]  Lars Eklundh,et al.  Rapid Generation of Digital Elevation Models from Topographic Maps , 1995, Int. J. Geogr. Inf. Sci..

[33]  J. Aber,et al.  Predicting the relative sensitivity of forest production in Ireland to site quality and climate change , 1998 .