“…The idea behind these methods is that temperature measured at particular points can provide information about the temperatures at points where direct measurements are not available. Methods used to interpolate among these measured points to create a smooth spatial surface of temperature, or to estimate temperatures at nearby locations, include kriging, inverse distance weighting methods, regression methods (Vicente-Serrano et al, 2003), an interpolation optimization method (Loubier, 2007), smoothing splines (Luo et al, 1998), and spatial-temporal modeling (Im et al, 2009). Secondary information related to temperature has also been incorporated into these techniques to improve estimation, including such variables as distance to water bodies (Im et al, 2009), topographic and geographic variables such as elevation, longitude and latitude (Vicente-Serrano et al, 2003), solar radiation (Ninyerola et al, 2000), quantitative climate/meteorological model predictions (Degaetano and Belcher, 2006) and satellite-derived information such as land surface temperature (Vogt et al, 1997).…”