2006
DOI: 10.1175/bams-87-6-769
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Calculating A Daily Normal Temperature Range That Reflects Daily Temperature Variability

Abstract: By utilizing daily normal ranges, weathercasters and others could better communicate to the public the natural expected variability of day-to-day temperatures-a variability not suggested by normals derived from smoothed trend lines.

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Cited by 17 publications
(9 citation statements)
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“…However, the T r abscissa from the original universal triangle is replaced by the percent of sensible heating (PH). These fractional PH values will actually be the HI‐LUT output, and they will be used for our purposes to determine the partitioning of solar energy into H and LE—which will eventually help us calculate the final HI values themselves—because it is the quantities of vegetation cover and surface soil moisture that primarily dictate this partitioning [ LeMone et al , 2003; Diak et al , 2004; Holder et al , 2006]. Also, in the HI‐LUT, ordered bins of API values are used to replace the former surface moisture availability fraction isopleths.…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…However, the T r abscissa from the original universal triangle is replaced by the percent of sensible heating (PH). These fractional PH values will actually be the HI‐LUT output, and they will be used for our purposes to determine the partitioning of solar energy into H and LE—which will eventually help us calculate the final HI values themselves—because it is the quantities of vegetation cover and surface soil moisture that primarily dictate this partitioning [ LeMone et al , 2003; Diak et al , 2004; Holder et al , 2006]. Also, in the HI‐LUT, ordered bins of API values are used to replace the former surface moisture availability fraction isopleths.…”
Section: Methodsmentioning
confidence: 99%
“…Over the past several years, much attention has been paid to the modulating effects of certain land surface characteristics on the thermodynamic profile within the convective boundary layer (CBL). In particular, surface vegetation and soil moisture have been examined with respect to their ability to partition incoming solar radiation, or insolation, into sensible and latent heating, “H” and “LE,” respectively [ Segal et al , 1988; LeMone et al , 2003; Diak et al , 2004; Holder et al , 2006]. The influence this effect has upon the preferential location of shallow and deep convection has also been studied in great detail [ Rabin et al , 1990; Mahrt et al , 1994; Hong et al , 1995; Segal et al , 1995; Crook , 1996; Rabin and Martin , 1996; Pielke , 2001; Dissing and Verbyla , 2003; Ek and Holtslag , 2004; Kustas et al , 2005; Holt et al , 2006; Childs et al , 2006].…”
Section: Introductionmentioning
confidence: 99%
“…According to Holder et al [28], the choice of sigma value depends on the data set. 95.46% of the sensor data will fall within 2 standard deviation of the mean with 2 sigma consideration.…”
Section: Network and System Architecturementioning
confidence: 99%
“…In temperature collection WSN we consider the normal temperature range is T= 8 to 10 degree centigrade based on the Gaussian distributing with 1 sigma based on the approach taken by holder el at [6] , and ~T means the temperature is out of range and consider the node M is misbehaved. So, the frame of discernment consists of two probabilities concerning the attacker node A: Θ = {T, ~T}.…”
Section: Evaluation In Wsnmentioning
confidence: 99%