Journal Article10.1080/02723646.1981.10642213
On the validation of models
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TL;DR: In this paper, it is suggested that the correlation coefficieness between observed and simulated variates is not as good as observed variates, and that correlation can be improved.
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Abstract: Traditional methods of evaluating geographic models by statistical comparisons between observed and simulated variates are criticized. In particular, it is suggested that the correlation coefficien...
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A modeling study on the hydrodynamics of a coastal embayment occupied by mussel farms (Ria de Ares-Betanzos, NW Iberian Peninsula)
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References
Variations of Box Plots
TL;DR: Box plots as mentioned in this paper display batches of data and use five values from a set of data: the extremes, the upper and lower hinges (quartiles), and the median, commonly used for exploratory data analysis and in preparing visual summaries.
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An improved equation for estimating long-wave radiation from the atmosphere
TL;DR: In this paper, an equation that predicts downcoming long-wave radiation from clear skies on the basis of screen air temperature and vapor pressure has been developed, which fits measured data at extremes of temperature and humidity better than existing equations, and exhibits comparable accuracy at intermediate values.
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An Empirical Method for the Spatial Interpolation of Monthly Precipitation within California
Cort J. Willmott,Donald E. Wicks +1 more
TL;DR: In this paper, an empirical method for interpolating monthly precipitation totals within California is described and evaluated using 120 monthly precipitation total observed from 1961-1970 at each of 90 randomly selected stations in California and a P-mode principal components analysis of a co-variance matrix, four independent sources of precipitation variability were identified and quantitatively paraphrased.
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A numerical solar radiation model based on standard meteorological observations
M.A. Atwater,J.T. Ball +1 more
TL;DR: In this article, a numerical model based on standard meteorological data, as described above, can be used to extend the data base for design purposes, and the model is used to compute the amount of direct solar flux.
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Fitting straight lines when both variables are subject to error.
TL;DR: In this paper, the maximum likelihood estimators of α and β under functional and structural models are discussed, and the least square procedure is also considered, leading to a quadratic equation which can be solved to give an estimate of β.
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