Comparing two spatial variables with the probability of agreement
Jonathan Acosta, Ronny Vallejos, Aaron M. Ellison, Felipe Osorio, Mario de Castro
TL;DR
This work extends the probability of agreement (PA) from scalar comparisons to spatial and spatiotemporal settings by defining PA as a function of spatial lag (and temporal lag in the spatiotemporal case). It derives closed-form PA expressions under Gaussian assumptions and common covariance families (e.g., Matérn, Wendland), and proves monotonic decay of PA with lag under suitable conditions. Estimation uses plug-in parameters with the delta method to obtain asymptotic uncertainty, enabling confidence intervals and hypothesis tests, demonstrated through simulations and a PhenoCam-based forest imagery example. The results show PA robustly captures practical agreement patterns across space and time, offering a tool to quantify and test spatial-temographic similarity in ecological and remote-sensing applications.
Abstract
Computing the agreement between two continuous sequences is of great interest in statistics when comparing two instruments or one instrument with a gold standard. The probability of agreement (PA) quantifies the similarity between two variables of interest, and it is useful for accounting what constitutes a practically important difference. In this article we introduce a generalization of the PA for the treatment of spatial variables. Our proposal makes the PA dependent on the spatial lag. As a consequence, for isotropic stationary and nonstationary spatial processes, the conditions for which the PA decays as a function of the distance lag are established. Estimation is addressed through a first-order approximation that guarantees the asymptotic normality of the sample version of the PA. The sensitivity of the PA is studied for finite sample size, with respect to the covariance parameters. The new method is described and illustrated with real data involving autumnal changes in the green chromatic coordinate (Gcc), an index of "greenness" that captures the phenological stage of tree leaves, is associated with carbon flux from ecosystems, and is estimated from repeated images of forest canopies.
