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Any observations located outside the grid box, regardless of their proximity to the boundary of the grid box, will not affect the interpolated value of the grid box.
Ignores the influence of stations outside each grid box.
All heatwaves are calculated at the grid box level.
Equations describing conservation of mass, energy, and other processes are solved at each grid box.
Observations are averaged over large distances, reducing variability within each grid box.
Regional IDF curves at the grid box and the station scales are proposed.
When the weaver function is used to interpolate to an equally spaced longitude/latitude grid, only the observations located within each grid box are used to calculate the interpolated value for that grid box.
Parker and N.A. Rayner, 2001: Adjusting for sampling density in grid box land and ocean surface temperature time series.
The value of each grid box is found by computing a simple arithmetic average of the observations.
The "false setweave" command tells the function to perform an interpolation by averaging the stations in each grid box.
This results in an annual value per characteristic for both experiments at each land-based grid box.
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