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Advanced Research WRF (ARW) Technical Note - MMM - University ...

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Figure 7.4: Similar to Fig. 7.3, but with a 2:1 grid-distance ratio.<br />

that are required (briefly described in Fig. 7.5). While the following text details a simulation<br />

with a single coarse-grid and a single fine-grid, this implies no lack of generality when handling<br />

multiple grid levels or multiple grids on the same level.<br />

Nest Instantiation<br />

The fine grid is instantiated as a child of a parent grid at the requested start time. This<br />

initialization is within the integration step for the parent grid, so no child grid can begin if<br />

the parent is not active. To fill in the correct meteorological fields, an initialization routine is<br />

called to horizontally interpolate the coarse-grid data to the fine grid locations using a monotone<br />

interpolation scheme (described in Smolarkiewicz and Grell, 1990) for most fields (i.e., the same<br />

scheme employed for generating the fine grid lateral boundary conditions) and a simple linear<br />

interpolation or averaging scheme for masked or categorical fields. For fields that are masked<br />

with the land/sea background (such as land only fields (e.g., snow), or water only fields (e.g.,<br />

sea ice)), the interpolator needs to know what field defines the template for the masking (such<br />

as the land use category). Part of the automatic code generation handles calling each field with<br />

its associated interpolator.<br />

48

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