We have interpolated it onto our model grid to form a 3D conductivity distribution.
This model assumed the hypocentral parameters from D. Zhao (personal communication), and allowed the model grid to extend to the furthest up-dip limit of the upper plate in the Japan trench.
Uniform geological properties and stresses, such as well pumps, are assigned to each cell of the model grid to simulate steady-state or transient flow conditions (USGS 2008; Walter and Whealan 2005).
For this purpose, we regress monthly deseasonalized anomalies of state variables and carbon fluxes at each model grid point to the monthly SAM index considering a lag of 0 to 12 months.
Such 1-dimensional model grids can be used to model repeated finite horizon.
Considerable effort was put into distributing available meteorological station data to the model grids as forcing data.
This study uses a distributed hydrological model, the Grid-to-Grid (G2G), to assess future changes in peak river flows for a range of catchments across the Thames Basin.
In particular, daily temperature forecasts collected from five daily initialization runs were averaged out to obtain a weekly forecast for each model grid point related to the three Italian macro-areas; afterwards, each temperature forecast of the model grid point was once again averaged in order to obtain a single temperature forecast value for each week (12 in total for each area).
where: Zone j,k) is a function of the jth grid cell column and kth grid cell row that returns 1 if model grid (j,k) corresponds to Zone 1, and returns 2 if (j,k) corresponds to Zone 2. q jk * is the modeled extraction rate at model grid location (j,k).
See Figure 2 for definitions of Zones 1 and 2: If Zone j, k = 1, then q jk * α ≤ 400 gpm else q jk * α ≤ 1, 000 gpm (21) where: Zone j,k) is a function of the jth grid cell column and kth grid cell row that returns 1 if model grid (j,k) corresponds to Zone 1, and returns 2 if (j,k) corresponds to Zone 2 q jk * is the modeled extraction rate at model grid location (j,k).
