- Problem #1 - The meteorology error tutorial section showed results only using the NARR and WRF27UW data. Add the ERA40 and WRF27 data to the graphic.
- Hint - Retrieve traj_fwrd_control.txt to get started.
- Solution - Note that the first trajectory in the display list determines the image domain. The ERA40 is the northern most trajectory while the NARR is the southern most trajectory.
- Problem #2 - Determine the sensitivity of the trajectories to the integration time step by comparing the calculation using the default time step with an arbitrary one set to a fixed value equal to the meteorological data interval. Computational differences can be enhanced using the 3 km resolution WRF data which is provided at a 15 min temporal resolution.
- Hint - Define the WRF03 data file and compute the trajectory (without using SETUP.CFG). Then open the advanced menu and set the time step to 15 minutes. After changing the name of the trajectory endpoints file, rerun the model.
- Solution - Although trajectories using the smaller domain 3 km data terminate near the Ohio-Pennsylvania border, it is already clear that the mid-boundary layer trajectories are starting to become different from each other. The faster trajectory (red) was calculated with the variable time step while the slower trajectory (blue) used the fixed 15 min time step. The longer fixed time step forces the calculation to skip over grid points. Unlike other modeling approaches, Lagrangian calculations will not fail if the time step criterion is violated.