Introduction : This calculator demonstrates an example equation of motion - temperature advection in one direction -- as an example of the type of equations used in numerical weather prediction. This equation is an example of a "finite-difference" equation, which is loosely defined as:
New value = old value + change
For example, In this calculator, you have seven input values:
- the potential temperature at the beginning of the forecast (for example, time = 0)
- the potential temperature in the box of interest at some change in time (dt) later, in this example at time = 10 minutes
- the potential temperature in the "western" box at the latest time
- the potential temperature in the "eastern" box at the latest time
- the wind speed (U) in meters/sec (changed to km/min automatically by the calculator)
- the width of the box in the x-direction (dx), in meters
- the time step (dt)
The algorithm for the the cumulative daytime heating is:

For example, a sample scenario (the one modeled by this calculator) is shown below:
In this scenario, we are looking at 10-minute intervals, with the potential temperatures shown in underneath each of the grid boxes. In this schematic, i=3,4, and 5 (moving across from left to right), and k=4. We are interested in forecasting the potential temperature (in degrees C) at time=20 minutes for Gridbox 44. We know that the temperature at t=10 minutes is 15.1 degrees, and we wish to know the temperature 10 minutes later. The windspeed from Gridbox 34 going into 44 is 10 m/s.
In the algorithm above, t= 10 minutes, t+dt= 20 minutes, t-dt = 0 minutes, i=4, k=4.
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Temperature Advection Calculator
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