| 404 | | ||[=#PA0345 PA0345] ||uv_heights(1) must be 0.0|| || |
| 405 | | ||[=#PA0346 PA0346] ||u_profile(1) and v_profile(1) must be 0.0|| || |
| | 404 | ||[=#PA0345 PA0345] ||uv_heights(1) must be 0.0 || || |
| | 405 | ||[=#PA0346 PA0346] ||u_profile(1) and v_profile(1) must be 0.0 || || |
| | 406 | ||[=#PA0347 PA0347] ||maxtry > 40 in Rosenbrock method ||Error may appear if curvature and solution effects are included in the calculation of droplet growth by condensation (see [../inipar#curvature_solution_effects curvature_solution effects]. \\ \\It means that the Rosenbrock method, used for integrating the stiff droplet growth equation, was unable to find an internal timestep which gives a sufficiently small truncation error within 40 tries. \\ \\So far, this problem has not appeared. It might happen if some of the cloud physics parameters, which determine the growth by condensation, are given unrealistic values or if the droplet radius is extremely small. || |
| | 407 | ||[=#PA0348 PA0348] ||zero stepsize in Rosenbrock method ||Error may appear if curvature and solution effects are included in the calculation of droplet growth by condensation (see [../inipar#curvature_solution_effects curvature_solution effects]. \\ \\It means that within the Rosenbrock method, used for integrating the stiff droplet growth equation, the internal timestep has become zero, so that the integration cannot be performed. \\ \\So far, this problem has not appeared. It might happen if some of the cloud physics parameters, which determine the growth by condensation, are given unrealistic values or if the droplet radius is extremely small. || |
