143 | | Parameter to consider solution and curvature effects on the equilibrium vapor pressure of cloud droplets. For the initialization of the corresponding dry aerosol spectrum, see [#init_aerosol_probabilistic init_aerosol_probabilistic].In this case, the radius growth equation is a stiff o.d.e, which is integrated in time using a Rosenbrock method (see Numerical Recipes in FORTRAN, 2nd Edition, p.731). '''curvature_solution_effects''' = ''.T.'' may significantly increase CPU time of jobs. |
| 143 | Parameter to consider solution and curvature effects on the equilibrium vapor pressure of cloud droplets. For the initialization of the corresponding dry aerosol spectrum, see [#init_aerosol_probabilistic init_aerosol_probabilistic]. In this case, the radius growth equation is a stiff o.d.e, which is integrated in time using a Rosenbrock method (see Numerical Recipes in FORTRAN, 2nd Edition, p.731). '''curvature_solution_effects''' = ''.T.'' may significantly increase CPU time of jobs. |
| 383 | [=#n1 '''n1'''] |
| 384 | }}} |
| 385 | {{{#!td style="vertical-align:top" |
| 386 | R |
| 387 | }}} |
| 388 | {{{#!td style="vertical-align:top" |
| 389 | 100.0 |
| 390 | }}} |
| 391 | {{{#!td |
| 392 | Number concentration of the first log-normal distribution steering the initial dry aerosol spectrum. See [#init_aerosol_probabilistic init_aerosol_probabilistic] for more details. |
| 393 | |
| 394 | '''n1''' can be given in arbitrary units, since the final number concentration is still steered via [#initial_weighting_factor]. |
| 395 | }}} |
| 396 | |---------------- |
| 397 | {{{#!td style="vertical-align:top" |
| 398 | [=#n2 '''n2'''] |
| 399 | }}} |
| 400 | {{{#!td style="vertical-align:top" |
| 401 | R |
| 402 | }}} |
| 403 | {{{#!td style="vertical-align:top" |
| 404 | 0.0 |
| 405 | }}} |
| 406 | {{{#!td |
| 407 | Number concentration of the second log-normal distribution steering the initial dry aerosol spectrum. See [#n1 n1]. |
| 408 | }}} |
| 409 | |---------------- |
| 410 | {{{#!td style="vertical-align:top" |
| 411 | [=#n3 '''n3'''] |
| 412 | }}} |
| 413 | {{{#!td style="vertical-align:top" |
| 414 | R |
| 415 | }}} |
| 416 | {{{#!td style="vertical-align:top" |
| 417 | 0.0 |
| 418 | }}} |
| 419 | {{{#!td |
| 420 | Number concentration of the third log-normal distribution steering the initial dry aerosol spectrum. See [#n1 n1]. |
| 421 | }}} |
| 422 | |---------------- |
| 423 | {{{#!td style="vertical-align:top" |
| 648 | [=#rm1 '''rm1'''] |
| 649 | }}} |
| 650 | {{{#!td style="vertical-align:top" |
| 651 | R |
| 652 | }}} |
| 653 | {{{#!td style="vertical-align:top" |
| 654 | 0.05E-6 |
| 655 | }}} |
| 656 | {{{#!td |
| 657 | Mode radius of the first log-normal distribution steering the initial dry aerosol spectrum. See [#init_aerosol_probabilistic init_aerosol_probabilistic] for more details. |
| 658 | |
| 659 | '''rm1''' should be entered in meters. |
| 660 | }}} |
| 661 | |---------------- |
| 662 | {{{#!td style="vertical-align:top" |
| 663 | [=#rm2 '''rm2'''] |
| 664 | }}} |
| 665 | {{{#!td style="vertical-align:top" |
| 666 | R |
| 667 | }}} |
| 668 | {{{#!td style="vertical-align:top" |
| 669 | 0.05E-6 |
| 670 | }}} |
| 671 | {{{#!td |
| 672 | Mode radius of the second log-normal distribution steering the initial dry aerosol spectrum. See [#rm1 rm1]. |
| 673 | }}} |
| 674 | |---------------- |
| 675 | {{{#!td style="vertical-align:top" |
| 676 | [=#rm3 '''rm3'''] |
| 677 | }}} |
| 678 | {{{#!td style="vertical-align:top" |
| 679 | R |
| 680 | }}} |
| 681 | {{{#!td style="vertical-align:top" |
| 682 | 0.05E-6 |
| 683 | }}} |
| 684 | {{{#!td |
| 685 | Mode radius of the third log-normal distribution steering the initial dry aerosol spectrum. See [#rm1 rm1]. |
| 686 | }}} |
| 687 | |---------------- |
| 688 | {{{#!td style="vertical-align:top" |