| | 665 | }}} |
| | 666 | [[BR]] |
| | 667 | |
| | 668 | [=#phys '''Physics:]\\ |
| | 669 | ||='''Parameter Name''' =||='''[../fortrantypes#FORTRAN\\Type FORTRAN]\\[../fortrantypes#FORTRAN\\Type Type]''' =||='''Default Value''' =||='''Explanation''' =|| |
| | 670 | |---------------- |
| | 671 | {{{#!td style="vertical-align:top;width: 150px" |
| | 672 | [=#omega '''omega'''] |
| | 673 | }}} |
| | 674 | {{{#!td style="vertical-align:top;width: 50px" |
| | 675 | R |
| | 676 | }}} |
| | 677 | {{{#!td style="vertical-align:top;width: 75px" |
| | 678 | 7.29212E-5 |
| | 679 | }}} |
| | 680 | {{{#!td |
| | 681 | Angular velocity of the rotating system (in rad s^-1^).\\\\ |
| | 682 | The angular velocity of the earth is set by default. The values of the Coriolis parameters are calculated as:\\\\ |
| | 683 | f = 2.0 * '''omega''' * sin([#phi phi])\\ |
| | 684 | f* = 2.0 * '''omega''' * cos(phi) |
| | 685 | }}} |
| | 686 | |---------------- |
| | 687 | {{{#!td style="vertical-align:top" |
| | 688 | [=#phi '''phi'''] |
| | 689 | }}} |
| | 690 | {{{#!td style="vertical-align:top" |
| | 691 | R |
| | 692 | }}} |
| | 693 | {{{#!td style="vertical-align:top" |
| | 694 | 55.0 |
| | 695 | }}} |
| | 696 | {{{#!td |
| | 697 | Geographical latitude (in degrees).\\\\ |
| | 698 | The value of this parameter determines the value of the Coriolis parameters f and f*, provided that the angular velocity (see [#omega omega]) is non-zero. |
| | 699 | }}} |
| | 700 | |---------------- |
| | 701 | {{{#!td style="vertical-align:top" |
| | 702 | [=#prandtl_number '''prandtl_number'''] |
| | 703 | }}} |
| | 704 | {{{#!td style="vertical-align:top" |
| | 705 | R |
| | 706 | }}} |
| | 707 | {{{#!td style="vertical-align:top" |
| | 708 | 1.0 |
| | 709 | }}} |
| | 710 | {{{#!td |
| | 711 | Ratio of the eddy diffusivities for momentum and heat (K,,m,,/K,,h,,).\\\\ |
| | 712 | For runs with constant eddy diffusivity (see [#km_constant km_constant]), this parameter can be used to assign the Prandtl number (ratio K,,m,, / K,,h,,). |