| 13 | |---------------- |
| 14 | {{{#!td style="vertical-align:top;width: 50px" |
| 15 | 26/10/15 |
| 16 | }}} |
| 17 | {{{#!td style="vertical-align:top;width: 50px" |
| 18 | BM |
| 19 | }}} |
| 20 | {{{#!td style="vertical-align:top;width: 75px" |
| 21 | r1691 |
| 22 | }}} |
| 23 | {{{#!td style="vertical-align:top" |
| 24 | 4.0 |
| 25 | }}} |
| 26 | {{{#!td style="vertical-align:top" |
| 27 | B,C,N |
| 28 | }}} |
| 29 | {{{#!td style="vertical-align:top" |
| 30 | '''New:''' |
| 31 | * new module {{{surface_layer_fluxes.f90}}} added (replaces {prandtl_fluxes.f90}). PALM now offers three methods to derive the surface fluxes that are steered via the {{{inipar}}} parameter {{{most_method}}}: |
| 32 | |
| 33 | * the "old" method ({{{most_method = 'circular'}}}, which is the fastest method, but inaccurate) |
| 34 | |
| 35 | * a new method based on the evaluation of the Richardson number to derive the Obukhov length by using a Newton iteration algorithm ({{{most_method = 'newton'}}} accurate, but relatively slow) |
| 36 | |
| 37 | * a new method based on the evaluation of the Richardson number to derive the Obukhov length using a lookup-table ({{{most_method = 'lookup'}}} accurate, faster than the Newton iteration method, but slightly slower than the old method) |
| 38 | |
| 39 | '''Changed:''' |
| 40 | * in the course of the implementation of the new surface flux calculations, the following parameters have been changed: |
| 41 | * {{{rif}}} was removed |
| 42 | |
| 43 | * {{{rif_max}}} and {{{rif_min}}} have been renamed to {{{zeta_max}}} and {{{zeta_min}}} ({{{zeta = z_mo/L}}} with {{{z_mo}}} being the height of the constant flux layer, and {{{L}}} being the Obukhov length |
| 44 | |
| 45 | * limits for {{{zeta_max}}} and {{{zeta_min}}} have been changed to allow better representation of free convection and very stable conditions |
| 46 | |
| 47 | * similarity functions for stable conditions has bee altered to allow for very stable conditions |
| 48 | |
| 49 | |
| 50 | '''Bugfix:''' |
| 51 | * Minor formatting corrections |
| 52 | * Calculation of trace gas profiles in RRTMG corrected |
| 53 | * Prognostic equations for skin temperature in land surface model corrected |
| 54 | |
| 55 | }}} |