Changes between Version 480 and Version 481 of doc/tec/changelog_2018


Ignore:
Timestamp:
Oct 26, 2015 4:28:57 PM (10 years ago)
Author:
maronga
Comment:

--

Legend:

Unmodified
Added
Removed
Modified
  • doc/tec/changelog_2018

    v480 v481  
    1111
    1212||='''Date'''  =||='''Author'''  =||='''svn\\Revision'''  =||='''Last\\Release'''  =||='''Type''' =||='''Description''' =||
     13|----------------
     14{{{#!td style="vertical-align:top;width: 50px"
     1526/10/15
     16}}}
     17{{{#!td style="vertical-align:top;width: 50px"
     18BM
     19}}}
     20{{{#!td style="vertical-align:top;width: 75px"
     21r1691
     22}}}
     23{{{#!td style="vertical-align:top"
     244.0
     25}}}
     26{{{#!td style="vertical-align:top"
     27B,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}}}
    1356|----------------
    1457{{{#!td style="vertical-align:top;width: 50px"