Changes between Version 205 and Version 206 of doc/tec/changelog_2018


Ignore:
Timestamp:
Nov 29, 2012 5:00:17 PM (12 years ago)
Author:
franke
Comment:

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  • doc/tec/changelog_2018

    v205 v206  
    1111
    1212||='''Date'''  =||='''Author'''  =||='''svn\\Revision'''  =||='''Last\\Release'''  =||='''Type''' =||='''Description''' =||
     13|----------------
     14{{{#!td style="vertical-align:top;width: 50px"
     1529/11/12
     16}}}
     17{{{#!td style="vertical-align:top;width: 50px"
     18TR
     19}}}
     20{{{#!td style="vertical-align:top;width: 75px"
     21r1071
     22}}}
     23{{{#!td style="vertical-align:top"
     243.9
     25}}}
     26{{{#!td style="vertical-align:top"
     27N, C, B
     28}}}
     29{{{#!td style="vertical-align:top"
     30'''New:'''
     31Ventilation effect for evaporation of large cloud droplets included. (lpm_droplet_condensation)
     32
     33'''Changed:''' \\
     34Removed unnecessary calculations in lpm_droplet_condensation.
     35
     36Calculation of droplet growth due to collisions now uses collision-coalescence formulation proposed by Wang in case of Hall and Wang kernel. (lpm_droplet_collision)
     37
     38'''Bugfixes:'''\\
     39Collision efficiencies for Hall kernel should not be negative. (lpm_collision_kernels)
     40
     41Surface tension for calculation of cloud droplet condensation/evaporation using Rosenbrock method corrected. (lpm_droplet_condensation)
     42
     43Check for unreasonable results included in calculation of Rosenbrock method since unreasonable results may occur if external conditions significantly change. For the same reason the first internal time step in Rosenbrock method should be < 1.0E02 in case of evaporation. (lpm_droplet_condensation)
     44
     45Message identifiers added. (lpm_droplet_collision)
     46}}}
    1347|----------------
    1448{{{#!td style="vertical-align:top;width: 50px"