| 870 | |
| 871 | |
| 872 | |---------------- |
| 873 | {{{#!td style="vertical-align:top;width: 150px" |
| 874 | [=#large_scale_forcing_ug '''large_scale_forcing_ug''']// |
| 875 | (time,z) |
| 876 | }}} |
| 877 | {{{#!td style="vertical-align:top;width: 50px" |
| 878 | NC_FLOAT |
| 879 | }}} |
| 880 | {{{#!td style="vertical-align:top;width: 50px" |
| 881 | none |
| 882 | }}} |
| 883 | {{{#!td |
| 884 | Large-scale forcing data for the geostrophic wind component in x-direction. |
| 885 | Requires cyclic boundary conditions as well as [../../inipar#large_scale_forcing large_scale_forcing] = .T. to become effective. |
| 886 | }}} |
| 887 | |---------------- |
| 888 | {{{#!td style="vertical-align:top;width: 150px" |
| 889 | [=#large_scale_forcing_vg '''large_scale_forcing_vg''']// |
| 890 | (time,z) |
| 891 | }}} |
| 892 | {{{#!td style="vertical-align:top;width: 50px" |
| 893 | NC_FLOAT |
| 894 | }}} |
| 895 | {{{#!td style="vertical-align:top;width: 50px" |
| 896 | none |
| 897 | }}} |
| 898 | {{{#!td |
| 899 | Large-scale forcing data for the geostrophic wind component in y-direction. |
| 900 | Requires cyclic boundary conditions as well as [../../inipar#large_scale_forcing large_scale_forcing] = .T. to become effective. |
| 901 | }}} |
| 902 | |---------------- |
| 903 | {{{#!td style="vertical-align:top;width: 150px" |
| 904 | [=#large_scale_forcing_sub_w '''large_scale_forcing_sub_w''']// |
| 905 | (time,z) |
| 906 | }}} |
| 907 | {{{#!td style="vertical-align:top;width: 50px" |
| 908 | NC_FLOAT |
| 909 | }}} |
| 910 | {{{#!td style="vertical-align:top;width: 50px" |
| 911 | none |
| 912 | }}} |
| 913 | {{{#!td |
| 914 | Large-scale forcing data for the subsidence velocity. |
| 915 | Requires cyclic boundary conditions as well as [../../inipar#large_scale_forcing large_scale_forcing] = .T. to become effective. |
| 916 | }}} |
| 917 | |---------------- |
| 918 | {{{#!td style="vertical-align:top;width: 150px" |
| 919 | [=#large_scale_forcing_adv_lpt '''large_scale_forcing_adv_lpt''']// |
| 920 | (time,z) |
| 921 | }}} |
| 922 | {{{#!td style="vertical-align:top;width: 50px" |
| 923 | NC_FLOAT |
| 924 | }}} |
| 925 | {{{#!td style="vertical-align:top;width: 50px" |
| 926 | none |
| 927 | }}} |
| 928 | {{{#!td |
| 929 | Large-scale forcing data for the advection tendency of potential temperature. |
| 930 | Requires cyclic boundary conditions as well as [../../inipar#large_scale_forcing large_scale_forcing] = .T. to become effective. |
| 931 | }}} |
| 932 | |---------------- |
| 933 | {{{#!td style="vertical-align:top;width: 150px" |
| 934 | [=#large_scale_forcing_adv_qv '''large_scale_forcing_adv_qv''']// |
| 935 | (time,z) |
| 936 | }}} |
| 937 | {{{#!td style="vertical-align:top;width: 50px" |
| 938 | NC_FLOAT |
| 939 | }}} |
| 940 | {{{#!td style="vertical-align:top;width: 50px" |
| 941 | none |
| 942 | }}} |
| 943 | {{{#!td |
| 944 | Large-scale forcing data for the advection tendency of mixing ratio. |
| 945 | Requires cyclic boundary conditions as well as [../../inipar#large_scale_forcing large_scale_forcing] = .T. to become effective. |
| 946 | }}} |
| 947 | |
| 948 | |
| 949 | |
| 950 | |
| 951 | |