Changes between Version 314 and Version 315 of doc/app/runtime_parameters


Ignore:
Timestamp:
Dec 19, 2019 1:31:19 PM (6 years ago)
Author:
oliver.maas
Comment:

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  • doc/app/runtime_parameters

    v314 v315  
    124124||v ||v-component of the velocity ||m/s || ||
    125125||w ||w-component of the velocity ||m/s || ||
    126 ||wq ||product of w and q. Output of wq_av can be used to calculate the resolved turbulent water flux according to the temporal eddy covariance method by substracting the advective water flux (product of w_av and q_av) from wq_av. ||m/s ||requires [[../inipar#humidity|humidity]] = ''.T.'' ||
     126||wq ||product of w and q, output of wq_av can be used to calculate the resolved turbulent water flux according to the temporal eddy covariance method by substracting the advective water flux (product of w_av and q_av) from wq_av. ||m/s ||requires [[../inipar#humidity|humidity]] = ''.T.'' ||
    127127||wspeed_10m* ||10-m wind speed (estimated from logarithmic interpolation if the 10m level is below the first prognostic grid point, else interpolated between two vertical levels)||m/s ||only horizontal cross section is allowed ||
    128 ||wtheta ||w-component of the velocity ||m/s || ||
    129 ||wu || ||m/s || ||
    130 ||wv || ||m/s || ||
     128||wtheta ||product of w and theta, refer to wq ||K m/s || ||
     129||wu ||product of w and u, refer to wq ||m^2/s^2 || ||
     130||wv ||product of w and v, refer to wq ||m^2/s^2 || ||
    131131||z0* ||roughness length ||m || ||
    132132||z0h* ||roughness length for scalar quantities ||m || ||