Changes between Version 313 and Version 314 of doc/app/runtime_parameters

Timestamp:

Dec 19, 2019 1:24:49 PM (6 years ago)

Author:

oliver.maas

Comment:

--

doc/app/runtime_parameters

@@ -124 +124 @@
 ||v ||v-component of the velocity ||m/s || ||
 ||w ||w-component of the velocity ||m/s || ||
-||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 w_av*q_av from wq_av ||m/s || ||
+||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.'' ||
 ||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 ||
 ||wtheta ||w-component of the velocity ||m/s || ||