You signed in with another tab or window. Reload to refresh your session.You signed out in another tab or window. Reload to refresh your session.You switched accounts on another tab or window. Reload to refresh your session.Dismiss alert
NRL is working heavily on the high-altitude physics in NEPTUNE using CCPP. A question came up for which I don't have a good answer.
In the high-altitude configuration, there are two non-orographic gravity wave drag schemes active at the same time. The "ordinary" non-orographic GWD scheme from the "lower" atmosphere, and the high-altitude version from the high-altitude physics. Both are active at the same time, and the high-altitude version runs over the entire column, i.e. including the lower atmosphere where the ordinary scheme is active. It is necessary to keep the standard names for these quantities separate so that they can be treated as different tendencies in the tendencies array etc.
What do we do in this case? We were trying to find physically meaningful names. The qualifier "in_thermosphere", for example, doesn't make sense since the HA version runs over the entire column. Should we add a qualifier to the "due_to" descriptor? That is,
I am not sure I like this, because it somewhat still suggests that this is something in the upper atmosphere, but at least it allows for the interpretation that it can influence the lower atmosphere.
The text was updated successfully, but these errors were encountered:
At today's framework meeting we discussed the potential of being more specific about "nonorographic". For example, if this is coming from magnetic high-altitude processes, can we call it cumulative_change_of_x_wind_due_to_magnetic_gravity_wave_drag?
At today's framework meeting we discussed the potential of being more specific about "nonorographic". For example, if this is coming from magnetic high-altitude processes, can we call it cumulative_change_of_x_wind_due_to_magnetic_gravity_wave_drag?
In this case, we would also replace the existing cumulative_change_of_x_wind_due_to_nonorographic_gravity_wave_drag with the actual physical process XYZ behind it: cumulative_change_of_x_wind_due_to_XYZ_gravity_wave_drag
Unfortunately, life is not so easy. I checked with the NRL developers, and the actual processes behind the non-orographic GWD from standard- and high-altitude physics are indeed the same or at least overlapping. We are trying to come up with something better.
NRL is working heavily on the high-altitude physics in NEPTUNE using CCPP. A question came up for which I don't have a good answer.
In the high-altitude configuration, there are two non-orographic gravity wave drag schemes active at the same time. The "ordinary" non-orographic GWD scheme from the "lower" atmosphere, and the high-altitude version from the high-altitude physics. Both are active at the same time, and the high-altitude version runs over the entire column, i.e. including the lower atmosphere where the ordinary scheme is active. It is necessary to keep the standard names for these quantities separate so that they can be treated as different tendencies in the tendencies array etc.
What do we do in this case? We were trying to find physically meaningful names. The qualifier "in_thermosphere", for example, doesn't make sense since the HA version runs over the entire column. Should we add a qualifier to the "due_to" descriptor? That is,
I am not sure I like this, because it somewhat still suggests that this is something in the upper atmosphere, but at least it allows for the interpretation that it can influence the lower atmosphere.
The text was updated successfully, but these errors were encountered: