Figure 6:
1D files (NetCDF): Predicted vs. measured unit-width discharges during cooling periods in Rotsee
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Name   FieldVsScaling_DayX.nc		X = Day of year

output time step = 15 min

ouput variables:
time        	time in days from 01/01/2019 00:00:00									1D
qfield		Measured offshore discharges in Rotsee (m^2/s)								1D
qfield_smth	Measured offshore discharges in Rotsee (3h-smoothing, m^2/s)						1D
qc        	Offshore discharges (m^2/s) with convective scaling (Rotsee), a = 0.34 (Mean value)			1D
qc_Up	    	Offshore discharges (m^2/s) with convective scaling (Rotsee), a = 0.36 (upper bound)			1D
qc_down		Offshore discharges (m^2/s) with convective scaling (Rotsee), a = 0.33 (lower bound)			1D
qtotal	    	Offshore discharges, qc + qw  (m^2/s), a= 0.34 [0.33, 0.36], νz = 6.06 × 10‒4 ± 3.6 × 10‒5 m^2 s^-1	1D 
qtotal_Up	Offshore discharges, qc + qw  (m^2/s), upper bound (m^2/s)						1D
qtotal_down	Offshore discharges, qc + qw  (m^2/s), lower bound (m^2/s)						1D
B0		Surface buoyancy flux (W/kg)										1D

Figure 6b shows the time average of qfield, qc and qtotal.

For details of field experiments in Rotsee go to:
Doda, T., Ramón, C. L., Ulloa, H. N., Wüest, A., and Bouffard, D.: Seasonality of density currents induced by differential cooling, 
Hydrol. Earth Syst. Sci., 26, 331–353, https://doi.org/10.5194/hess-26-331-2022, 2022.