Figure S4:

Details: bathymetry and Forcing conditions as in Ulloa et al. (2022):

LES:
Ulloa, H. N., Ramón, C. L., Doda, T., Wüest, A., & Bouffard, D. (2022). 
Development of overturning circulation in sloping waterbodies due to surface cooling. 
Journal of Fluid Mechanics, 930, A18. https://doi.org/doi:10.1017/jfm.2021.883

MITgcm: run 9 in Table S1 in Supporting information

Averaging time period: 18-24 h (quasi-steady state)

Data displayed in Fig. S4
1D files (NetCDF): Time-Averaged variables in the littoral region 
*****************************************************
Name   X_LittoralTransect.nc		X = LES (Ulloa et al., 2022) or MITgcm (run 9 in SI)

output variables:
x           	x-Distance (m)						1D
h_TS		TS thickneess (m)					1D
u_TS		TS average velocity (m/s)				1D
u_Top		Top-layer average velocity (m/s)			1D
q_TS	   	Unit-width discharges (m^2/s)				1D
T_TS		TS temperature (°C)					1D
T_Top		Top-layer temperature(°C)				1D
gprime_TS	Reduced gravity (m s^-^2)				1D

**********************************************************

Extra: 2D files (NetCDF): Time-averaged T, u and w values for the whole 2D domain
************************************************************************
Name   X_WholeDomain.nc		X = LES (Ulloa et al., 2022) or MITgcm (run 9 in SI)

output variables:
x           	x-Distance (m)						1D
z           	Depth (m)						1D
T		Temperature (°C)					2D [z,x]
u_x		Velocity in x-direction (m/s)				2D [z,x]
w		Vertical velocity (m/s)					2D [z,x]










