Calculates the total solar energy received over a full Martian day on a horizontal surface.
Obtained by integrating global hourly insolation from sunrise to sunset.
Usage
H_h(
Ls,
phi,
longitude,
tau,
al = albedo(latitude = phi, longitude = longitude, tau = tau)
)
Arguments
- Ls
Areocentric longitude [deg]
- phi
Planetary latitude [deg]
- longitude
Planetary longitude [deg]
- tau
Atmospheric optical depth (dimensionless)
- al
Surface albedo (dimensionless, 0-1). If not provided, calculated from latitude, longitude, and tau
Value
Global daily insolation [Wh/m²-day]