Calculates the diffuse solar energy (scattered by atmospheric dust) received over a full Martian day on an inclined surface. Obtained by integrating diffuse irradiance from sunrise to sunset.
H_di(
Ls,
phi,
longitude,
tau,
al = albedo(latitude = phi, longitude = longitude, tau = tau),
beta,
gamma_c
)Diffuse daily insolation on inclined surface [Wh/m²-day]
Areocentric longitude [deg]
Planetary latitude [deg]
Planetary longitude [deg]
Atmospheric optical depth (dimensionless)
Surface albedo (dimensionless, 0-1). If not provided, calculated from latitude, longitude, and tau
Surface tilt/slope angle from horizontal [deg]
Surface azimuth angle [deg]. Zero facing equator, east negative, west positive (-180 to +180)