1:3.4.3.2 Solar Radiation
The continuity equation relates average daily solar radiation adjusted for wet or dry conditions to the average daily solar radiation for the month:
μradmon∗daystot=μWradmon∗dayswet+μDradmon∗daysdry 1:3.4.19
where μradmon is the average daily solar radiation for the month (MJ m−2), daystot are the total number of days in the month, μWradmon is the average daily solar radiation of the month on wet days (MJ m−2), dayswet are the number of wet days in the month, μDradmon is the average daily solar radiation of the month on dry days (MJ m−2), and daysdry are the number of dry days in the month.
The wet day average solar radiation is assumed to be less than the dry day average solar radiation by some fraction:
μWradmon=bR∗μDradmon 1:3.4.20
where μWradmon is the average daily solar radiation of the month on wet days (MJ m−2), μDradmon is the average daily solar radiation of the month on dry days (MJ m−2), and bR is a scaling factor that controls the degree of deviation in solar radiation caused by the presence or absence of precipitation. The scaling factor, bR, is set to 0.5 in SWAT+.
To calculate the dry day average solar radiation, equations 1:3.4.19 and 1:3.4.20 are combined and solved for μDradmon:
μDradmon=bR∗dayswet+daysdryμradmon∗daystot 1:3.4.21
Incorporating the modified values into equation 1:3.4.12, SWAT+ calculated the solar radiation on a wet day using the equation:
Hday=μWradmon+χi(3)∗σradmon 1:3.4.22
and the solar radiation on a dry day using the equation:
Hday=μDradmon+χi(3)∗σradmon 1:3.4.23
Table 1:3-4: SWAT+ input variables that pertain to generation of temperature and solar radiation.
σmxmon: standard deviation for maximum air temperature in month (°C)
tmpstdmx
tmp_max_sd
σmnmon: standard deviation for minimum air temperature in month (°C)
tmpstdmn
tmp_min_sd
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