I am running a NEON site simulation and noticed a behavior that I do not fully understand.
In a transient simulation, after modifying the soil texture to make the soil more sandy, I found that the soil moisture in the first year decreased quite noticeably. To trace where the water went, I checked several output flux variables, including ET, QOVER, QDRAI, QDRAI_PERCH, and QFLX_SNOW_DRAIN, but I did not see any obvious increase in these fluxes that could explain the magnitude of the soil moisture decline.
I am therefore wondering where this “missing” water may have gone. Are there other important variables or water balance terms that I may have overlooked and should examine?
In a transient simulation, after modifying the soil texture to make the soil more sandy, I found that the soil moisture in the first year decreased quite noticeably. To trace where the water went, I checked several output flux variables, including ET, QOVER, QDRAI, QDRAI_PERCH, and QFLX_SNOW_DRAIN, but I did not see any obvious increase in these fluxes that could explain the magnitude of the soil moisture decline.
I am therefore wondering where this “missing” water may have gone. Are there other important variables or water balance terms that I may have overlooked and should examine?