Hi all!
I want to echo and add to Oscar's question about understanding the final channel outflow, vs 'water yield' and other outputs, and see if anyone else out there can assist us both.
I have a SWAT+ model that is giving me a 'water yield' (basin_wb_day.txt file) that is far far greater than my channel flo_out once I get them both into the same units (convert channel flo_out in m3/s into mm).
Anyone know how this can be?
I have not added significant channel seepage rates or anything like that.....
I was assuming that the 'water yield' value is what enters the channel from the surface and lateral flows from soils.
HOWEVER it may just be the simple sum of what leaves the surface and soil of every HRU in the model?
If I have lateral flow and some surface flow from my upland LSU HRUs entering my riparian LSU HRUs, rather than going straight to the channel, this water could get further delayed and subject to ET or recharging the riparian aquifer.
If 'water yield' is the simple sum of all HRU outputs individually, and it does not account for the routing of water via the riparian zone, then this may explain why, in my case, the channel flow is a lot lower than the 'water yield' output.
Does anyone know if that is actually what is happening? If so, it would be helpful to clarify that in the documentation.
In answer to Oscar's question on groundwater contributions to streamflow and where to find these, there is a SWAT+ output file aquifer_day.txt which has aquifer to channel flows in it.
However these values are in mm and it is not clear if this is mm as a depth over the entire basin area or mm as a depth over the area of that particular aquifer (in my case upland & riparian).
When there is seepage from the channel, it shows up in the channel_sd_day.txt file, but I don't know if that amount is added to the aquifer and also shows up in the aquifer_day.txt file amounts somewhere (as part of the 'recharge'?) or not... anyone know this?
Thanks,
Julia