| ... | @@ -28,7 +28,7 @@ k_{d} = 0.24 + 0.036 \cdot TPM |
... | @@ -28,7 +28,7 @@ k_{d} = 0.24 + 0.036 \cdot TPM |
|
|
|
|
|
|
|
Where the background extinction is 0.24 m<sup>-1</sup> (including the extinction due to dissolved humic substances) and TPM is the concentration of suspended sediment particles (mg l<sup>-1</sup>)
|
|
Where the background extinction is 0.24 m<sup>-1</sup> (including the extinction due to dissolved humic substances) and TPM is the concentration of suspended sediment particles (mg l<sup>-1</sup>)
|
|
|
|
|
|
|
|
The average light ($`I_{avg}`$) is calculated by integration of the function over the whole water column divided over the waterdepth.
|
|
The average light ($`I_{avg}`$) is calculated by integration of the function over the whole water column divided over the water depth.
|
|
|
|
|
|
|
|
```math
|
|
```math
|
|
|
I_{avg} = \frac{ \int_{z=0}^{z=Depth} \cdot I_{z} \cdot dz}{Depth}
|
|
I_{avg} = \frac{ \int_{z=0}^{z=Depth} \cdot I_{z} \cdot dz}{Depth}
|
| ... | | ... | |