NPZ-model/Physical-Processes.md

@@ -11,20 +11,19 @@ T_{fac} = e^{( \frac{T-10}{10}\cdot\log(Q_{10}))}
 
 Where T is the ambient water temperature and $`Q_{10}`$ indicates the relative increase in the rate for an increase of the water temperature with 10 °C.
 
-[top](NPZ model/Physical Processes)
-# SinkDet
-The detritus sinks to the sea floor with a constant sinking velocity ($`SinkinRate_{Det}`$)[m d<sup>-1</sup>]. The units of SinkDet is [mmol N m<sup>-2</sup> d<sup>-1</sup>].
-```math
-SinkDet = SinkinRate_{Det}\cdot\ Det
-```
 [top](NPZ model/Physical Processes)
 # SinkPhy
 The phytoplankton sinks to the sea floor with a constant sinking velocity ($`SinkinRate_{Phy}`$)[m d<sup>-1</sup>]. The units of SinkPhy is [mmol N m<sup>-2</sup> d<sup>-1</sup>].
 ```math
 SinkPhy = SinkinRate_{Phy}\cdot\ Phyto
 ```
-
-[top](NPZ model/Physical Processes)
+[[top](NPZ model/Physical Processes)
+# SinkDet
+The detritus sinks to the sea floor with a constant sinking velocity ($`SinkinRate_{Det}`$)[m d<sup>-1</sup>]. The units of SinkDet is [mmol N m<sup>-2</sup> d<sup>-1</sup>].
+```math
+SinkDet = SinkinRate_{Det}\cdot\ Det
+```
+top](NPZ model/Physical Processes)
 # Transport
 State variables in the water column (DIN, Phyto, Zoo and Det) are transported by tidal currents. This transport is modeled as exchange rates between the neighboring compartments. It is assumed that the exchange rates are bi-directional, i.e. the exchange rate [m<sup>3</sup> d<sup>-1</sup>] from compartment $`i`$ to compartment $`j`$ is the same as the exchange rate from compartment $`j`$ to $`i`$.