start:hype_model_description:hype_np_riv_lake
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start:hype_model_description:hype_np_riv_lake [2018/11/16 15:45] cpers [Basic assumptions] |
start:hype_model_description:hype_np_riv_lake [2018/11/16 15:46] cpers [Basic assumptions] |
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| ====== Nitrogen and phosphorus processes in rivers and lakes ====== | ====== Nitrogen and phosphorus processes in rivers and lakes ====== | ||
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| - | ===== Basic assumptions ===== | ||
| HYPE simulates concentration of inorganic nitrogen (IN), organic nitrogen (ON), soluble reactive phosphorus (SP) and particulate phosphorus (PP) in discharge and other surface waters. As output also the total nitrogen (TN) and phosphorus (TP) concentration can be had. In addition total suspended sediments (TS) can be simulated. It consists of the sum of suspended sediments (SS) and algae (AE) simulated concentrations. | HYPE simulates concentration of inorganic nitrogen (IN), organic nitrogen (ON), soluble reactive phosphorus (SP) and particulate phosphorus (PP) in discharge and other surface waters. As output also the total nitrogen (TN) and phosphorus (TP) concentration can be had. In addition total suspended sediments (TS) can be simulated. It consists of the sum of suspended sediments (SS) and algae (AE) simulated concentrations. | ||
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| + | ===== Basic assumptions ===== | ||
| Transformations of nutrients take place in lakes and rivers. For lakes, which are divided into fast (FLP) and slow (SLP) lake parts, the process is performed only in SLP (Fig. 1). For rivers, which hold delayed water in a queue and in the damping box, the processes is performed only in the damping box. | Transformations of nutrients take place in lakes and rivers. For lakes, which are divided into fast (FLP) and slow (SLP) lake parts, the process is performed only in SLP (Fig. 1). For rivers, which hold delayed water in a queue and in the damping box, the processes is performed only in the damping box. | ||
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