start:hype_model_description:hype_tracer
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start:hype_model_description:hype_tracer [2020/04/30 10:53] cpers [Table] |
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| To simulate temperature as the substance T2 the lake is divided in two lake parts, lake temperature in a hypothetical epilimnion and hypolimnion (//uppertemp//, //lowertemp//) is handled in the model. The average temperature of the lake is also a state variable. The size of volumes related to the upper and lower temperatures are determined by the thermocline which is estimated for each outlet lake. | To simulate temperature as the substance T2 the lake is divided in two lake parts, lake temperature in a hypothetical epilimnion and hypolimnion (//uppertemp//, //lowertemp//) is handled in the model. The average temperature of the lake is also a state variable. The size of volumes related to the upper and lower temperatures are determined by the thermocline which is estimated for each outlet lake. | ||
| - | | {{:start:hype_model_description:epi_hypo_lake.png?300}} | | + | | {{:start:hype_model_description:epi_hypo_lake.png?400}} | |
| | Figure 3: Two different divisions of a lake. Left: two parts signifying fast flows (FLP) and slow flows (SLP). Right: epilimnion (EPI) and hypolimnion (HYPO). | | | Figure 3: Two different divisions of a lake. Left: two parts signifying fast flows (FLP) and slow flows (SLP). Right: epilimnion (EPI) and hypolimnion (HYPO). | | ||
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