Metalimnion Thickness
Locate one contiguous sampled metalimnion using a caller absolute-gradient threshold; disjoint layers are ambiguous and are not merged into a false single thickness.
Description
The metalimnion is a transition layer identified from strong vertical temperature gradients.
The metalimnion is a transition layer identified from strong vertical temperature gradients. A sampled-gradient threshold defines its boundaries at observed depths.1
The tool returns topMetalimnionDepthM, bottomMetalimnionDepthM, metalimnionThicknessM. The computation uses supplied observations and parameters rather than acquiring measurements.
When to use Metalimnion Thickness
Use this for the following task: Locate one contiguous sampled metalimnion using a caller absolute-gradient threshold; disjoint layers are ambiguous and are not merged into a false single thickness. Prepare observations and calibration parameters on the same unit and reporting basis.
How to use Metalimnion Thickness and understand its results
- Prepare the measured quantities and supplied model parameters. Match the units and align paired lists before calculating.
- Enter depthsM, temperaturesC, minimumThermalGradientCPerM according to the field table, then run the tool.
- Read topMetalimnionDepthM, bottomMetalimnionDepthM, metalimnionThicknessM. Use the calculation below to interpret the selected mean or the model’s signs, units and comparison flags.
- Review the supplied assumptions and calibration before comparing or reporting the result.
| Input field | Meaning | Value type and bounds | Requirement |
|---|---|---|---|
| depthsM | Depths m | list of number | Required |
| temperaturesC | Temperatures c | list of number | Required |
| minimumThermalGradientCPerM | Minimum thermal gradient c per m | number | Required |
Supply aligned temperatures and increasing nonnegative depths, plus a positive threshold. Find the first and last selected intervals and require every intervening interval also selected.
select interval when abs(ΔT/Δz)≥minimumGradient; thickness=bottomDepth−topDepth The symbols and boundary conditions refer to the supplied fields and the implementation described above.
| Output field | Meaning | Value type |
|---|---|---|
| topMetalimnionDepthM | Top metalimnion depth m | number |
| bottomMetalimnionDepthM | Bottom metalimnion depth m | number |
| metalimnionThicknessM | Metalimnion thickness m | number |
{
"input": {
"depthsM": [
0,
5,
10,
15
],
"temperaturesC": [
20,
19,
9,
8
],
"minimumThermalGradientCPerM": 1
},
"output": {
"topMetalimnionDepthM": 5,
"bottomMetalimnionDepthM": 10,
"metalimnionThicknessM": 5
}
} Limitations and assumptions
No selected interval or disjoint selected layers is rejected. The threshold is caller chosen, and boundaries are sample depths rather than continuous fitted interfaces.
Numerical inputs must be finite. Input-shape and calculation checks do not establish measurement quality or the validity of a supplied calibration.
Alternative or Complementary methods
Choose Thermocline Depth Max Gradient when you need its operation: Identify a unique maximum absolute interval temperature gradient, reporting interval center rather than claiming sub-sample thermocline precision. Choose Epilimnion Hypolimnion Volume Split for the complementary operation: Integrate a supplied piecewise-linear area-depth curve across thermal-layer boundaries including split contour intervals; geometry is supplied, not reconstructed from map coordinates.
Background reference: Lake Physics Tools: rLakeAnalyzer reference manual.
References
-
Lake Physics Tools: rLakeAnalyzer reference manual — Winslow, Read and colleagues; GLEON
Similar or alternative tools
- Thermocline Depth Max Gradient
Identify a unique maximum absolute interval temperature gradient, reporting interval center rather than claiming sub-sample thermocline precision.
- Epilimnion Hypolimnion Volume Split
Integrate a supplied piecewise-linear area-depth curve across thermal-layer boundaries including split contour intervals; geometry is supplied, not reconstructed from map coordinates.