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: Random wave transformation on Laminaria hyperboria field (EM-897)
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EM Identity and Description
EM Identification (* Note that run information is shown only where run data differ from the "parent" entry shown at left)
EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
EM Short Name
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Random wave transformation L. hyperborea field | * | * | * | * | * | * |
EM Full Name
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Random wave transformation on Laminaria hyperboria field | * | * | * | * | * | * |
EM Source or Collection
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None | * | * | * | * | * | * |
EM Source Document ID
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424 | * | * | * | * | * | * |
Document Author
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Mendez, F. J. and I. J. Losada | * | * | * | * | * | * |
Document Year
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2004 | * | * | * | * | * | * |
Document Title
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An empirical model to estimate the propagation of random breaking and nonbreaking waves over vegetation fields | * | * | * | * | * | * |
Document Status
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Peer reviewed and published | * | * | * | * | * | * |
Comments on Status
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Published journal manuscript | * | * | * | * | * | * |
Software and Access (* Note that run information is shown only where run data differ from the "parent" entry shown at left)
EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
Not applicable | * | * | * | * | * | * | |
Contact Name
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F. J. Mendez ?Comment:Tel.: +34-942-201810 |
* ?Comment:Tel.: +34-942-201810 |
* ?Comment:Tel.: +34-942-201810 |
* ?Comment:Tel.: +34-942-201810 |
* ?Comment:Tel.: +34-942-201810 |
* ?Comment:Tel.: +34-942-201810 |
* ?Comment:Tel.: +34-942-201810 |
Contact Address
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Not reported | * | * | * | * | * | * |
Contact Email
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mendezf@unican.es | * | * | * | * | * | * |
EM Description (* Note that run information is shown only where run data differ from the "parent" entry shown at left)
EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
Summary Description
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ASTRACT: "In this work, a model for wave transformation on vegetation fields is presented. The formulation includes wave damping and wave breaking over vegetation fields at variable depths. Based on a nonlinear formulation of the drag force, either the transformation of monochromatic waves or irregular waves can be modelled considering geometric and physical characteristics of the vegetation field. The model depends on a single parameter similar to the drag coefficient, which is parameterized as a function of the local Keulegan–Carpenter number for a specific type of plant. Given this parameterization, determined with laboratory experiments for each plant type, the model is able to reproduce the root-mean-square wave height transformation observed in experimental data with reasonable accuracy." AUTHOR'S DESCRIPTION: "The theoretical solution for random waves is compared to the experimental results for an artificial kelp field given by Dubi (1995). The experiment was carried out in a 33-m-long, 1-m-wide and 1.6-m-high wave flume...The artificial kelp models were L. hyperborea" | ASTRACT: "In this work, a model for wave transformation on vegetation fields is presented. The formulation includes wave damping and wave breaking over vegetation fields at variable depths. Based on a nonlinear formulation of the drag force, either the transformation of monochromatic waves or irregular waves can be modelled considering geometric and physical characteristics of the vegetation field. The model depends on a single parameter similar to the drag coefficient, which is parameterized as a function of the local Keulegan–Carpenter number for a specific type of plant. Given this parameterization, determined with laboratory experiments for each plant type, the model is able to reproduce the root-mean-square wave height transformation observed in experimental data with reasonable accuracy." AUTHOR'S DESCRIPTION: "The theoretical solution for random waves is compared to the experimental results for an artificial kelp field given by Dubi (1995). The experiment was carried out in a 33-m-long, 1-m-wide and 1.6-m-high wave flume...The artificial kelp models were L. hyperborea" "Fig. 3 shows the comparisons between the experimental data and the theoretical root-mean-square wave height described by Eq. (31) for six different runs covering the range of parameters." | ASTRACT: "In this work, a model for wave transformation on vegetation fields is presented. The formulation includes wave damping and wave breaking over vegetation fields at variable depths. Based on a nonlinear formulation of the drag force, either the transformation of monochromatic waves or irregular waves can be modelled considering geometric and physical characteristics of the vegetation field. The model depends on a single parameter similar to the drag coefficient, which is parameterized as a function of the local Keulegan–Carpenter number for a specific type of plant. Given this parameterization, determined with laboratory experiments for each plant type, the model is able to reproduce the root-mean-square wave height transformation observed in experimental data with reasonable accuracy." AUTHOR'S DESCRIPTION: "The theoretical solution for random waves is compared to the experimental results for an artificial kelp field given by Dubi (1995). The experiment was carried out in a 33-m-long, 1-m-wide and 1.6-m-high wave flume...The artificial kelp models were L. hyperborea" "Fig. 3 shows the comparisons between the experimental data and the theoretical root-mean-square wave height described by Eq. (31) for six different runs covering the range of parameters." | ASTRACT: "In this work, a model for wave transformation on vegetation fields is presented. The formulation includes wave damping and wave breaking over vegetation fields at variable depths. Based on a nonlinear formulation of the drag force, either the transformation of monochromatic waves or irregular waves can be modelled considering geometric and physical characteristics of the vegetation field. The model depends on a single parameter similar to the drag coefficient, which is parameterized as a function of the local Keulegan–Carpenter number for a specific type of plant. Given this parameterization, determined with laboratory experiments for each plant type, the model is able to reproduce the root-mean-square wave height transformation observed in experimental data with reasonable accuracy." AUTHOR'S DESCRIPTION: "The theoretical solution for random waves is compared to the experimental results for an artificial kelp field given by Dubi (1995). The experiment was carried out in a 33-m-long, 1-m-wide and 1.6-m-high wave flume...The artificial kelp models were L. hyperborea" "Fig. 3 shows the comparisons between the experimental data and the theoretical root-mean-square wave height described by Eq. (31) for six different runs covering the range of parameters." | ASTRACT: "In this work, a model for wave transformation on vegetation fields is presented. The formulation includes wave damping and wave breaking over vegetation fields at variable depths. Based on a nonlinear formulation of the drag force, either the transformation of monochromatic waves or irregular waves can be modelled considering geometric and physical characteristics of the vegetation field. The model depends on a single parameter similar to the drag coefficient, which is parameterized as a function of the local Keulegan–Carpenter number for a specific type of plant. Given this parameterization, determined with laboratory experiments for each plant type, the model is able to reproduce the root-mean-square wave height transformation observed in experimental data with reasonable accuracy." AUTHOR'S DESCRIPTION: "The theoretical solution for random waves is compared to the experimental results for an artificial kelp field given by Dubi (1995). The experiment was carried out in a 33-m-long, 1-m-wide and 1.6-m-high wave flume...The artificial kelp models were L. hyperborea" "Fig. 3 shows the comparisons between the experimental data and the theoretical root-mean-square wave height described by Eq. (31) for six different runs covering the range of parameters." | ASTRACT: "In this work, a model for wave transformation on vegetation fields is presented. The formulation includes wave damping and wave breaking over vegetation fields at variable depths. Based on a nonlinear formulation of the drag force, either the transformation of monochromatic waves or irregular waves can be modelled considering geometric and physical characteristics of the vegetation field. The model depends on a single parameter similar to the drag coefficient, which is parameterized as a function of the local Keulegan–Carpenter number for a specific type of plant. Given this parameterization, determined with laboratory experiments for each plant type, the model is able to reproduce the root-mean-square wave height transformation observed in experimental data with reasonable accuracy." AUTHOR'S DESCRIPTION: "The theoretical solution for random waves is compared to the experimental results for an artificial kelp field given by Dubi (1995). The experiment was carried out in a 33-m-long, 1-m-wide and 1.6-m-high wave flume...The artificial kelp models were L. hyperborea" "Fig. 3 shows the comparisons between the experimental data and the theoretical root-mean-square wave height described by Eq. (31) for six different runs covering the range of parameters." | ASTRACT: "In this work, a model for wave transformation on vegetation fields is presented. The formulation includes wave damping and wave breaking over vegetation fields at variable depths. Based on a nonlinear formulation of the drag force, either the transformation of monochromatic waves or irregular waves can be modelled considering geometric and physical characteristics of the vegetation field. The model depends on a single parameter similar to the drag coefficient, which is parameterized as a function of the local Keulegan–Carpenter number for a specific type of plant. Given this parameterization, determined with laboratory experiments for each plant type, the model is able to reproduce the root-mean-square wave height transformation observed in experimental data with reasonable accuracy." AUTHOR'S DESCRIPTION: "The theoretical solution for random waves is compared to the experimental results for an artificial kelp field given by Dubi (1995). The experiment was carried out in a 33-m-long, 1-m-wide and 1.6-m-high wave flume...The artificial kelp models were L. hyperborea" "Fig. 3 shows the comparisons between the experimental data and the theoretical root-mean-square wave height described by Eq. (31) for six different runs covering the range of parameters." |
Specific Policy or Decision Context Cited
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None identified | * | * | * | * | * | * |
Biophysical Context
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No additional description provided | * | * | * | * | * | * |
EM Scenario Drivers
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No scenarios presented | * | * | * | * | * | * |
EM Relationship to Other EMs or Applications
EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
Method Only, Application of Method or Model Run
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Method + Application (multiple runs exist) | Model Run Associated with a Specific EM Application | Model Run Associated with a Specific EM Application | Model Run Associated with a Specific EM Application | Model Run Associated with a Specific EM Application | Model Run Associated with a Specific EM Application | Model Run Associated with a Specific EM Application |
New or Pre-existing EM?
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New or revised model | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
Related EMs (for example, other versions or derivations of this EM) described in ESML
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EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
Document ID for related EM
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Doc-424 | None | None | None | None | None | None |
EM ID for related EM
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EM-896 | EM-904 | EM-896 | EM-896 | EM-896 | EM-896 | EM-896 | EM-896 |
EM Modeling Approach
EM Relationship to Time (* Note that run information is shown only where run data differ from the "parent" entry shown at left)
EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
EM Temporal Extent
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Not appicable | * | * | * | * | * | * |
EM Time Dependence
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time-dependent | * | * | * | * | * | * |
EM Time Reference (Future/Past)
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Not applicable | * | * | * | * | * | * |
EM Time Continuity
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continuous | * | * | * | * | * | * |
EM Temporal Grain Size Value
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Not applicable | * | * | * | * | * | * |
EM Temporal Grain Size Unit
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Not applicable | * | * | * | * | * | * |
EM spatial extent (* Note that run information is shown only where run data differ from the "parent" entry shown at left)
EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
Bounding Type
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Other | * | * | * | * | * | * |
Spatial Extent Name
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wave flume | * | * | * | * | * | * |
Spatial Extent Area (Magnitude)
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<1 ha | * | * | * | * | * | * |
Spatial Distribution of Computations (* Note that run information is shown only where run data differ from the "parent" entry shown at left)
EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
EM Spatial Distribution
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spatially distributed (in at least some cases) | * | * | * | * | * | * |
Spatial Grain Type
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length, for linear feature (e.g., stream mile) | * | * | * | * | * | * |
Spatial Grain Size
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1 m | * | * | * | * | * | * |
EM Structure and Computation Approach (* Note that run information is shown only where run data differ from the "parent" entry shown at left)
EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
EM Computational Approach
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Analytic | * | * | * | * | * | * |
EM Determinism
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deterministic | * | * | * | * | * | * |
Statistical Estimation of EM
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* | * | * | * | * | * |
Model Checking Procedures Used (* Note that run information is shown only where run data differ from the "parent" entry shown at left)
EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
Model Calibration Reported?
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No | * | * | * | * | * | * |
Model Goodness of Fit Reported?
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No | * | * | * | * | * | * |
Goodness of Fit (metric| value | unit)
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None | * | * | * | * | * | * |
Model Operational Validation Reported?
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Yes | * | * | * | * | * | * |
Model Uncertainty Analysis Reported?
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No | * | * | * | * | * | * |
Model Sensitivity Analysis Reported?
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No | * | * | * | * | * | * |
Model Sensitivity Analysis Include Interactions?
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Not applicable | * | * | * | * | * | * |
EM Locations, Environments, Ecology
Location of EM Application (* Note that run information is shown only where run data differ from the "parent" entry shown at left)
Terrestrial location (Classification hierarchy: Continent > Country > U.S. State [United States only])
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
None | * | * | * | * | * | * |
Marine location (Classification hierarchy: Realm > Region > Province > Ecoregion)
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
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Centroid Lat/Long (Decimal Degree)
EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
Centroid Latitude
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58.1 | * | * | * | * | * | * |
Centroid Longitude
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-7.1 | * | * | * | * | * | * |
Centroid Datum
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WGS84 | * | * | * | * | * | * |
Centroid Coordinates Status
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Estimated | * | * | * | * | * | * |
Environments and Scales Modeled (* Note that run information is shown only where run data differ from the "parent" entry shown at left)
EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
EM Environmental Sub-Class
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Near Coastal Marine and Estuarine | * | * | * | * | * | * |
Specific Environment Type
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Near coastal marine and estuarine | * | * | * | * | * | * |
EM Ecological Scale
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Ecological scale corresponds to the Environmental Sub-class | * | * | * | * | * | * |
Organisms modeled (* Note that run information is shown only where run data differ from the "parent" entry shown at left)
Scale of differentiation of organisms modeled
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EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
EM Organismal Scale
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Species | * | * | * | * | * | * |
Taxonomic level and name of organisms or groups identified
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
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* | * | * | * | * | * |
EnviroAtlas URL
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EM Ecosystem Goods and Services (EGS) potentially modeled, by classification system
* Note that run information is shown only where run data differ from the "parent" entry shown at left
CICES v 4.3 - Common International Classification of Ecosystem Services (Section > Division > Group > Class)
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
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* | * | * | * | * | * |
(Environmental Subclass > Ecological End-Product (EEP) > EEP Subclass > EEP Modifier)
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
None | * | * | * | * | * | * |
EM Variable Names (and Units)
* Note that for runs, variable name is displayed only where data for that variable differed by run AND those differences were reported in the source document. Where differences occurred but were not reported, the variable is not listed. Click on variable name to view details.
Predictor
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EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
Driving Variables (and Units)
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Constant or Factor Variables (and Units)
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Intermediate
EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
Intermediate (Computed) Variables (and Units)
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Response
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EM ID
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EM-897 | IR12WD44 | IR8WD57 | IR5WD63 | IR7WD68 | IR6WD75 | IR8WD104 |
Observed Response Variables (and Units)
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None | * | * | * | * | * | * |
Computed Response Variables (and Units)
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