EO-derived turbidity for Lake Hume using Sentinel 2
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Description
Turbidity is derived from the scattering caused by suspended particles in water and determined by the backward scattering of light between 450 to 800nm.
Parameter: Turbidity (NTU)
Spatial resolution | Temporal resolution |
10 m | 10 days |
Temporal coverage
2015 – 2019
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Area of interest
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Related Datasets
- WW-HYPE simulated data of evapotranspiration of the upstream subbasin areas of Lake Hume
- EOInput Exp02 for Hume Lake
- Radiance to the Top of the Atmosphere for the PRISMA hyperspectral sensor (Lake Hume)
- WW-HYPE simulated data of suspended sediment concentrations in outflow from subbasin (Lake Hume)
- EO-derived total absorption for Lake Hume using Landsat 8
- Reanalysis Meteorological data for Hume Lake (Exp01)