Analyzing Cloud Coverage and Mineral Concentration Effects on Remote Sensing Data in Hydrolight
This study evaluates the impact of cloud coverage and mineral concentration on remote sensing reflectance (Rrs) using the HydroLight model. Cloud coverage showed no significant effect on the diffuse attenuation coefficient (Kd) and Rrs, although some variations were observed. Measured and predicted Rrs values aligned reasonably well despite outliers. The study highlights the influence of mineral concentration on Rrs and the effects of bottom reflectance in optically shallow waters. These findings contribute to understanding water optics and improving model accuracy.
Analyzing Cloud Coverage and Mineral Concentration Effects on Remote Sensing Data in Hydrolight
E N D
Presentation Transcript
Lab 9 Hydrolight and Ecolight
Kd(1/m) • Cloud has no effects on Kd. • At wavelength of 445nm and 555nm, Kd has a similar trend as Chl conc. Depth (m)
Cloud coverage has no effect on Rrs. • But we had a outlier in our model output.
As cloud coverage increases, μd decreases. • Multiple scattering events cause μd to approach 0.5 with increasing depth. μd Depth(m)
Q2. Import IOPs a b
HydroLight Input: Predicted vs. Measured Rrs
Predicted vs. Measured Rrs Reasonable, given that measurements were taken over a week long period (not ready to ask for my money back yet). Captures the high absorption of CDOM in the blue, something not capture by the case 1 models.
Q3. IOP Case 2 water model • Influence of the mineral concentration on the Rrs • Rrsincreases with the mineral concentration
Q3. IOP Case 2 water model • Influence of the mineral composition on the Rrs
Q4. simulatingopticallyshallow water • Influence of the bottomreflectance on the Rrs • Bahamas - Coralsandbottom • HigherRrs for shallowerbottoms
Q5- hydrolight support user2 hypotheses: Problems caused by wrong backscatter number or data inputBackscatter changes don’t appear to help drop the hydrolight curveEditing out the anomalous data line appears to create the desired shape