“…The SAM LT algorithm, recently proposed by Maselli et al, 36 is based on the simulation of remote sensing reflectance, Rrs sim through the following equation: The algorithm simulates a wide range of reflectances by varying the concentrations of the three optically active constituents within Eq. (2).…”
Section: Sam Ltmentioning
confidence: 99%
“…In this way, the algorithm is insensitive to amplitude variations of the measured reflectances, which may be due to the presence of seawater constituents with variable spectral properties and/or to inaccurate atmospheric correction of the satellite data. 36 Since all specific coefficients of absorption and backscattering coefficients used in Eq. (2) are obtained from a bio-optical survey of the Ligurian and North Tyrrhenian Seas, the algorithm has intrinsically a local validity.…”
Section: Sam Ltmentioning
confidence: 99%
“…In this case, [CHL] is particularly overestimated for the CTD13 and CTD22 samples, both belonging to the BP09 cruise. Table 4 summarizes the results obtained by applying the optical classification rules of Lee and Hu, 21 and Maselli et al, 36 to the samples taken during the three cruises. The mean chlorophyll concentrations measured and estimated by the four algorithms in Case 1 and 2 waters are summarized in the bar plot of Fig.…”
Section: Modis [Chl] Estimatesmentioning
confidence: 99%
“…5. The Lee and Hu criterion identifies 15 Case 1 water 36 to the data of the three cruises (total number of stations: 33-BP09, 9-MOMAR, 21-REP10). Lee ).…”
Section: Modis [Chl] Estimatesmentioning
confidence: 99%
“…25,31,32 OC5 algorithm, which, although more specific for Atlantic waters (Bay of Biscay and the English Channel), performs well also in other areas. [33][34][35] The semi-analytical SAM LT algorithm 36 is locally tuned for the coastal Ligurian and North Tyrrhenian Sea areas.…”
Abstract. The estimation of chlorophyll concentration in marine waters is fundamental for a number of scientific and practical purposes. Standard ocean color algorithms applicable to moderate resolution imaging spectroradiometer (MODIS) imagery, such as OC3M and MedOC3, are known to overestimate chlorophyll concentration ([CHL]) in Mediterranean oligotrophic waters. The performances of these algorithms are currently evaluated together with two relatively new algorithms, OC5 and SAM_LT, which make use of more of the spectral information of MODIS data. This evaluation exercise has been carried out using in situ data collected in the North Tyrrhenian and Ligurian Seas during three recent oceanographic campaigns. The four algorithms perform differently in Case 1 and Case 2 waters defined following global and local classification criteria. In particular, the mentioned [CHL] overestimation of OC3M and MedOC3 is not evident for typical Case 1 waters; this overestimation is instead significant in intermediate and Case 2 waters. OC5 and SAM_LT are less sensitive to this problem, and are generally more accurate in Case 2 waters. These results are finally interpreted and discussed in light of a possible operational utilization of the [CHL] estimation methods.
“…The SAM LT algorithm, recently proposed by Maselli et al, 36 is based on the simulation of remote sensing reflectance, Rrs sim through the following equation: The algorithm simulates a wide range of reflectances by varying the concentrations of the three optically active constituents within Eq. (2).…”
Section: Sam Ltmentioning
confidence: 99%
“…In this way, the algorithm is insensitive to amplitude variations of the measured reflectances, which may be due to the presence of seawater constituents with variable spectral properties and/or to inaccurate atmospheric correction of the satellite data. 36 Since all specific coefficients of absorption and backscattering coefficients used in Eq. (2) are obtained from a bio-optical survey of the Ligurian and North Tyrrhenian Seas, the algorithm has intrinsically a local validity.…”
Section: Sam Ltmentioning
confidence: 99%
“…In this case, [CHL] is particularly overestimated for the CTD13 and CTD22 samples, both belonging to the BP09 cruise. Table 4 summarizes the results obtained by applying the optical classification rules of Lee and Hu, 21 and Maselli et al, 36 to the samples taken during the three cruises. The mean chlorophyll concentrations measured and estimated by the four algorithms in Case 1 and 2 waters are summarized in the bar plot of Fig.…”
Section: Modis [Chl] Estimatesmentioning
confidence: 99%
“…5. The Lee and Hu criterion identifies 15 Case 1 water 36 to the data of the three cruises (total number of stations: 33-BP09, 9-MOMAR, 21-REP10). Lee ).…”
Section: Modis [Chl] Estimatesmentioning
confidence: 99%
“…25,31,32 OC5 algorithm, which, although more specific for Atlantic waters (Bay of Biscay and the English Channel), performs well also in other areas. [33][34][35] The semi-analytical SAM LT algorithm 36 is locally tuned for the coastal Ligurian and North Tyrrhenian Sea areas.…”
Abstract. The estimation of chlorophyll concentration in marine waters is fundamental for a number of scientific and practical purposes. Standard ocean color algorithms applicable to moderate resolution imaging spectroradiometer (MODIS) imagery, such as OC3M and MedOC3, are known to overestimate chlorophyll concentration ([CHL]) in Mediterranean oligotrophic waters. The performances of these algorithms are currently evaluated together with two relatively new algorithms, OC5 and SAM_LT, which make use of more of the spectral information of MODIS data. This evaluation exercise has been carried out using in situ data collected in the North Tyrrhenian and Ligurian Seas during three recent oceanographic campaigns. The four algorithms perform differently in Case 1 and Case 2 waters defined following global and local classification criteria. In particular, the mentioned [CHL] overestimation of OC3M and MedOC3 is not evident for typical Case 1 waters; this overestimation is instead significant in intermediate and Case 2 waters. OC5 and SAM_LT are less sensitive to this problem, and are generally more accurate in Case 2 waters. These results are finally interpreted and discussed in light of a possible operational utilization of the [CHL] estimation methods.
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