2008
DOI: 10.1016/j.rse.2007.09.001
|View full text |Cite
|
Sign up to set email alerts
|

HYDROPT: A fast and flexible method to retrieve chlorophyll-a from multispectral satellite observations of optically complex coastal waters

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

3
46
0

Year Published

2010
2010
2024
2024

Publication Types

Select...
5
5

Relationship

0
10

Authors

Journals

citations
Cited by 87 publications
(49 citation statements)
references
References 48 publications
3
46
0
Order By: Relevance
“…Errors in satellite Chl-a algorithm retrievals in Case II waters (e.g., MODIS-OC3; OC4 for SeaWIFS; O'Reilly et al, 1998) do not provide accurate Chl-a estimates in coastal environments (e.g., Gitelson et al, 2007) and hamper our understanding of the dynamics of bio-optical properties (e.g., Van Der Woerd & Pasterkamp, 2008;Ruddick et al, 2014). To improve the noise:error ratios associated with Chl-a retrievals, a new satellite product was developed following the SeaWiFS mission to better understand space-time patterns of Chl-a biomass and other phytoplankton properties.…”
mentioning
confidence: 99%
“…Errors in satellite Chl-a algorithm retrievals in Case II waters (e.g., MODIS-OC3; OC4 for SeaWIFS; O'Reilly et al, 1998) do not provide accurate Chl-a estimates in coastal environments (e.g., Gitelson et al, 2007) and hamper our understanding of the dynamics of bio-optical properties (e.g., Van Der Woerd & Pasterkamp, 2008;Ruddick et al, 2014). To improve the noise:error ratios associated with Chl-a retrievals, a new satellite product was developed following the SeaWiFS mission to better understand space-time patterns of Chl-a biomass and other phytoplankton properties.…”
mentioning
confidence: 99%
“…The standard products of ocean colour instruments are based on the calculated water leaving radiance or remote sensing reflectance (R rs ) and the derived inherent optical properties of water (IOP) that describe the attenuation by absorption (a), scattering (b), and total attenuation (c = a + b m −1 ) at each wavelength (λ). These quantities that describe the incoming and outgoing light field are combined in simple blue-green ratio or more complex semi-empirical algorithms to estimate the substance composition in water (Chl a), suspended particulate material (SPM), and coloured dissolved organic matter (CDOM)) [33][34][35][36]. A very short resume of products involved is given in the last column of Table 2.…”
Section: Quality Control and Compatability To Common Coast And Ocean mentioning
confidence: 99%
“…More recent efforts have concentrated on a variety of non-linear optimization algorithms (for a review see [26]). Despite this switch to more advanced optimization methods, many authors still use simple error, or objective functions based on the sum of squared error (SSE) or mean squared error (MSE) to measure the disparity between measured and modeled r rs during optimization [2,3,25,26,36,37]:…”
Section: Inversion Of Reflectancementioning
confidence: 99%