2020
DOI: 10.3390/rs12193210
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Evaluation of the CDOM Absorption Coefficient in the Arctic Seas Based on Sentinel-3 OLCI Data

Abstract: Our work’s primary goal is to reveal the problematic issues related to estimates of the colored organic matter absorption coefficient in the northern seas from data of the Ocean and Land Color Instrument (OLCI) installed on the Sentinel-3 satellites, e.g., a comparison of the OLCI standard error assessment ADG443_NN_err relating to the measurement and the retrieval of the geophysical products and the uncertainties in the northern seas’ real situation. The natural conditions are incredibly unfavorable there, ma… Show more

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Cited by 15 publications
(13 citation statements)
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“…The OLCI ocean color scanners launched in February 2016 (Sentinel-3A) and in April 2018 (Sentinel-3B) should provide satellite data in the next decade. It was shown by Glukhovets et al [31] that the standard OLCI algorithm for estimating the CDOM absorp-tion coefficient ADG443_NN gives high errors in the Arctic seas. The dataset presented in this work may be used to improve existing standard and regional [78] algorithms and to create new ones.…”
Section: Discussionmentioning
confidence: 99%
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“…The OLCI ocean color scanners launched in February 2016 (Sentinel-3A) and in April 2018 (Sentinel-3B) should provide satellite data in the next decade. It was shown by Glukhovets et al [31] that the standard OLCI algorithm for estimating the CDOM absorp-tion coefficient ADG443_NN gives high errors in the Arctic seas. The dataset presented in this work may be used to improve existing standard and regional [78] algorithms and to create new ones.…”
Section: Discussionmentioning
confidence: 99%
“…Obtained results on CDOM absorption can be valuable in remote sensing and modeling issues. For example, calculated from satellite data, CDOM absorption coefficients may be used as an effective indicator of the Kara Sea surface desalinated layer distribution and dynamics [31]. As the values of light absorption in this layer are significantly higher than in surrounding seawaters [56,77], its characteristics must be taken into account in heat budget models.…”
Section: Cdom Absorption At 350 Nm and 440 Nmmentioning
confidence: 99%
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“…As a rule, however, for comparison with satellite data, either data from various PT analogs are used [77], or data from floating spectroradiometers that are widely employed today for validating satellite data obtained during field experiments. They measure absolute spectral irradiance at the sea surface and water leaving radiance immediately under the sea surface [78]. TM data are usually used for estimating river water penetration depth and turbidity profiling.…”
Section: Performance Of Contact Turbidity Sensorsmentioning
confidence: 99%
“…However, these algorithms are based on a limited set of data and need validation. Previously, the validation of algorithms for estimating of the colored organic matter absorption coefficient 4 in the northern seas was performed. Measurements on cruises 72, 76, and 81 of the R/V «Akademik Mstislav Keldysh» (AMK) in 2018-2020 in the Kara Sea were used to test and modify the algorithms for estimation of the total suspended matter (TSM) concentration using data of MODIS and OLCI satellite ocean color scanners.…”
Section: Introductionmentioning
confidence: 99%