FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2014379819> ?p ?o ?g. }

• W2014379819 endingPage "2685" @default.
• W2014379819 startingPage "2677" @default.
• W2014379819 abstract "The portion of the radiance exiting the ocean and transmitted to the top of the atmosphere (TOA) in a particular direction depends on the angular distribution of the exiting radiance, not just the radiance exiting in the direction of interest. The diffuse transmittance t relates the water component of the TOA radiance to that exiting the water in the same direction. As such t is a property of the ocean–atmosphere system and not just the atmosphere. Its computation requires not only the properties of the atmosphere but the angular distribution of the exiting radiance as well. The latter is not known until a determination of the water properties can be made (which is the point of measuring the radiance in the first place). Because of this, it has been customary to assume an angular distribution (uniform upward radiance beneath the water surface) in the computation of t, which is referred to as t⁎. However, it is known that replacing t with t⁎ can result in an error of several percent in the retrieved water-leaving radiance. Since the error depends on sun-viewing direction, this error could be particularly important when water-leaving radiance from two or more sensors in different orbits are compared. Even given an estimate of the angular distribution of the water-leaving radiance, computation of t using full radiative transfer theory in an image processing environment is not practical. Thus, we developed a first-order correction to t for bidirectional effects in the water-leaving radiance that captures much of the variability of t with viewing direction. The correction computed across a SeaWiFS scan line shows that a t⁎-induced error of as much as 5–6% could occur near the edges of the scan; however, limiting the scan to polar viewing angles (θ) < 60° reduces the error to ~ 1%. Direct application to SeaWIFS and MODIS (AQUA) suggests that the bidirectionally-induced error in the diffuse transmittance will result in an error less than about 1% in the comparison of their normalized water-leaving radiances, as long as θ is less than about 60°. We conclude that, given this constraint, the normalized water-leaving retrievals from these two sensors at a given location can be merged without regard for the bidirectionally-induced error in the diffuse transmittance, as the resulting uncertainty is well below that from other sources. It is important to note that this result is likely to apply to any other polar-orbiting sensor with equatorial crossing times (similar to SeaWiFS and MODIS) between 1030 and 1330 h (local time)." @default.
• W2014379819 created "2016-06-24" @default.
• W2014379819 creator A5072553193 @default.
• W2014379819 creator A5080633828 @default.
• W2014379819 date "2008-05-01" @default.
• W2014379819 modified "2023-09-24" @default.
• W2014379819 title "Remote sensing of ocean color: Assessment of the water-leaving radiance bidirectional effects on the atmospheric diffuse transmittance for SeaWiFS and MODIS intercomparisons" @default.
• W2014379819 cites W1972660144 @default.
• W2014379819 cites W1976556171 @default.
• W2014379819 cites W1999981717 @default.
• W2014379819 cites W2006904697 @default.
• W2014379819 cites W2008771271 @default.
• W2014379819 cites W2043683651 @default.
• W2014379819 cites W2074994079 @default.
• W2014379819 cites W2128968708 @default.
• W2014379819 cites W2129825189 @default.
• W2014379819 cites W2131752879 @default.
• W2014379819 cites W2134658045 @default.
• W2014379819 doi "https://doi.org/10.1016/j.rse.2007.12.010" @default.
• W2014379819 hasPublicationYear "2008" @default.
• W2014379819 type Work @default.
• W2014379819 sameAs 2014379819 @default.
• W2014379819 citedByCount "44" @default.
• W2014379819 countsByYear W20143798192012 @default.
• W2014379819 countsByYear W20143798192013 @default.
• W2014379819 countsByYear W20143798192014 @default.
• W2014379819 countsByYear W20143798192015 @default.
• W2014379819 countsByYear W20143798192016 @default.
• W2014379819 countsByYear W20143798192017 @default.
• W2014379819 countsByYear W20143798192018 @default.
• W2014379819 countsByYear W20143798192020 @default.
• W2014379819 countsByYear W20143798192022 @default.
• W2014379819 countsByYear W20143798192023 @default.
• W2014379819 crossrefType "journal-article" @default.
• W2014379819 hasAuthorship W2014379819A5072553193 @default.
• W2014379819 hasAuthorship W2014379819A5080633828 @default.
• W2014379819 hasConcept C117082904 @default.
• W2014379819 hasConcept C120665830 @default.
• W2014379819 hasConcept C121332964 @default.
• W2014379819 hasConcept C127313418 @default.
• W2014379819 hasConcept C1276947 @default.
• W2014379819 hasConcept C142796444 @default.
• W2014379819 hasConcept C153294291 @default.
• W2014379819 hasConcept C178790620 @default.
• W2014379819 hasConcept C185592680 @default.
• W2014379819 hasConcept C19269812 @default.
• W2014379819 hasConcept C23690007 @default.
• W2014379819 hasConcept C2776939893 @default.
• W2014379819 hasConcept C2780892065 @default.
• W2014379819 hasConcept C39432304 @default.
• W2014379819 hasConcept C62649853 @default.
• W2014379819 hasConcept C65440619 @default.
• W2014379819 hasConcept C74902906 @default.
• W2014379819 hasConceptScore W2014379819C117082904 @default.
• W2014379819 hasConceptScore W2014379819C120665830 @default.
• W2014379819 hasConceptScore W2014379819C121332964 @default.
• W2014379819 hasConceptScore W2014379819C127313418 @default.
• W2014379819 hasConceptScore W2014379819C1276947 @default.
• W2014379819 hasConceptScore W2014379819C142796444 @default.
• W2014379819 hasConceptScore W2014379819C153294291 @default.
• W2014379819 hasConceptScore W2014379819C178790620 @default.
• W2014379819 hasConceptScore W2014379819C185592680 @default.
• W2014379819 hasConceptScore W2014379819C19269812 @default.
• W2014379819 hasConceptScore W2014379819C23690007 @default.
• W2014379819 hasConceptScore W2014379819C2776939893 @default.
• W2014379819 hasConceptScore W2014379819C2780892065 @default.
• W2014379819 hasConceptScore W2014379819C39432304 @default.
• W2014379819 hasConceptScore W2014379819C62649853 @default.
• W2014379819 hasConceptScore W2014379819C65440619 @default.
• W2014379819 hasConceptScore W2014379819C74902906 @default.
• W2014379819 hasIssue "5" @default.
• W2014379819 hasLocation W20143798191 @default.
• W2014379819 hasOpenAccess W2014379819 @default.
• W2014379819 hasPrimaryLocation W20143798191 @default.
• W2014379819 hasRelatedWork W1968464003 @default.
• W2014379819 hasRelatedWork W1991506583 @default.
• W2014379819 hasRelatedWork W2007427384 @default.
• W2014379819 hasRelatedWork W2014379819 @default.
• W2014379819 hasRelatedWork W2079013937 @default.
• W2014379819 hasRelatedWork W2121383674 @default.
• W2014379819 hasRelatedWork W2161495293 @default.
• W2014379819 hasRelatedWork W2168906044 @default.
• W2014379819 hasRelatedWork W3172464660 @default.
• W2014379819 hasRelatedWork W790450531 @default.
• W2014379819 hasVolume "112" @default.
• W2014379819 isParatext "false" @default.
• W2014379819 isRetracted "false" @default.
• W2014379819 magId "2014379819" @default.
• W2014379819 workType "article" @default.