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Relationships between Q‐factor and seawater optical properties in a coastal region
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Zeitschriftentitel: | Limnology and Oceanography |
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Personen und Körperschaften: | , |
In: | Limnology and Oceanography, 46, 2001, 5, S. 1130-1140 |
Format: | E-Article |
Sprache: | Englisch |
veröffentlicht: |
Wiley
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Schlagwörter: |
author_facet |
Zibordi, Giuseppe Berthon, Jean-François Zibordi, Giuseppe Berthon, Jean-François |
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author |
Zibordi, Giuseppe Berthon, Jean-François |
spellingShingle |
Zibordi, Giuseppe Berthon, Jean-François Limnology and Oceanography Relationships between Q‐factor and seawater optical properties in a coastal region Aquatic Science Oceanography |
author_sort |
zibordi, giuseppe |
spelling |
Zibordi, Giuseppe Berthon, Jean-François 0024-3590 1939-5590 Wiley Aquatic Science Oceanography http://dx.doi.org/10.4319/lo.2001.46.5.1130 <jats:p>The <jats:italic>Q</jats:italic>‐factor—the ratio between upwelling irradiance and upwelling radiance—describes the bidirectional structure of seawater apparent optical properties as a function of geometry and of marine and atmospheric optical characteristics. A 3‐yr time series of Q<jats:sub>n</jats:sub>(λ) measurements—the Q‐factor determined by nadir radiance—from the North Adriatic Sea coastal waters, has been analyzed. Scatter plots of Qn(λ) versus sun zenith, θ<jats:sub>0</jats:sub>, for different intervals of the diffuse attenuation coefficient Kd(λ) have shown a consistent exponential trend. In addition, leastsquares regressions of Q<jats:sub>n</jats:sub>(λ) versus Q<jats:sub>n</jats:sub>(490) have exhibited determination coefficients R<jats:sup>2</jats:sup> that vary from 0.77 to 0.94 in the spectral range between 412 and 555 nm and R<jats:sup>2</jats:sup> = 0.50 at 665 nm. To account for these findings, an empirical model for Q<jats:sub>n</jats:sub>(λ) as a function of θ<jats:sub>0</jats:sub> and K<jats:sub>d</jats:sub>(λ<jats:sub>0</jats:sub>) at the reference wavelength λ<jats:sub>0</jats:sub> = 490 nm is proposed for North Adriatic coastal waters.</jats:p> Relationships between <i>Q</i>‐factor and seawater optical properties in a coastal region Limnology and Oceanography |
doi_str_mv |
10.4319/lo.2001.46.5.1130 |
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Biologie Allgemeine Naturwissenschaft |
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Limnology and Oceanography |
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title |
Relationships between Q‐factor and seawater optical properties in a coastal region |
title_unstemmed |
Relationships between Q‐factor and seawater optical properties in a coastal region |
title_full |
Relationships between Q‐factor and seawater optical properties in a coastal region |
title_fullStr |
Relationships between Q‐factor and seawater optical properties in a coastal region |
title_full_unstemmed |
Relationships between Q‐factor and seawater optical properties in a coastal region |
title_short |
Relationships between Q‐factor and seawater optical properties in a coastal region |
title_sort |
relationships between <i>q</i>‐factor and seawater optical properties in a coastal region |
topic |
Aquatic Science Oceanography |
url |
http://dx.doi.org/10.4319/lo.2001.46.5.1130 |
publishDate |
2001 |
physical |
1130-1140 |
description |
<jats:p>The <jats:italic>Q</jats:italic>‐factor—the ratio between upwelling irradiance and upwelling radiance—describes the bidirectional structure of seawater apparent optical properties as a function of geometry and of marine and atmospheric optical characteristics. A 3‐yr time series of Q<jats:sub>n</jats:sub>(λ) measurements—the Q‐factor determined by nadir radiance—from the North Adriatic Sea coastal waters, has been analyzed. Scatter plots of Qn(λ) versus sun zenith, θ<jats:sub>0</jats:sub>, for different intervals of the diffuse attenuation coefficient Kd(λ) have shown a consistent exponential trend. In addition, leastsquares regressions of Q<jats:sub>n</jats:sub>(λ) versus Q<jats:sub>n</jats:sub>(490) have exhibited determination coefficients R<jats:sup>2</jats:sup> that vary from 0.77 to 0.94 in the spectral range between 412 and 555 nm and R<jats:sup>2</jats:sup> = 0.50 at 665 nm. To account for these findings, an empirical model for Q<jats:sub>n</jats:sub>(λ) as a function of θ<jats:sub>0</jats:sub> and K<jats:sub>d</jats:sub>(λ<jats:sub>0</jats:sub>) at the reference wavelength λ<jats:sub>0</jats:sub> = 490 nm is proposed for North Adriatic coastal waters.</jats:p> |
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author | Zibordi, Giuseppe, Berthon, Jean-François |
author_facet | Zibordi, Giuseppe, Berthon, Jean-François, Zibordi, Giuseppe, Berthon, Jean-François |
author_sort | zibordi, giuseppe |
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description | <jats:p>The <jats:italic>Q</jats:italic>‐factor—the ratio between upwelling irradiance and upwelling radiance—describes the bidirectional structure of seawater apparent optical properties as a function of geometry and of marine and atmospheric optical characteristics. A 3‐yr time series of Q<jats:sub>n</jats:sub>(λ) measurements—the Q‐factor determined by nadir radiance—from the North Adriatic Sea coastal waters, has been analyzed. Scatter plots of Qn(λ) versus sun zenith, θ<jats:sub>0</jats:sub>, for different intervals of the diffuse attenuation coefficient Kd(λ) have shown a consistent exponential trend. In addition, leastsquares regressions of Q<jats:sub>n</jats:sub>(λ) versus Q<jats:sub>n</jats:sub>(490) have exhibited determination coefficients R<jats:sup>2</jats:sup> that vary from 0.77 to 0.94 in the spectral range between 412 and 555 nm and R<jats:sup>2</jats:sup> = 0.50 at 665 nm. To account for these findings, an empirical model for Q<jats:sub>n</jats:sub>(λ) as a function of θ<jats:sub>0</jats:sub> and K<jats:sub>d</jats:sub>(λ<jats:sub>0</jats:sub>) at the reference wavelength λ<jats:sub>0</jats:sub> = 490 nm is proposed for North Adriatic coastal waters.</jats:p> |
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spelling | Zibordi, Giuseppe Berthon, Jean-François 0024-3590 1939-5590 Wiley Aquatic Science Oceanography http://dx.doi.org/10.4319/lo.2001.46.5.1130 <jats:p>The <jats:italic>Q</jats:italic>‐factor—the ratio between upwelling irradiance and upwelling radiance—describes the bidirectional structure of seawater apparent optical properties as a function of geometry and of marine and atmospheric optical characteristics. A 3‐yr time series of Q<jats:sub>n</jats:sub>(λ) measurements—the Q‐factor determined by nadir radiance—from the North Adriatic Sea coastal waters, has been analyzed. Scatter plots of Qn(λ) versus sun zenith, θ<jats:sub>0</jats:sub>, for different intervals of the diffuse attenuation coefficient Kd(λ) have shown a consistent exponential trend. In addition, leastsquares regressions of Q<jats:sub>n</jats:sub>(λ) versus Q<jats:sub>n</jats:sub>(490) have exhibited determination coefficients R<jats:sup>2</jats:sup> that vary from 0.77 to 0.94 in the spectral range between 412 and 555 nm and R<jats:sup>2</jats:sup> = 0.50 at 665 nm. To account for these findings, an empirical model for Q<jats:sub>n</jats:sub>(λ) as a function of θ<jats:sub>0</jats:sub> and K<jats:sub>d</jats:sub>(λ<jats:sub>0</jats:sub>) at the reference wavelength λ<jats:sub>0</jats:sub> = 490 nm is proposed for North Adriatic coastal waters.</jats:p> Relationships between <i>Q</i>‐factor and seawater optical properties in a coastal region Limnology and Oceanography |
spellingShingle | Zibordi, Giuseppe, Berthon, Jean-François, Limnology and Oceanography, Relationships between Q‐factor and seawater optical properties in a coastal region, Aquatic Science, Oceanography |
title | Relationships between Q‐factor and seawater optical properties in a coastal region |
title_full | Relationships between Q‐factor and seawater optical properties in a coastal region |
title_fullStr | Relationships between Q‐factor and seawater optical properties in a coastal region |
title_full_unstemmed | Relationships between Q‐factor and seawater optical properties in a coastal region |
title_short | Relationships between Q‐factor and seawater optical properties in a coastal region |
title_sort | relationships between <i>q</i>‐factor and seawater optical properties in a coastal region |
title_unstemmed | Relationships between Q‐factor and seawater optical properties in a coastal region |
topic | Aquatic Science, Oceanography |
url | http://dx.doi.org/10.4319/lo.2001.46.5.1130 |