Downwelling solar irradiance, upwelling solar radiance, sky leaving radiance, and cloud cover observed during ARCHEMHAB study (on Maria S. Merian Leg MSM21/3) from 2012-07-26 to 2012-08-10 ...
The need to obtain ocean color essential climate variables (OC-ECVs) using hyperspectral technology has gained increased interest in recent years. Assessing ocean color on a large scale in high latitude environments using satellite remote sensing is constrained by polar environmental conditions. Nev...
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ftdatacite:10.1594/pangaea.819717 2024-09-15T18:03:37+00:00 Downwelling solar irradiance, upwelling solar radiance, sky leaving radiance, and cloud cover observed during ARCHEMHAB study (on Maria S. Merian Leg MSM21/3) from 2012-07-26 to 2012-08-10 ... Garaba, Shungudzemwoyo Pascal Zielinski, Oliver 2013 application/zip https://dx.doi.org/10.1594/pangaea.819717 https://doi.pangaea.de/10.1594/PANGAEA.819717 en eng PANGAEA https://dx.doi.org/10.1364/oe.21.015938 https://dx.doi.org/10.1364/ao.54.003602 https://dx.doi.org/10.2971/jeos.2013.13058 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 article Collection Supplementary Publication Series of Datasets 2013 ftdatacite https://doi.org/10.1594/pangaea.81971710.1364/oe.21.01593810.1364/ao.54.00360210.2971/jeos.2013.13058 2024-08-01T09:03:33Z The need to obtain ocean color essential climate variables (OC-ECVs) using hyperspectral technology has gained increased interest in recent years. Assessing ocean color on a large scale in high latitude environments using satellite remote sensing is constrained by polar environmental conditions. Nevertheless, on a small scale we can assess ocean color using above-water and in-water remote sensing. Unfortunately, above-water remote sensing can only determine apparent optical properties leaving the sea surface and is susceptible to near surface environmental conditions for example sky and sunglint. Consequently, we have to rely on accurate in-water remote sensing as it can provide both synoptic inherent and apparent optical properties of seawater. We use normalized water leaving radiance LWN or the equivalent remote sensing reflectance RRS from 27 stations to compare the differences in above-water and in-water OC-ECVs. Analysis of above-water and in-water RRS spectra provided very good match-ups (R2 > 0.97, ... : Supplement to: Garaba, Shungudzemwoyo Pascal; Zielinski, Oliver (2013): Comparison of remote sensing reflectance from above-water and in-water measurements west of Greenland, Labrador Sea, Denmark Strait, and west of Iceland. Optics Express, 21(13), 15938 ... Article in Journal/Newspaper Denmark Strait Greenland Iceland Labrador Sea DataCite |
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Open Polar |
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ftdatacite |
language |
English |
description |
The need to obtain ocean color essential climate variables (OC-ECVs) using hyperspectral technology has gained increased interest in recent years. Assessing ocean color on a large scale in high latitude environments using satellite remote sensing is constrained by polar environmental conditions. Nevertheless, on a small scale we can assess ocean color using above-water and in-water remote sensing. Unfortunately, above-water remote sensing can only determine apparent optical properties leaving the sea surface and is susceptible to near surface environmental conditions for example sky and sunglint. Consequently, we have to rely on accurate in-water remote sensing as it can provide both synoptic inherent and apparent optical properties of seawater. We use normalized water leaving radiance LWN or the equivalent remote sensing reflectance RRS from 27 stations to compare the differences in above-water and in-water OC-ECVs. Analysis of above-water and in-water RRS spectra provided very good match-ups (R2 > 0.97, ... : Supplement to: Garaba, Shungudzemwoyo Pascal; Zielinski, Oliver (2013): Comparison of remote sensing reflectance from above-water and in-water measurements west of Greenland, Labrador Sea, Denmark Strait, and west of Iceland. Optics Express, 21(13), 15938 ... |
format |
Article in Journal/Newspaper |
author |
Garaba, Shungudzemwoyo Pascal Zielinski, Oliver |
spellingShingle |
Garaba, Shungudzemwoyo Pascal Zielinski, Oliver Downwelling solar irradiance, upwelling solar radiance, sky leaving radiance, and cloud cover observed during ARCHEMHAB study (on Maria S. Merian Leg MSM21/3) from 2012-07-26 to 2012-08-10 ... |
author_facet |
Garaba, Shungudzemwoyo Pascal Zielinski, Oliver |
author_sort |
Garaba, Shungudzemwoyo Pascal |
title |
Downwelling solar irradiance, upwelling solar radiance, sky leaving radiance, and cloud cover observed during ARCHEMHAB study (on Maria S. Merian Leg MSM21/3) from 2012-07-26 to 2012-08-10 ... |
title_short |
Downwelling solar irradiance, upwelling solar radiance, sky leaving radiance, and cloud cover observed during ARCHEMHAB study (on Maria S. Merian Leg MSM21/3) from 2012-07-26 to 2012-08-10 ... |
title_full |
Downwelling solar irradiance, upwelling solar radiance, sky leaving radiance, and cloud cover observed during ARCHEMHAB study (on Maria S. Merian Leg MSM21/3) from 2012-07-26 to 2012-08-10 ... |
title_fullStr |
Downwelling solar irradiance, upwelling solar radiance, sky leaving radiance, and cloud cover observed during ARCHEMHAB study (on Maria S. Merian Leg MSM21/3) from 2012-07-26 to 2012-08-10 ... |
title_full_unstemmed |
Downwelling solar irradiance, upwelling solar radiance, sky leaving radiance, and cloud cover observed during ARCHEMHAB study (on Maria S. Merian Leg MSM21/3) from 2012-07-26 to 2012-08-10 ... |
title_sort |
downwelling solar irradiance, upwelling solar radiance, sky leaving radiance, and cloud cover observed during archemhab study (on maria s. merian leg msm21/3) from 2012-07-26 to 2012-08-10 ... |
publisher |
PANGAEA |
publishDate |
2013 |
url |
https://dx.doi.org/10.1594/pangaea.819717 https://doi.pangaea.de/10.1594/PANGAEA.819717 |
genre |
Denmark Strait Greenland Iceland Labrador Sea |
genre_facet |
Denmark Strait Greenland Iceland Labrador Sea |
op_relation |
https://dx.doi.org/10.1364/oe.21.015938 https://dx.doi.org/10.1364/ao.54.003602 https://dx.doi.org/10.2971/jeos.2013.13058 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.81971710.1364/oe.21.01593810.1364/ao.54.00360210.2971/jeos.2013.13058 |
_version_ |
1810441104241197056 |