Moderate Resolution Imaging Spectroradiometer (MODIS- Aqua) Chlorophyll-a Concentration 2002 - Present

This algorithm returns the near-surface concentration of chlorophyll-a (chlor_a) in mg m-3, calculated using an empirical relationship derived from in situ measurements of chlor_a and blue-to-green band ratios of in situ remote sensing reflectances (Rrs). Implementation is contingent on the availabi...

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Main Authors: P. Jeremy Werdell, NASA Goddard Space Flight Center
Format: Dataset
Language:unknown
Published: Arctic Data Center 2014
Subjects:
Online Access:https://doi.org/10.5067/AQUA/MODIS_OC.2014.0
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spelling dataone:doi:10.5067/AQUA/MODIS_OC.2014.0 2024-06-03T18:46:41+00:00 Moderate Resolution Imaging Spectroradiometer (MODIS- Aqua) Chlorophyll-a Concentration 2002 - Present P. Jeremy Werdell NASA Goddard Space Flight Center Global ENVELOPE(-180.0,180.0,90.0,-90.0) BEGINDATE: 2002-01-01T00:00:00Z ENDDATE: 2020-01-01T00:00:00Z 2014-01-01T00:00:00Z https://doi.org/10.5067/AQUA/MODIS_OC.2014.0 unknown Arctic Data Center Arctic Report Card 2020 Dataset 2014 dataone:urn:node:ARCTIC https://doi.org/10.5067/AQUA/MODIS_OC.2014.0 2024-06-03T18:16:55Z This algorithm returns the near-surface concentration of chlorophyll-a (chlor_a) in mg m-3, calculated using an empirical relationship derived from in situ measurements of chlor_a and blue-to-green band ratios of in situ remote sensing reflectances (Rrs). Implementation is contingent on the availability three or more sensor bands spanning the 440 - 570 nm spectral regime. The algorithm is applicable to all current ocean color sensors. The chlor_a product is included as part of the standard Level-2 OC product suite and the Level-3 CHL product suite. The current implementation for the default chlorophyll algorithm (chlor_a) employs the standard OC3/OC4 (OCx) band ratio algorithm merged with the color index (CI) of Hu et al. (2012). As described in that paper, this refinement is restricted to relatively clear water, and the general impact is to reduce artifacts and biases in clear-water chlorophyll retrievals due to residual glint, stray light, atmospheric correction errors, and white or spectrally-linear bias errors in Rrs. As implemented, the algorithm diverges slightly from what was published in Hu et al. (2012) in that the transition between CI and OCx now occurs at 0.15 less than CI less than 0.2 mg/m3 to ensure a smooth transition. Hu, C., Lee, Z., and Franz, B. (2012). Chlorophyll a algorithms for oligotrophic oceans: A novel approach based on three-band reflectance difference. Journal of Geophysical Research, 117(C1). doi:10.1029/2011jc007395 Dataset Arctic Arctic Data Center (via DataONE) Arctic
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic Arctic Report Card 2020
spellingShingle Arctic Report Card 2020
P. Jeremy Werdell
NASA Goddard Space Flight Center
Moderate Resolution Imaging Spectroradiometer (MODIS- Aqua) Chlorophyll-a Concentration 2002 - Present
topic_facet Arctic Report Card 2020
description This algorithm returns the near-surface concentration of chlorophyll-a (chlor_a) in mg m-3, calculated using an empirical relationship derived from in situ measurements of chlor_a and blue-to-green band ratios of in situ remote sensing reflectances (Rrs). Implementation is contingent on the availability three or more sensor bands spanning the 440 - 570 nm spectral regime. The algorithm is applicable to all current ocean color sensors. The chlor_a product is included as part of the standard Level-2 OC product suite and the Level-3 CHL product suite. The current implementation for the default chlorophyll algorithm (chlor_a) employs the standard OC3/OC4 (OCx) band ratio algorithm merged with the color index (CI) of Hu et al. (2012). As described in that paper, this refinement is restricted to relatively clear water, and the general impact is to reduce artifacts and biases in clear-water chlorophyll retrievals due to residual glint, stray light, atmospheric correction errors, and white or spectrally-linear bias errors in Rrs. As implemented, the algorithm diverges slightly from what was published in Hu et al. (2012) in that the transition between CI and OCx now occurs at 0.15 less than CI less than 0.2 mg/m3 to ensure a smooth transition. Hu, C., Lee, Z., and Franz, B. (2012). Chlorophyll a algorithms for oligotrophic oceans: A novel approach based on three-band reflectance difference. Journal of Geophysical Research, 117(C1). doi:10.1029/2011jc007395
format Dataset
author P. Jeremy Werdell
NASA Goddard Space Flight Center
author_facet P. Jeremy Werdell
NASA Goddard Space Flight Center
author_sort P. Jeremy Werdell
title Moderate Resolution Imaging Spectroradiometer (MODIS- Aqua) Chlorophyll-a Concentration 2002 - Present
title_short Moderate Resolution Imaging Spectroradiometer (MODIS- Aqua) Chlorophyll-a Concentration 2002 - Present
title_full Moderate Resolution Imaging Spectroradiometer (MODIS- Aqua) Chlorophyll-a Concentration 2002 - Present
title_fullStr Moderate Resolution Imaging Spectroradiometer (MODIS- Aqua) Chlorophyll-a Concentration 2002 - Present
title_full_unstemmed Moderate Resolution Imaging Spectroradiometer (MODIS- Aqua) Chlorophyll-a Concentration 2002 - Present
title_sort moderate resolution imaging spectroradiometer (modis- aqua) chlorophyll-a concentration 2002 - present
publisher Arctic Data Center
publishDate 2014
url https://doi.org/10.5067/AQUA/MODIS_OC.2014.0
op_coverage Global
ENVELOPE(-180.0,180.0,90.0,-90.0)
BEGINDATE: 2002-01-01T00:00:00Z ENDDATE: 2020-01-01T00:00:00Z
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_doi https://doi.org/10.5067/AQUA/MODIS_OC.2014.0
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