Diffuse downwelling attenuation coefficients for Southern Ocean waters for wavelengths 290-700 nm ...

Diffuse downwelling attenuation coefficients in Napierian form (DAC down) for Southern Ocean waters for wavelengths 290-700 nm. Coefficients for 320-700 nm were calculated directly from depth profiles of in situ irradiance made with an Ocean Optics Jaz spectrophotometer at PAL-LTER Station B, Arthur...

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Main Authors: Collins, James R, Marchetti, Adrian, Ducklow, Hugh W, Van Mooy, Benjamin A S
Format: Dataset
Language:English
Published: PANGAEA 2018
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.889858
https://doi.pangaea.de/10.1594/PANGAEA.889858
id ftdatacite:10.1594/pangaea.889858
record_format openpolar
spelling ftdatacite:10.1594/pangaea.889858 2024-03-31T07:49:09+00:00 Diffuse downwelling attenuation coefficients for Southern Ocean waters for wavelengths 290-700 nm ... Collins, James R Marchetti, Adrian Ducklow, Hugh W Van Mooy, Benjamin A S 2018 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.889858 https://doi.pangaea.de/10.1594/PANGAEA.889858 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.879582 https://dx.doi.org/10.1016/j.gca.2018.04.030 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Wavelength Diffuse attenuation coefficient, downward Diffuse attenuation coefficient, downward, standard deviation Monitoring station dataset Dataset 2018 ftdatacite https://doi.org/10.1594/pangaea.88985810.1594/pangaea.87958210.1016/j.gca.2018.04.030 2024-03-04T13:34:28Z Diffuse downwelling attenuation coefficients in Napierian form (DAC down) for Southern Ocean waters for wavelengths 290-700 nm. Coefficients for 320-700 nm were calculated directly from depth profiles of in situ irradiance made with an Ocean Optics Jaz spectrophotometer at PAL-LTER Station B, Arthur Harbor, Antarctica. The station is a 75 m deep sampling location about 1 km offshore. Due to the low signal-to-noise ratio in the in situ irradiance observations at wavelengths < 320 nm, coefficients were estimated for 290-320 nm using an exponential model fit to observed data from the 320-370 nm interval:DAC down =e^(-0.0149 * lamda+3.60)To achieve minimum boat shadow while making the irradiance profile measurements, the fiber optic cable and light sensor (cosine corrector) were streamed away from the small boat in a direction that was both to windward and toward the sun; the boat was then allowed to drift downwind from the measurement location to a suitable stand-off distance. A series of concurrent surface ... : Version 2, 2018-05-14. ... Dataset Antarc* Antarctica Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Arthur Harbor ENVELOPE(-64.067,-64.067,-64.767,-64.767) Southern Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Wavelength
Diffuse attenuation coefficient, downward
Diffuse attenuation coefficient, downward, standard deviation
Monitoring station
spellingShingle Wavelength
Diffuse attenuation coefficient, downward
Diffuse attenuation coefficient, downward, standard deviation
Monitoring station
Collins, James R
Marchetti, Adrian
Ducklow, Hugh W
Van Mooy, Benjamin A S
Diffuse downwelling attenuation coefficients for Southern Ocean waters for wavelengths 290-700 nm ...
topic_facet Wavelength
Diffuse attenuation coefficient, downward
Diffuse attenuation coefficient, downward, standard deviation
Monitoring station
description Diffuse downwelling attenuation coefficients in Napierian form (DAC down) for Southern Ocean waters for wavelengths 290-700 nm. Coefficients for 320-700 nm were calculated directly from depth profiles of in situ irradiance made with an Ocean Optics Jaz spectrophotometer at PAL-LTER Station B, Arthur Harbor, Antarctica. The station is a 75 m deep sampling location about 1 km offshore. Due to the low signal-to-noise ratio in the in situ irradiance observations at wavelengths < 320 nm, coefficients were estimated for 290-320 nm using an exponential model fit to observed data from the 320-370 nm interval:DAC down =e^(-0.0149 * lamda+3.60)To achieve minimum boat shadow while making the irradiance profile measurements, the fiber optic cable and light sensor (cosine corrector) were streamed away from the small boat in a direction that was both to windward and toward the sun; the boat was then allowed to drift downwind from the measurement location to a suitable stand-off distance. A series of concurrent surface ... : Version 2, 2018-05-14. ...
format Dataset
author Collins, James R
Marchetti, Adrian
Ducklow, Hugh W
Van Mooy, Benjamin A S
author_facet Collins, James R
Marchetti, Adrian
Ducklow, Hugh W
Van Mooy, Benjamin A S
author_sort Collins, James R
title Diffuse downwelling attenuation coefficients for Southern Ocean waters for wavelengths 290-700 nm ...
title_short Diffuse downwelling attenuation coefficients for Southern Ocean waters for wavelengths 290-700 nm ...
title_full Diffuse downwelling attenuation coefficients for Southern Ocean waters for wavelengths 290-700 nm ...
title_fullStr Diffuse downwelling attenuation coefficients for Southern Ocean waters for wavelengths 290-700 nm ...
title_full_unstemmed Diffuse downwelling attenuation coefficients for Southern Ocean waters for wavelengths 290-700 nm ...
title_sort diffuse downwelling attenuation coefficients for southern ocean waters for wavelengths 290-700 nm ...
publisher PANGAEA
publishDate 2018
url https://dx.doi.org/10.1594/pangaea.889858
https://doi.pangaea.de/10.1594/PANGAEA.889858
long_lat ENVELOPE(-64.067,-64.067,-64.767,-64.767)
geographic Arthur Harbor
Southern Ocean
geographic_facet Arthur Harbor
Southern Ocean
genre Antarc*
Antarctica
Southern Ocean
genre_facet Antarc*
Antarctica
Southern Ocean
op_relation https://dx.doi.org/10.1594/pangaea.879582
https://dx.doi.org/10.1016/j.gca.2018.04.030
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.88985810.1594/pangaea.87958210.1016/j.gca.2018.04.030
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