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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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 |
_version_ |
1795038186871717888 |