Integrated net primary production during POLARSTERN cruise ARK-XXVII/3 (IceArc) in 2012

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Hauptverfasser: Fernández-Méndez, Mar, Peeken, Ilka, Boetius, Antje
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2014
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author Fernández-Méndez, Mar
Peeken, Ilka
Boetius, Antje
author_facet Fernández-Méndez, Mar
Peeken, Ilka
Boetius, Antje
collection Datos científicos de ciencias marinas y ambientales
contents Depth-integrated in situ rates were calculated for each environment as a function of the available photosynthetically active radiation (PAR). Irradiance profiles were calculated for each environment (sea ice, melt pond, water under the ice and open water) from the daily average incoming solar shortwave irradiance measured by a pyranometer (Kipp & Zonen, Delft, Netherland) mounted on the ship. We used light attenuation coefficients of 10 m**-1 for snow, 1.5 m**-1 for sea ice (Perovich, 1996) and 0.1 m**-1 for Atlantic-influenced Arctic seawater, based on literature values and observations during the cruise. Planar irradiance was transformed to scalar irradiance according to Ehn and Mundy (2013) and Katlein et al., (2014). Water column production was integrated over the euphotic zone (1% of incoming irradiance) and sea ice production over the ice core thickness. Melt pond coverage and sea ice concentration were taken into account when calculating the total primary production per area.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_834218
institution PANGAEA
language en
publishDate 2014
publisher PANGAEA
record_format pangaea
spellingShingle Integrated net primary production during POLARSTERN cruise ARK-XXVII/3 (IceArc) in 2012
Fernández-Méndez, Mar
Peeken, Ilka
Boetius, Antje
ABYSS; Arctic Ocean; ARK-XXVII/3; Assessment of bacterial life and matter cycling in deep-sea surface sediments; Calculated; CTD/Rosette; CTD-RO; Date/Time of event; Depth of the euphotic zone; Event label; Expendable CTD; Gear; ICE; Ice station; Ice station #1; Ice station #2; Ice station #3; Ice station #4; Ice station #5; Ice station #6; Ice station #7; Ice station #8; Laptev Sea; Latitude of event; Longitude of event; Melt pond depth; Net primary production of carbon; Optional event label; Polarstern; PS80/209-1; PS80/213-1; PS80/215-1; PS80/218-1; PS80/220-1; PS80/224-1; PS80/234-1; PS80/235-1; PS80/237-1; PS80/250-1; PS80/255-1; PS80/263-1; PS80/269-1; PS80/271-1; PS80/277-1; PS80/284-1; PS80/287-1; PS80/289-1; PS80/294-1; PS80/298-1; PS80/311-1; PS80/316-1; PS80/319-1; PS80/323-1; PS80/333-2; PS80/335-1; PS80/341-1; PS80/349-1; PS80/360-1; PS80/372-1; PS80/377-1; PS80/380-1; PS80/383-1; PS80/XCTD30-1; PS80 IceArc; Sea ice thickness; Short-wave downward (GLOBAL) radiation; XCTD
Depth-integrated in situ rates were calculated for each environment as a function of the available photosynthetically active radiation (PAR). Irradiance profiles were calculated for each environment (sea ice, melt pond, water under the ice and open water) from the daily average incoming solar shortwave irradiance measured by a pyranometer (Kipp & Zonen, Delft, Netherland) mounted on the ship. We used light attenuation coefficients of 10 m**-1 for snow, 1.5 m**-1 for sea ice (Perovich, 1996) and 0.1 m**-1 for Atlantic-influenced Arctic seawater, based on literature values and observations during the cruise. Planar irradiance was transformed to scalar irradiance according to Ehn and Mundy (2013) and Katlein et al., (2014). Water column production was integrated over the euphotic zone (1% of incoming irradiance) and sea ice production over the ice core thickness. Melt pond coverage and sea ice concentration were taken into account when calculating the total primary production per area.
title Integrated net primary production during POLARSTERN cruise ARK-XXVII/3 (IceArc) in 2012
topic ABYSS; Arctic Ocean; ARK-XXVII/3; Assessment of bacterial life and matter cycling in deep-sea surface sediments; Calculated; CTD/Rosette; CTD-RO; Date/Time of event; Depth of the euphotic zone; Event label; Expendable CTD; Gear; ICE; Ice station; Ice station #1; Ice station #2; Ice station #3; Ice station #4; Ice station #5; Ice station #6; Ice station #7; Ice station #8; Laptev Sea; Latitude of event; Longitude of event; Melt pond depth; Net primary production of carbon; Optional event label; Polarstern; PS80/209-1; PS80/213-1; PS80/215-1; PS80/218-1; PS80/220-1; PS80/224-1; PS80/234-1; PS80/235-1; PS80/237-1; PS80/250-1; PS80/255-1; PS80/263-1; PS80/269-1; PS80/271-1; PS80/277-1; PS80/284-1; PS80/287-1; PS80/289-1; PS80/294-1; PS80/298-1; PS80/311-1; PS80/316-1; PS80/319-1; PS80/323-1; PS80/333-2; PS80/335-1; PS80/341-1; PS80/349-1; PS80/360-1; PS80/372-1; PS80/377-1; PS80/380-1; PS80/383-1; PS80/XCTD30-1; PS80 IceArc; Sea ice thickness; Short-wave downward (GLOBAL) radiation; XCTD
url https://doi.org/10.1594/PANGAEA.834218