Biogeochemical variations at the Porcupine Abyssal Plain sustained Observatory in the northeast Atlantic Ocean, from weekly to inter-annual timescales

We present high-resolution autonomous measurements of carbon dioxide partial pressure p (CO 2 ) taken in situ at the Porcupine Abyssal Plain sustained Observatory (PAP-SO) in the northeast Atlantic (49° N, 16.5° W; water depth of 4850 m) for the period 2010–2012. Measurements of p (CO 2 ) made at 30...

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Bibliographic Details
Published in:Biogeosciences
Main Authors: Hartman, S. E., Jiang, Z.-P., Turk, D., Lampitt, R. S., Frigstad, H., Ostle, C., Schuster, U.
Format: Text
Language:English
Published: 2018
Subjects:
North Atlantic
Northeast Atlantic
Online Access:https://doi.org/10.5194/bg-12-845-2015
https://www.biogeosciences.net/12/845/2015/
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Summary:We present high-resolution autonomous measurements of carbon dioxide partial pressure p (CO 2 ) taken in situ at the Porcupine Abyssal Plain sustained Observatory (PAP-SO) in the northeast Atlantic (49° N, 16.5° W; water depth of 4850 m) for the period 2010–2012. Measurements of p (CO 2 ) made at 30 m depth on a sensor frame are compared with other autonomous biogeochemical measurements at that depth (including chlorophyll a fluorescence and nitrate concentration data) to analyse weekly to seasonal controls on p (CO 2 ) flux in the inter-gyre region of the North Atlantic. Comparisons are also made with in situ regional time series data from a ship of opportunity and mixed layer depth (MLD) measurements from profiling Argo floats. There is a persistent under-saturation of CO 2 in surface waters throughout the year which gives rise to a perennial CO 2 sink. Comparison with an earlier data set collected at the site (2003–2005) confirms seasonal and inter-annual changes in surface seawater chemistry. There is year-to-year variability in the timing of deep winter mixing and the intensity of the spring bloom. The 2010–2012 period shows an overall increase in p (CO 2 ) values when compared to the 2003–2005 period as would be expected from increases due to anthropogenic CO 2 emissions. The surface temperature, wind speed and MLD measurements are similar for both periods of time. Future work should incorporate daily CO 2 flux measurements made using CO 2 sensors at 1 m depth and the in situ wind speed data now available from the UK Met Office Buoy.

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