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Sea surface carbon dioxide at the Georgia time series site (2006-2007): Air-sea flux and controlling processes

期刊

PROGRESS IN OCEANOGRAPHY
卷 140, 期 -, 页码 14-26

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.pocean.2015.09.008

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资金

  1. NOAA Global Carbon Cycle Program [GCO5-208]
  2. Ocean Acidification Program [OAPFY11.01.NGI.003]
  3. NSF [OCE-0425153]
  4. NOAA Climate Program Office
  5. NOAA Ocean Acidification Program
  6. China Scholarship Council for providing the scholarship fund [201404180014]
  7. National Natural Science Foundation of China [41506099]

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Carbon dioxide partial pressure (pCO(2)) in surface seawater was continuously recorded every three hours from 18 July 2006 through 31 October 2007 using a moored autonomous pCO(2) (MAPCO(2)) system deployed on the Gray's Reef buoy off the coast of Georgia, USA. Surface water pCO(2) (average 373 +/- 52 mu atm) showed a clear seasonal pattern, undersaturated with respect to the atmosphere in cold months and generally oversaturated in warm months. High temporal resolution observations revealed important events not captured in previous ship-based observations, such as sporadically occurring biological CO2 uptake during April-June 2007. In addition to a qualitative analysis of the primary drivers of pCO(2) variability based on property regressions, we quantified contributions of temperature, air-sea exchange, mixing, and biological processes to monthly pCO(2) variations using a 1-D mass budget model. Although temperature played a dominant role in the annual cycle of pCO(2), river inputs especially in the wet season, biological respiration in peak summer, and biological production during April-June 2007 also substantially influenced seawater pCO(2). Furthermore, sea surface pCO(2) was higher in September-October 2007 than in September-October 2006, associated with increased river inputs in fall 2007. On an annual basis this site was a moderate atmospheric CO2 sink, and was autotrophic as revealed by monthly mean net community production (NCP) in the mixed layer. If the sporadic short productive events during April-May 2007 were missed by the sampling schedule, one would conclude erroneously that the site is heterotrophic. While previous ship-based pCO(2) data collected around this buoy site agreed with the buoy CO2 data on seasonal scales, high resolution buoy observations revealed that the cruise-based surveys undersampled temporal variability in coastal waters, which could greatly bias the estimates of air-sea CO2 fluxes or annual NCP, and even produce contradictory results. (C) 2015 Elsevier Ltd. All rights reserved.

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