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  • 标题:Autonomous seawater pCO2 and pH time series from 40 surface buoys and the emergence of anthropogenic trends
  • 本地全文:下载
  • 作者:Sutton, Adrienne J. ; Feely, Richard A. ; Maenner-Jones, Stacy
  • 期刊名称:Earth System Science Data Discussions
  • 电子版ISSN:1866-3591
  • 出版年度:2019
  • 卷号:11
  • 期号:1
  • 页码:421-439
  • DOI:10.5194/essd-11-421-2019
  • 语种:English
  • 出版社:Copernicus Publications
  • 摘要:Ship-based time series, some now approaching over 3 decades long, arecritical climate records that have dramatically improved our ability tocharacterize natural and anthropogenic drivers of ocean carbon dioxide(CO2) uptake and biogeochemical processes. Advancements in autonomousmarine carbon sensors and technologies over the last 2 decades have led tothe expansion of observations at fixed time series sites, thereby improvingthe capability of characterizing sub-seasonal variability in the ocean. Here,we present a data product of 40 individual autonomous moored surface oceanpCO2 (partial pressure of CO2) time seriesestablished between 2004 and 2013, 17 also include autonomous pHmeasurements. These time series characterize a wide range of surface oceancarbonate conditions in different oceanic (17 sites), coastal (13 sites), andcoral reef (10 sites) regimes. A time of trend emergence (ToE) methodologyapplied to the time series that exhibit well-constrained daily to interannualvariability and an estimate of decadal variability indicates that the lengthof sustained observations necessary to detect statistically significantanthropogenic trends varies by marine environment. The ToE estimates forseawater pCO2 and pH range from 8 to 15 years at the openocean sites, 16 to 41 years at the coastal sites, and 9 to 22 years at thecoral reef sites. Only two open ocean pCO2 time series,Woods Hole Oceanographic Institution Hawaii Ocean Time-series Station (WHOTS)in the subtropical North Pacific and Stratus in the South Pacific gyre, havebeen deployed longer than the estimated trend detection time and, for these,deseasoned monthly means show estimated anthropogenic trends of 1.9±0.3and 1.6±0.3µatm yr−1, respectively. In the future, itis possible that updates to this product will allow for the estimation ofanthropogenic trends at more sites; however, the product currently provides avaluable tool in an accessible format for evaluating climatology and naturalvariability of surface ocean carbonate chemistry in a variety of regions.Data are available at https://doi.org/10.7289/V5DB8043 andhttps://www.nodc.noaa.gov/ocads/oceans/Moorings/ndp097.html (Sutton etal., 2018).
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