4.7 Article

Decadal changes in Arctic Ocean Chlorophyll a: Bridging ocean color observations from the 1980s to present time

期刊

REMOTE SENSING OF ENVIRONMENT
卷 275, 期 -, 页码 -

出版社

ELSEVIER SCIENCE INC
DOI: 10.1016/j.rse.2022.113020

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资金

  1. NSERC/CRSNG
  2. joint international laboratory Takuvik (ULaval/CNRS)
  3. Canada Excellence Research Chair in remote sensing of Canada's new Arctic frontier
  4. ANR [111112]
  5. CNES [131425]
  6. IPEV [1164]
  7. CSA
  8. Fondation Total
  9. ArcticNet
  10. LEFE
  11. French Arctic Initiative (Green Edge project)

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Remotely-sensed ocean color data provide a unique opportunity for studying variations of bio-optical properties in the Arctic Ocean where in situ data are limited. This study reprocessed raw data from SeaWiFS and MODIS sensors to establish a consistent Chl a dataset for the Arctic Ocean, allowing for the assessment of decadal changes in phytoplankton biomass.
Remotely-sensed Ocean color data offer a unique opportunity for studying variations of bio-optical properties which is especially valuable in the Arctic Ocean (AO) where in situ data are sparse. In this study, we re-processed the raw data from the Sea-viewing Wide Field-of-View (SeaWiFS, 1998-2010) and the MODerate resolution Imaging Spectroradiometer (MODIS, 2003-2016) ocean-color sensors to ensure compatibility with the first ocean color sensor, namely, the Coastal Zone Color Scanner (CZCS, 1979-1986). Based on a bio-regional approach, this study assesses the quality of this new homogeneous pan-Arctic Chl a dataset, which provides the longest (but non-continuous) ocean color time-series ever produced for the AO (37 years long between 1979 and 2016). We show that despite the temporal gaps between 1986 and 1998 due to the absence of ocean color satellite, the time series is suitable to establish a baseline of phytoplankton biomass for the early 1980s, before sea-ice loss accelerated in the AO. More importantly, it provides the opportunity to quantify decadal changes over the AO revealing for instance the continuous Chl a increase in the inflow shelves such as the Barents Sea since the CZCS era.

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