Mills, L.; Janeiro, J.; Martins, F. Baseline Climatology of the Canary Current Upwelling System and Evolution of Sea Surface Temperature. Remote Sens.2024, 16, 504.
Mills, L.; Janeiro, J.; Martins, F. Baseline Climatology of the Canary Current Upwelling System and Evolution of Sea Surface Temperature. Remote Sens. 2024, 16, 504.
Mills, L.; Janeiro, J.; Martins, F. Baseline Climatology of the Canary Current Upwelling System and Evolution of Sea Surface Temperature. Remote Sens.2024, 16, 504.
Mills, L.; Janeiro, J.; Martins, F. Baseline Climatology of the Canary Current Upwelling System and Evolution of Sea Surface Temperature. Remote Sens. 2024, 16, 504.
Abstract
Global climate change has induced a rise in sea surface temperature (SST), although this increase is not uniform across the world. Significant variations exist between coastal and offshore waters, particularly in regions affected by upwelling processes. This study focuses on the Canary Current Upwelling System (CCUS), stretching from Northwest Iberia to Northwest Africa. High-resolution remotely sensed SST data (0.05°) from the ODYSSEA Level 4 Sea Surface Temperature Reprocessed dataset were validated with in-situ measurements and employed to establish a regional climatological baseline for 1982 – 2012. Subsequent years were compared to this baseline to construct SST anomaly maps, revealing SST changes since 2012. The study area was further divided into sub-regions for comparative analysis. Results indicate that SST consistently increased at a higher rate offshore compared to the adjacent nearshore regions. A reference dataset spanning 1951 – 1981 was used to gauge SST variability between the two baselines. SST exhibited a 0.59°C increase from 1951 – 1981 to 1982 – 2012, with a slowing of SST trends beyond the 1982 – 2012 baseline. This research offers valuable insights into the climatological dynamics of the CCUS. These findings enhance our understanding of this critical coastal system's climatology, laying the groundwork for future investigations into evolving climate patterns in coastal regions.
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