AMOC Tools [ amoc-msdat | amoc-msdam ] - Thermal Monitoring (IFREMER/VIIRS/Copernicus/NASA)
Core Methodology: Trend Analysis
My protocol cross-references raw multidimensional data with visual meteorological models. By avoiding the "smoothing" inherent in algorithms, i preserve the granular anomalies necessary for detecting systemic shifts.
Primary Data Source: NetCDF (.nc) multidimensional arrays via VIIRS (Visible Infrared Imaging Radiometer Suite) and Copernicus Marine Service. Manual of data extracted via Rust from the daily .nc (NetCDF) files of Ifremer and VIIRS satellites (NOAA).
This monitoring protocol tracks the Latitudinal Sea Surface Temperature (SST) Gradient across the North Atlantic Transect (40°N to 65°N). By extracting the thermal variables from the .nc files, we visualize the heat exchange between the subtropics and the subpolar gyre.
⚠️ Key Indicators of AMOC Instability
A statistical decrease in the Delta between the 40°N and 60°N latitudes. This indicates a weakening of the "conveyor belt" and a slowdown in northward heat transport.
Technical Note: The values presented by my aplications (amoc-msdat | amoc-msdam) focus on critical latitudes (40.0°N to 60.0°N), where thermal instability becomes most evident before a systemic collapse.
The "Cold Blob" Anomaly: Persistent, isolated cooling anomalies in the 50°N–60°N range. This appears as unexpected hues in regions where seasonal norms predict warmer transitions. Real-time observation of the formation of the "Cold Blob" in the North Atlantic, a physical indicator of the slowdown in heat transport.
Data Voids & Masking: * "---" or Null Values: Dynamically represented by descriptive captions in my applications