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Arctic sea ice extent (monthly)
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== Monitoring and Measurement == Arctic sea ice extent is monitored using a combination of satellite remote sensing, in situ observations, and modeling. The primary data source is satellite passive microwave sensors, which provide consistent, year-round measurements of sea ice concentration and extent. These sensors can penetrate clouds and operate in polar darkness, enabling continuous monitoring. Key monitoring institutions include the National Snow and Ice Data Center (NSIDC), which produces the Sea Ice Index v3 dataset, and the Ocean and Sea Ice Satellite Application Facility (OSI SAF), which provides sea ice concentration data. The extent is typically calculated by applying a concentration threshold (commonly 15%) to satellite-derived ice concentration maps, summing the area of grid cells exceeding this threshold. Monthly aggregation of data allows for tracking seasonal and interannual variability. Additional methods such as airborne surveys and ice buoys complement satellite observations to validate and enhance data accuracy. Within the SIGNAL system, Arctic sea ice extent is treated as a defined environmental signal whose boundaries and measurement conventions are described below.
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