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The Sub-Polar Gyre Index – a community data set for application in fisheries and environment research

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Figure

Figure 1. Map of the sub-tropical and sub-polar North Atlantic witha schematic representation of the ocean circulation.
Figure 2. First mode of the EOFA of sea surface height: (a) empir-ical orthogonal function (spatial field, in centimetres); (b) principalcomponent (temporal variability, dimensionless).
Figure 4. Comparison of yearly SPG-I for different domains within the North Atlantic: (a) yearly SPG-I time series; (b–d) correspondingempirical orthogonal function (spatial field, in centimetres) for three domains
Figure 5. Sensitivity of yearly SPG-I to time series length: (a) principal component (temporal variability, dimensionless) for time periodsfrom 1993 to 2002, increasing 1 year in length (grey lines) with periods shown in (b–d) in bold black lines; empirical orthogonal function(spatial field, in centimetres) for four time periods: (b) 1993 to 2002, (c) 1993 to 2007, (d) 1993 to 2012, and (e) 1993 to 2015.
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