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Figure 3

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modified on 2017-11-10, 16:09
Figure 3 | a,The difference between the mean Eddy Kinetic Energy (EKE, defined as half of the horizontal velocity deviation from mean squared, isoline increment is 25 cm2∙s-2) of the altimetry–derived (AVISO31) ocean surface currents between the averaged eight El-Niño and seven La-Niña periods, calculated over 1993-2016. CCZ licence areas in the Tropical Pacific are shown with yellow and protected areas (APEIs) with green lines. b, Surface EKE over the BGR mooring site (star on a map). High_Res_Figure_3 (https://figshare.com/s/2a1da19c8d6afe765e52). Figure was plotted using MATLAB R2015b (http://www.mathworks.com/).The map in this figure was queried from Google Static Map APIs (http://code.google.com/apis/maps/) using the Get_google_map mapping package version 1.4 (https://uk.mathworks.com/matlabcentral/fileexchange/24113-get-google-map).

Funding

European Commission's Framework 7 Programme project - Managing Impacts of Deep-seA reSource exploitation (MIDAS), Grant No 603418