vertically integrated kinetic energy difference [j/m 5 3r ... · ï 5 3r 1r 1r 3r 5 subsampling...
TRANSCRIPT
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Vertically Integrated Kinetic Energy Difference [J/m2]
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Supplementary Figure 1: Increased ‘spin up’ and ‘spin down’ signal is recovered if one only chooses eddies that reside in a wind gradient. Here chosen to avoid the peak in the cold core eddy abundance residing in no wind gradient.Regions North of 45S and South of 55S. (Mesoscale Fully Coupled - Mesoscale Mechanically Coupled)
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Supplementary Figure 2: Subsamples of eddy field for Fully Coupled (red) and Mechanically Coupled (black)with even number eddies (solid) andodd number eddies (dashed) for a) Northern spin up region, E��6RXWKHUQ�VSLQ�GRZQ�UHJLRQ�
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Kinetic Energy Difference [%]
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Fully - Mechanically Coupled
Time [Days]
Supplementary Figure 3: Percentage change in volume integrated ocean kinetic energy for ��!���6��¶VSLQ�XS·�DQG������6��¶VSLQ�GRZQ·�UHJLRQ���0HVRVFDOH�7KHUPRG\QDPLFDOO\�&RXSOHG���0HVRVFDH�0HFKDQLFDOO\�&RXSOHG�VLPXODWLRQV��GDVKHG�SXUSOH��� Fully Coupled - Mesoscale Mechanically Coupled (Solid Green)
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Warm Core - Wind Stress CurlFully Coupled Simulation
Warm Core -Wind Stress CurlMechanically Coupled Simulation
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Warm Core Wind Energy Input [W/m2]
Cold Core Wind Energy Input [W/m2]
Wind Energy Input
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6XSSOHPHQWDU\�)LJXUH����6DWHOOLWH�2EVHUYDWLRQ�EDVHG�DQDO\VLV�FRUUHVSRQGLQJ�WR�)LJXUH��EF�Eddy composites of wind energy input associated with geostrophic current anomalies for anticyclones (a) and cyclones (b) for eddies existing in meridional wind stress gradients JUHDWHU�WKDQ�RU�OHVV�WKDQ������1�P-2��(GGLHV�DUH�QRUPDOL]HG�ZLWK�WKHLU�LQGLYLGXDO�UDGLL�EHIRUH�DYHUDJLQJ��5�UHIHUV�WR�HGG\�UDGLXV�DQG�RQO\�HGGLHV�ZLWK�OLIHVSDQV�RI�DW�OHDVW�WZR�ZHHNV�DUH�LQFOXGHG�LQ�WKH�DQDO\VLV���F��6RXWK�1RUWK�&KRUGV�DFURVV�WKH�ZLQG�HQHUJ\�LQSXW�HGG\�FRPSRVLWHV�IRU�DQWLF\FORQHV��UHG��DQG�F\FORQHV��EOXH���