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High temporal and spatial variability of dissolved oxygen and pH in a nearshore California kelp forest

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Figure

Fig. 1. Placement of SeapHOx sensors among moorings to charac-terize DO and pH differences (a) over time, (b) with depth, (c) in analongshore direction, and (d) in a cross-shore direction
Fig. 2. Frequency power spectra (cycles per day) from mooring Aat 7 m water depth for (a) temperature, (b) dissolved oxygen, (c) pHand (d) pressure
Table 1. Event-scale mean increases in dissolved oxygen (�DO) and pH (�pH) proceeding intrusion of high-density water(σ > 25.1 kg m−3) at 7 m water depth
Fig. 6. Scatter plots of (a) density difference (�Density) and dis-solved oxygen difference (�DO) between 7 and 17 m at mooringA, and (b) �Density and pH difference (�pH) between 7 and 17 mat mooring A
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