distribution pattern August 2008; see more typical distribution patterns in the paper by
Hamme et al. (2010). (d) Rise in pH and drop in pCO 2 at Station P (dot in part c) after
plume arrival about 12 August. (e) Raw seaglider fluorescence data from the vicinity
of Station P before and after plume arrival.
(^) (After Hamme et al. 2010.)
Plate 16.4 Time vs. offshore distance at CalCOFI Line 80 (Fig. 16.22a) contoured for
(a & c) depth (m) of the 12°C isotherm as a proxy for thermocline and nutricline
depths and for (b & d) loge[macrozooplankton displacement volume, ml (1000 m)−3].
Above (a & b) 1950–1975 and below (c & d) 1976–2000. Dots (1392 for thermocline
depth and 1750 for plankton volume) represent stations. Gray shading covers times
with long gaps between cruises.
(After McGowan et al. 2003.)