| _bx_events_caption_title | The maximum CC | ||
| _bx_events_caption_place | ocean123 | ||
| _bx_events_caption_event_start | 30.03.2011 15:50 (419 Days Ago) | ||
| _bx_events_caption_event_end | 29.03.2012 15:50 (54 Days Ago) |
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mean in the western zone was observed during Cruise VI with the minimum occurring during Cruise I. The eastern zone collections had the highest CC mean during Cruise III with lowest means observed during Cruise I. Highest mean OC values in the western zone occurred during Cruise VII with the lowest mean being observed during Cruise Christian Louboutin Shoes VI. With respect to the eastern zone samples, the maximum OC mean was noted during Cruise VII with minimum means observed during Cruise I and III.The means and ranges for the carbonate carbon (CC) and the organic carbon (OC) for the southwestern nearshore zone samples were 0.63$ CC, 0.29-1.14$ CC and 0.11$ OC, 0.03-0.71$ OC at the 1/2 km contour; 1.26* CC, 0.18-2.70$ CC and 1.01* OC, 0.09-2.51$ OC for the 4 km contour; 0.92$ CC, 0.04-2.67$ CC and 1.51$ OC, Coach Outlet Stores 0.38-2.80$ OC at the 8 km contour, respectively. Table 33 lists the means and ranges by cruises for each 1/2, 4 and 8 km contour. Carbonate carbon reached a maximum during Coach Bags On Sale Cruise VI at the 1/2 km contour, Cruise XI at the 4 km Christian Louboutin Outlet and Cruise I Coach Handbags Outlet at the 8 km contours. Minimum CC means were observed in the samples during Cruise IX at the 1/2 km contour and Cruise VI at the 4 and 8 km contours. With respect to temperature, the maximum CC means were observed during spring unithermal conditions and minimum CC means during late summer stratified conditions in the 4 and 8 km contour samples. The 1/2 km contour samples were more complex with a fluctuating pattern. The OC reached maximum means during Cruise VI in the 1/2 and 4 km contour collections and Cruise XI in the 8 km contour collections. Minimum OC means were observed in the Cruise I and IX samples from the Coach Outlet Store Online 1/2 km contour and Cruise I from the 4 and 8 km contour. Generally the OC appeared to increase to a maximum during thermal stratified conditions then decreased to a minimum during unstratified conditions in the samples from the 1/2 and 4 km contours. The OC means appeared to be constant at the 8 km contour collections, with a possible accumulation from spring 1972 to spring 1973Figure 38 shows the relative CC-OC means from station to station and transect to transect. The 1/2 km contour was sampled at only five stations during Coach Bags Outlet IFYGL.
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