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The pressure gauges derived from the Paros measurement system have demonstrated good performances for observing tsunamis of the order of millimeters (Filloux, 1982), ocean tides (Mofjeld and Wimbush, 1977), and low-frequency (<1 day−1) oceanic variations of the order of centimeters (Niiler et al., 1993) (in general, a 1-cm sea-water height is equivalent to 1 hPa).
On the basis of the results shown in Figure 2, we assumed that weekly mesoscale oceanic variations caused by planetary Rossby waves were negligible compared with variations caused by the response of the ocean to a typhoon.
Although these HP pressure gauges show a fairly good ability to observe tsunamis of the order of millimeters (Hino et al., 2001; Hirata et al., 2003; Baba et al., 2004; Tanioka et al., 2004; Satake et al., 2005; Saito et al., 2010), there have been no reports of successful observations of low-frequency (<1 day−1) oceanic variations of the order of centimeters.
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Neptune's Mess is an oceanic variation with smoked salmon, cream cheese, sherry and scallions, and is no less of a mess.
The oceanic CO2 variation is especially large in the eastern tropical Pacific and eastern tropical Atlantic, where the equatorial and coastal upwelling has strong variation both on seasonal and interannual time scales [14].
The oceanic CO2 variation is especially large in the eastern tropical Pacific and eastern tropical Atlantic, where the equatorial and coastal upwelling has strong variation both on seasonal and interannual time scales [ 14].
Given their status as upper trophic-level predators foraging over vast areas of the subantarctic and Antarctic oceanic zone, variation in abundance and life history parameters in this species may be indicative of larger changes occurring throughout the Antarctic ecosystem [ 21].
Moreover, there is no large lateral variation in velocity within the igneous oceanic crust, so lateral variation in frequency distortion by NMO stretching is not so large there.
Temporal variability can be high, e.g. due to variations in oceanic circulations related to El Niño events [71, 99].
According to Schwimmer, the growth ring patterns observed could have been affected by a variety of factors, including "migrations of their prey, wet-dry seasonal climate variations, or oceanic circulation and nutrient cycles".
For example, different strains of cyanobacteria from different oceanic regions show large variations in CO2-dependent nitrogen fixation rates, suggesting that some strains benefit from increasing CO2 more than others (Hutchins et al. 2013).
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