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Interestingly, the ratio decreased as the maximum sea surface cooling increased.

The maximum sea surface cooling determined from the in situ observations exceeded 2°C for these four typhoons (Table 1).

Typically, the present global latitudinal limit of coral reef development is constrained by the 18 °C winter maximum sea surface isotherm (Kleypas et al. 1999).

The maximum sea surface cooling values (Table 1) were calculated from the water temperatures observed at a depth of 5 m during each analysis period.

It should be noted that the maximum sea surface cooling that occurred during the other four typhoons (T1112, T1114, T1115, and T1116) could have exceeded 2°C; however, we did not assess these four typhoons because no in situ observational evidence that the maximum sea surface cooling exceeded 2°C was available (Table 1).

The maximum sea surface cooling (1.2 2.6 °C) took place when the translation speed of cyclone is only 1.2 2.3 m/s.

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Based on their analysis, the investigators estimated that each additional storm in a month was associated with an 11% increase in CFP-related calls 18 months later, and that each 1°C increase in maximum sea-surface temperature during the month of August was associated with a 62% increase in calls after a lag of 5 16 months.

"Under greenhouse warming the eastern equatorial Pacific warms faster than the surrounding regions... making it easier to have maximum SST (sea surface temperatures) in the eastern equatorial Pacific, and hence more occurrences of extreme El Nino events," Cai said in an email.

= maximum monthly sea surface temperature (SST), Chlorophyll a max.

We illustrate the application of the coefficient of tail dependence, the χ and ¯¯¯χ statistics, and the conditional extremes model of Heffernan–Tawn to estimate the extremal dependence in time-series of 3-h maxima of sea surface elevation across a spatial array of measurement gauges at the US Army Corps of Engineers Field Research Facilityy on the Atlantic coast of North Carolina.

The analysis period is the period during which the typhoon passed over the area monitored by the profiling floats (Figure 1), and the maximum amount of sea surface cooling, which ranged from 0.8°C to 4.3°C (Table 1), was defined as the difference between the maximum and minimum water temperature at a depth of 5 m during each analysis period.

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