Quantifying climatological ranges and anomalies for Pacific coral reef ecosystems.

For example, upper climatological range limits in wave energy followed an overall trend with latitude; islands located farther north (i.e., Kure and Midway) showed higher upper limits of wave energy compared to islands located farther south (i.e., Swains and Tutuila), with the change in wave energy between island locations reducing with decreasing latitude ( Figs. 5B, S 1).

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