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Official Journal of the Asia Oceania Geosciences Society (AOGS)

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Fig. 2 | Geoscience Letters

Fig. 2

From: Understanding and reconstructing the coastal sea level variations along the western boundary of the North Pacific

Fig. 2

Comparison of the estimated SLA0 from Eq. 1 (blue) and the SLA from eight tide gauges (black dots) south of the KE and from five tide gauges (red dots) north of the KE in spring (March, April and May), summer (June, July, and August), autumn (September, October, and November) and winter (December, January and February). The black dash lines represent the contributions from coastal-trapped waves (the 1st term on the right-hand side of Eq. 1), while the red dash lines represent the contributions from the long Rossby waves (the 2nd term on the right side of Eq. 1)

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