For New Zealand, semidiurnal tides account for approximately 96% of the energy and the remaining 4% is attributed to barometric pressure and wind effects, storm surge, and the longer‐term seasonal and interannual fluctuations. Techniques have been developed for identifying each of these components of the sea level signal, involving analysis in both the time domain and the frequency domain. Analysis in the frequency domain is the favored method because the response to specific forcing functions can be identified, but the data should also be analyzed in the time domain to complement the results from the frequency‐domain analysis.
Techniques for analyzing sea level records around New Zealand
Reprints and Corporate Permissions
Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?
To request a reprint or corporate permissions for this article, please click on the relevant link below:
Academic Permissions
Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?
Obtain permissions instantly via Rightslink by clicking on the button below:
If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.
Related research
People also read lists articles that other readers of this article have read.
Recommended articles lists articles that we recommend and is powered by our AI driven recommendation engine.
Cited by lists all citing articles based on Crossref citations.
Articles with the Crossref icon will open in a new tab.