dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel Broadband annual oscillation in sea level anomaly data determined by wavelet technique and its impact on sea level prediction accuracy
VerfasserIn Maria Zbylut-Gorska, Wieslaw Kosek, Tomasz Niedzielski, Waldemar Popinski, Agnieszka Wnęk
Konferenz EGU General Assembly 2014
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 16 (2014)
Datensatznummer 250090261
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2014-4483.pdf
 
Zusammenfassung
Weekly sea level anomaly (SLA) maps are now available courtesy of the Archiving, Validation and Interpretation of Satellite Oceanographic (AVISO) data. Using the wavelet technique it is possible to compute variable broadband annual oscillation in these data as a function of geographic location. The time variable amplitudes and phases of this oscillation can be investigated using the wavelet transform with the modified Morlet wavelet function with different decay parameter σ that controls the transform time and frequency resolution. The maps of the standard deviations of amplitude variations and the products of amplitudes and phase differences were computed to show the ocean areas with the greatest amplitude and phase variability. Comparison of these maps allows to estimate whether amplitude variations are more irregular than phase ones. Additionally, the mean wavelet spectra of the global ocean can be computed with application of the same wavelet function. In these spectra there occur peaks corresponding to integer multiplicity of the annual oscillation frequency which suggests that this oscillation is nonlinear and broadband. The prediction of SLA time series was computed by a combination of the polynomial-harmonic approach with the autoregressive prediction. In order to detect the contribution of irregular amplitude and phase variations of the broadband annual oscillation on the SLA prediction errors the maps of amplitudes and standard deviations of amplitudes and of products of phase time differences and amplitudes were compared with the mean prediction errors of the SLA data for a few weeks in the future.