1 / 24

Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic

This study examines the internal tidal hydrodynamics and ambient characteristics of sea level variations in the Adriatic Sea. It covers topics such as tides, storm surges, and seiches, and includes data acquisition and processing methods. The study analyzes harmonic and spectral data and provides valuable insights into the dynamics of the Adriatic Sea.

loisk
Download Presentation

Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Sea Level Measurements ITHACA PROJECT Nenad Leder and Hrvoje Mihanović Hydrographic Institute of the Republic of Croatia Zagreb, 30 November 2006

  2. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Adriatic sea level oscillations • Sea level variations of the Adriatic Sea are basically generated by tidal and atmospheric influences, primarily by air pressure and wind. • TIDES • tides are of mixed type with pronounced inequality in height; • the most interested phenomena of the Adriatic tides is very well developed amphydromy; • mean tidal ranges are small: Dubrovnik (23 cm), Split (24 cm), Bakar (30 cm) and Trieste (68 cm); • Adriatic tides can be adequately described by using seven constituents: four semi-diurnal and three diurnal tides: • M2 (principal lunar, 12.421 hours), • S2 (principal solar, 12.000), • K2 (lunisolar, 11.967 hours) • N2 (larger lunar elliptic, 12.658), • K1 (lunisolar, 23.934 hours), • O1 (lunar, 25.819 hours), • P1 (solar, 24.066 hours). • STORM SURGES • -forced aperiodic oscillations of the sea level, • -mainly caused by the forcing of long-lasting and strong winds (synoptic- scale atmospheric disturbances) as well as by pronounced air pressure changes. • SEICHES • -free oscillations – occur as a sea response to sharp changes of meteorological parameters over the basin, especially the wind and air pressure, • - periods: first mode (fundamental) 21-22 h; second mode 10-11h.

  3. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Data acquisition SEA LEVEL DATA Time interval: 1 February to 30 September 2006 Sampling interval: 1 min SBE PRESSURE GAUGE DATA Time interval: 8 March to 1 September 2006 Sampling interval: 15 min Fig. 6.1. Location of tide gauge stations and SBE pressure gauge station.

  4. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Data acquisition Fig.6.1 Scheme of the tide gauge with characteristic values (tide gauge benchmark TGBM, sea level, tide gauge datum TGD). Fig. 6.2.OTTThalimedes instrument with additional equipment before and after the installation.

  5. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Data processing • Harmonic analysis: • TASK software: Bell et al. (2000) • T-TIDE software: Pawlowicz et al. (2002) • Spectral analysis: Fast Fourier Transform method (Welch, 1967), • Wavelet spectral analysis:Torrence and Compo (1998).

  6. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Harmonic analysis Table 6.1.a. Harmonic constants for Split tide gauge calculated by using TASK and T_TIDE software packages. Values presented in brackets are amplitudes and phases calculated by Hydrographic Institute (1973).

  7. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Harmonic analysis Table 6.1.b. Harmonic constants for Dubrovnik tide gauge calculated by using TASK and T_TIDE software packages. Values presented in brackets are amplitudes and phases calculated by Hydrographic Institute (1973).

  8. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Harmonic analysis Table 6.1.c. Harmonic constants for Ithaca 01 SBE pressure gauge calculated by using TASK and T_TIDE software packages.

  9. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Harmonic analysis – Polli (1960)

  10. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Spectral analysis Fig. 6.3. Power spectra of sea level data at Split and Dubrovnik and pressure gauge data on Ithaca01 station for the interval extending from 1 February to 30 September 2006 (Split and Dubrovnik) and from 8 March to 1 September 2006 (Ithaca01).

  11. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Spectral analysis Fig. 6.4. Power spectra of residual sea level at Split and Dubrovnik and residual pressure on Ithaca01 station for the interval extending from 1 February to 30 September 2006 (Split and Dubrovnik) and from 8 March to 1 September 2006 (Ithaca01).

  12. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Wavelet Spectral analysis Fig. 6.5. Wavelet spectrum of sea level measured at Split tide gauge, for the interval extending from 1 February to 30 September 2006. The spectrum is normalized by the respective variance. Dashed lines denote the K1 and M2 tidal periods.

  13. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Wavelet Spectral analysis 26 June 28 Sept. 14 Feb. 14 Feb. Fig. 6.6. Sea level measured at Split tide gauge and respective wavelet spectrum at the K1 tidal frequency for the interval extending from 1 February to 30 September 2006. The spectrum is normalized by the respective variance and significance level, so that the confidence level at 95% equals 1. Red arrows indicate datums of CTD cruises.

  14. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Wavelet Spectral analysis Fig. 6.7. Wavelet spectrum of sea level measured at Dubrovnik tide gauge, for the interval extending from 1 February to 30 September 2006. The spectrum is normalized by the respective variance. Dashed lines denote the K1 and M2 tidal periods.

  15. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Wavelet Spectral analysis 26 June 26 June 26 June 28 Sept. 28 Sept. 26 June 14 Feb. 14 Feb. 14 Feb. 28 Sept. Fig. 6.8. Sea level measured at Dubrovnik tide gauge and respective wavelet spectrum at the K1 tidal frequency for the interval extending from 1 February to 30 September 2006. The spectrum is normalized by the respective variance and significance level, so that the confidence level at 95% equals 1.Red arrows indicate datums of CTD cruises.

  16. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Wavelet Spectral analysis Fig. 6.9. Wavelet spectrum of pressure gauge data measured at Ithaca01 station, for the interval extending from 8 March to 1 September 2006. The spectrum is normalized by the respective variance. Dashed lines denote the K1 and M2 tidal periods.

  17. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Wavelet Spectral analysis 26 June Fig. 6.10. Bottom pressure measured at Ithaca01 station and respective wavelet spectrum at the K1 tidal frequency for the interval extending from 8 March to 1 September 2006. The spectrum is normalized by the respective variance and significance level, so that the confidence level at 95% equals 1.Red arrow indicates datum of CTD cruise.

  18. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Wavelet Spectral analysis Fig. 6.11. Wavelet spectrum of residual sea level at Split tide gauge, for the interval extending from 1 February to 30 September 2006. The spectrum is normalized by the respective variance. Dashed lines denote the periods of the fundamental mode and the first mode of the Adriatic seiche.

  19. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Wavelet Spectral analysis Fig. 6.12. Residual sea level at Split tide gauge and respective wavelet spectrum at the period of fundamental Adriatic seiche for the interval extending from 1 February to 30 September 2006. The spectrum is normalized by the respective variance and significance level, so that the confidence level at 95% equals 1.

  20. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Wavelet Spectral analysis Fig. 6.13. Wavelet spectrum of residual sea level at Dubrovnik tide gauge, for the interval extending from 1 February to 30 September 2006. The spectrum is normalized by the respective variance. Dashed lines denote the periods of the fundamental mode and the first mode of the Adriatic seiche.

  21. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Wavelet Spectral analysis Fig. 6.14. Residual sea level at Dubrovnik tide gauge and respective wavelet spectrum at the period of fundamental Adriatic seiche for the interval extending from 1 February to 30 September 2006. The spectrum is normalized by the respective variance and significance level, so that the confidence level at 95% equals 1.

  22. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Wavelet Spectral analysis Fig. 6.15. Wavelet spectrum of residual pressure at Ithaca01 station, for the interval extending from 8 March to 1 September 2006. The spectrum is normalized by the respective variance. Dashed lines denote the periods of the fundamental mode and the first mode of the Adriatic seiche.

  23. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic Wavelet Spectral analysis Fig. 6.16. Residual pressure at Ithaca01 station and respective wavelet spectrum at the period of fundamental Adriatic seiche for the interval extending from 8 March to 1 September 2006. The spectrum is normalized by the respective variance and significance level, so that the confidence level at 95% equals 1.

  24. Internal Tidal Hydrodynamics and Ambient Characteristics of the Adriatic SEICHE Fig. 6.17. A strong seiche episode recorded at the end of May and the beginning of June 2006.

More Related