scholarly journals Tide and mean sea level trend in the west coast of the Arabian Gulf from tide gauges and multi-missions satellite altimeter

Oceanologia ◽  
2019 ◽  
Vol 61 (4) ◽  
pp. 401-411 ◽  
Author(s):  
Nada Abdulraheem Siddig ◽  
Abdullah Mohammed Al-Subhi ◽  
Mohammed Ali Alsaafani
2021 ◽  
Vol 40 (7) ◽  
pp. 198-248
Author(s):  
Jianfen Li ◽  
Zhiwen Shang ◽  
Fu Wang ◽  
Yongsheng Chen ◽  
Lizhu Tian ◽  
...  

2020 ◽  
Vol 9 (1) ◽  
pp. 382-397
Author(s):  
Alberto Boretti

AbstractThe research issue of which are the present relative and absolute rates of rise and accelerations for North America is here addressed. The data of the 20 long-term-trend (LTT) tide stations of the West Coast of North America with more than 80 years of recorded data are shown. The absolute rates of rise are computed by considering the absolute vertical velocity of Global Navigation Satellite System (GNSS) antennas near the tide gauges, and the relative rate of sea-level rise from the tide gauge signals. The 20 LTT stations along the West Coast of North America show an average relative rate of rise of -0.38 mm/yr., an average acceleration of +0.0012 mm/yr2, and an average absolute rate of rise of +0.73 mm/yr. This is the first paper publishing a comprehensive survey of the absolute sea-level rates of rise along the West Coast of North America using the reliable information of relative sea-level rates of rise from LTT tide gauges plus the absolute subsidence rates from different GNSS antennas close to the tide gauge installations.


Author(s):  
A. R. M. Faizuddin ◽  
M. M. Razali

The importance of Chart Datum in hydrographic surveying is inarguable because its determination is part of the process to obtain the actual depth of bathymetry. The Chart Datum has a relationship with the determination of base points because any uncertainty of the base points would definitely cause uncertainty to the determination of the maritime baseline. If there is any doubt on the baselines, it will then cause doubt on the maritime zones as well which includes the equidistant line that forms the border between the two countries. However, due to the ongoing rising sea level, there has been some variations of the Chart Datum in some areas in Malaysia. This research discusses about the variation of Mean Sea Level and Chart Datum for the tide gauge stations at Geting, Cendering, Sedili and Tioman at East Coast and Kukup, Langkawi, Lumut and Penang at the West Coast of Peninsular Malaysia. The tidal analysis was carried out by using the 23 years of data beginning at 1993 to 2015. The observed tidal data for 23 years were processed and analysed by using GeoTide software. In this research, the Harmonic Analysis technique was used in order to calculate the values of Mean Sea Level and the Chart Datum while the slope of the shoreline is modelled by using Global Mapper. The linear trend of the Mean Sea Level and the Chart Datum was analysed to determine the increase of the annual sea level in millimetres accuracy and also to determine the variation of the Chart Datum for each tidal station and its impact towards maritime baseline. The result has shown that the linear trend of sea level rise varies from 24 millimetres per year up to 168 millimetres per year at the East Coast and 24 millimetres per year up to 96 millimetres per year at the West Coast of Peninsular Malaysia. As for the maritime baseline, results has indicated that there exist shifting in the horizontal which are varies from 1.564 metres per year to 3.299 metres per year at the East Coast and from 1.331 metres per year up to 5.857 metres per year at the West Cost of Peninsular Malaysia. From the analysis, it can be stated that the horizontal shift occur greater at the East Coast rather than at the West Coast of Peninsular Malaysia. As a conclusion, the sea level rise does have significant impact towards maritime baseline. Furthermore, the determination of a stable Chart Datum is important to define the maritime baseline in other to avoid conflict with other neighbouring countries.


1993 ◽  
Vol 44 (6) ◽  
pp. 911 ◽  
Author(s):  
M Amin

Long time-series of sea-level observations spanning 21 years (1966-86) from four ports on the west coast of Australia are analysed in yearly sets to study the secular trends and periodic changes in the tidal harmonic constituents. Mean sea level and five harmonic consistuents-Sa from low frequency band, O1 and K1 from the diurnal band, M2 and S2 from the semi-diurnal band-are investigated for secular trend and other variations that are not accounted for by conventional methods. Secular trends at Darwin, Wyndham and Geraldton are such that the amplitudes of M2 and S2 tides are decreasing and their phases are retarding. The changes observed at Fremantle are similar in magnitude but opposite in sign. In the diurnal band, variations in the phases of 01 and K1 are similar to those of the M2 and S2 tides. The observed trends of the diurnal and semidiurnal tides of Wyndham and Fremantle are well above standard error. Secular changes in the annual tide are not significant. In addition to the secular trends, these constituents are also modulated by terms which are not present in the tide-generating potential and they cannot be resolved from observations of less than 18.61 years. For example, in the spectrum of the equilibrium tide, there is no nodal term associated with the S2 constituent because it is of the solar origin, whereas in the observed tide two nodal terms appear as side bands. At some ports the amplitudes of the new nodal terms are large enough to modulate the principal tide by 2%. The mean sea level has been rising at the average rate of 1.73 mm year-1 over this period. It is modulated by a tidal signal of 18.61 years' cycle and non-tidal signals which are spatially consistent but aperiodic. A strong correlation between the residual component of the annual mean sea level and Southern Oscillation Index suggests that non-tidal long-period perturbations of mean sea level (MSL) are mainly due to El Nino-Southern Oscillation effects.


2013 ◽  
Vol 65 ◽  
pp. 678-683 ◽  
Author(s):  
Kyoung-Ho Cho ◽  
Jin-Yong Choi ◽  
Kwang-Soon Park ◽  
Sang-Kwon Hyun ◽  
Yuri Oh ◽  
...  

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