Tidal oscillations in the Caspian Sea
Long-term hourly data from 12 tide gauge stations were used to examine the character of tidal oscillations in the Caspian Sea. Diurnal and semidiurnal tidal peaks are well-defined in sea level spectra in the Middle and South Caspian basins. High-resolution spectral analysis revealed that the diurnal...
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Published in | Oceanology (Washington. 1965) Vol. 57; no. 3; pp. 360 - 375 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Moscow
Pleiades Publishing
01.05.2017
Springer Nature B.V |
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Abstract | Long-term hourly data from 12 tide gauge stations were used to examine the character of tidal oscillations in the Caspian Sea. Diurnal and semidiurnal tidal peaks are well-defined in sea level spectra in the Middle and South Caspian basins. High-resolution spectral analysis revealed that the diurnal sea level oscillations in the Middle Caspian Basin have a gravitational origin, while those in the South Caspian Basin are mainly caused by radiational effects: the amplitude of diurnal radiational harmonic S
1
is much higher than those of gravitational harmonics О
1
, P
1
, and K
1
. In the North Caspian Basin, there are no gravitational tides and only weak radiational tides are observed. A semidiurnal type of tide is predominant in the Middle and South Caspian basins. Harmonic analysis of the tides for individual annual series with subsequent vector averaging over the entire observational period was applied to estimate the mean amplitudes and phases of major tidal constituents. The amplitude of the M
2
harmonic reaches 5.4 cm in the South Caspian Basin (at Aladga). A maximum tidal range of 21 cm was found at the Aladga station in the southeastern part of the Caspian Sea, whereas the tidal range in the western part of the South Caspian Basin varies from 5 to 10 cm. |
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AbstractList | Long-term hourly data from 12 tide gauge stations were used to examine the character of Tidal oscillations in the Caspian Sea. Diurnal and semidiurnal tidal peaks are well-defined in sea level spectra in the Middle and South Caspian basins. High-resolution spectral analysis revealed that the diurnal sea level oscillations in the Middle Caspian Basin have a gravitational origin, while those in the South Caspian Basin are mainly caused by radiational effects: the amplitude of diurnal radiational harmonic S1 is much higher than those of gravitational harmonics Ðz1, P1, and K1. In the North Caspian Basin, there are no gravitational tides and only weak radiational tides are observed. A semidiurnal type of tide is predominant in the Middle and South Caspian basins. Harmonic analysis of the tides for individual annual series with subsequent vector averaging over the entire observational period was applied to estimate the mean amplitudes and phases of major tidal constituents. The amplitude of the M2 harmonic reaches 5.4 cm in the South Caspian Basin (at Aladga). A maximum tidal range of 21 cm was found at the Aladga station in the southeastern part of the Caspian Sea, whereas the tidal range in the western part of the South Caspian Basin varies from 5 to 10 cm. Long-term hourly data from 12 tide gauge stations were used to examine the character of tidal oscillations in the Caspian Sea. Diurnal and semidiurnal tidal peaks are well-defined in sea level spectra in the Middle and South Caspian basins. High-resolution spectral analysis revealed that the diurnal sea level oscillations in the Middle Caspian Basin have a gravitational origin, while those in the South Caspian Basin are mainly caused by radiational effects: the amplitude of diurnal radiational harmonic S 1 is much higher than those of gravitational harmonics О 1 , P 1 , and K 1 . In the North Caspian Basin, there are no gravitational tides and only weak radiational tides are observed. A semidiurnal type of tide is predominant in the Middle and South Caspian basins. Harmonic analysis of the tides for individual annual series with subsequent vector averaging over the entire observational period was applied to estimate the mean amplitudes and phases of major tidal constituents. The amplitude of the M 2 harmonic reaches 5.4 cm in the South Caspian Basin (at Aladga). A maximum tidal range of 21 cm was found at the Aladga station in the southeastern part of the Caspian Sea, whereas the tidal range in the western part of the South Caspian Basin varies from 5 to 10 cm. |
Author | Rabinovich, A. B. Kulikov, E. A. Medvedev, I. P. |
Author_xml | – sequence: 1 givenname: I. P. surname: Medvedev fullname: Medvedev, I. P. email: patamates@gmail.com organization: Shirshov Institute of Oceanology, Russian Academy of Sciences, Fedorov Institute of Applied Geophysics – sequence: 2 givenname: E. A. surname: Kulikov fullname: Kulikov, E. A. organization: Shirshov Institute of Oceanology, Russian Academy of Sciences – sequence: 3 givenname: A. B. surname: Rabinovich fullname: Rabinovich, A. B. organization: Shirshov Institute of Oceanology, Russian Academy of Sciences, Institute of Ocean Sciences |
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Cites_doi | 10.1111/j.1365-246X.1976.tb03658.x 10.1098/rsta.1966.0024 10.1175/1520-0485(1971)001<0032:ROTATC>2.0.CO;2 10.1002/2014JC010312 10.1007/978-94-011-1074-7 10.1142/9789812819307_0009 10.3103/S106837390912005X 10.1029/RG010i001p00001 10.1023/A:1010379601057 10.1017/CBO9781139235778 |
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References | Blatov, Vedev, Kosarev (CR1) 1990; 8 Levyant, Rabinovich, Rabinovich (CR12) 1994; 33 Parker (CR30) 2007 Lyubushin, Pisarenko, Bolgov, Rodkin, Rukavishnikova (CR13) 2004; 40 Pugh, Woodworth (CR31) 2014 Lapshin, Kulikov, Pobedonostsev, Kopeikina (CR10) 2005; 209 Rabinovich, Medvedev (CR21) 2015; 55 Spidchenko (CR23) 1973; 5 Kosarev (CR7) 1975 Frolov (CR24) 2003 Rodionov (CR33) 1994 Nekrasov (CR17) 1975 Popov, Zil’bershtein, Lobov, Chumakov (CR19) 2009; 34 Rabinovich (CR20) 1973; 4 Rabinovich, Kim (CR32) 2009 Zetler (CR35) 1971; 1 Malinovsky (CR14) 1926; 5 Skriptunov, Gorelits (CR22) 2001; 28 Wunsch (CR34) 1972; 10 CR2 Medvedev, Rabinovich, Kulikov (CR16) 2013; 53 CR6 CR5 Amin (CR25) 1976; 44 Feng, Tsimplis, Woodworth (CR27) 2015; 120 Munk, Cartwright (CR29) 1966; 259 CR26 Kosarev, Tsyganov (CR8) 1972; 2 (CR28) 2016; 46 Polukarov (CR18) 1960; 50 German (CR3) 1970; 103 Kritsky, Korenistov, Ratkovich (CR9) 1975 German, Levikov (CR4) 1988 Medvedev, Kulikov (CR15) 2016; 56 Lebedev, Kostyanoi (CR11) 2005 6853_CR6 B. D. Zetler (6853_CR35) 1971; 1 A. B. Rabinovich (6853_CR32) 2009 A. N. Kosarev (6853_CR7) 1975 B. B. Parker (6853_CR30) 2007 A. A. Lyubushin (6853_CR13) 2004; 40 S. G. Rodionov (6853_CR33) 1994 6853_CR2 A. S. Blatov (6853_CR1) 1990; 8 6853_CR5 6853_CR26 G. V. Polukarov (6853_CR18) 1960; 50 N. A. Skriptunov (6853_CR22) 2001; 28 I. P. Medvedev (6853_CR15) 2016; 56 I. P. Medvedev (6853_CR16) 2013; 53 S. K. Popov (6853_CR19) 2009; 34 V. Kh. German (6853_CR4) 1988 A. N. Kosarev (6853_CR8) 1972; 2 A. V. Frolov (6853_CR24) 2003 A. B. Rabinovich (6853_CR20) 1973; 4 C. Wunsch (6853_CR34) 1972; 10 A. B. Rabinovich (6853_CR21) 2015; 55 A. S. Levyant (6853_CR12) 1994; 33 V. B. Lapshin (6853_CR10) 2005; 209 N. V. Malinovsky (6853_CR14) 1926; 5 S. N. Kritsky (6853_CR9) 1975 S. A. Lebedev (6853_CR11) 2005 X. Feng (6853_CR27) 2015; 120 A. V. Nekrasov (6853_CR17) 1975 A. N. Spidchenko (6853_CR23) 1973; 5 V. Kh. German (6853_CR3) 1970; 103 W. H. Munk (6853_CR29) 1966; 259 M. Amin (6853_CR25) 1976; 44 D. Pugh (6853_CR31) 2014 (6853_CR28) 2016; 46 |
References_xml | – year: 1988 ident: CR4 publication-title: Probabilistic Analysis and Modeling of the Sea Level Oscillations contributor: fullname: Levikov – volume: 44 start-page: 293 year: 1976 end-page: 310 ident: CR25 article-title: The fine resolution of tidal harmonics publication-title: Geophys. J. Int. doi: 10.1111/j.1365-246X.1976.tb03658.x contributor: fullname: Amin – volume: 259 start-page: 533 issue: 1105 year: 1966 end-page: 581 ident: CR29 article-title: Tidal spectroscopy and prediction publication-title: Philos. Trans. R. Soc., A doi: 10.1098/rsta.1966.0024 contributor: fullname: Cartwright – volume: 33 start-page: 588 issue: 5 year: 1994 end-page: 598 ident: CR12 article-title: Computation of seiche oscillations in seas of arbitrary configuration (exemplified by the Caspian Sea) publication-title: Okeanologiya (Engl. 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Polukarov – ident: 6853_CR5 – volume: 55 start-page: 319 issue: 3 year: 2015 ident: 6853_CR21 publication-title: Oceanology (Engl. Transl.) contributor: fullname: A. B. Rabinovich – volume: 5 start-page: 98 year: 1973 ident: 6853_CR23 publication-title: Meteorol. Gidrol. contributor: fullname: A. N. Spidchenko – volume: 209 start-page: 129 year: 2005 ident: 6853_CR10 publication-title: Tr. Gos. Okeanogr. Inst. contributor: fullname: V. B. Lapshin – volume: 1 start-page: 34 issue: 1 year: 1971 ident: 6853_CR35 publication-title: J. Phys. Oceanogr. doi: 10.1175/1520-0485(1971)001<0032:ROTATC>2.0.CO;2 contributor: fullname: B. D. Zetler – volume: 53 start-page: 526 issue: 5 year: 2013 ident: 6853_CR16 publication-title: Oceanology (Engl. Transl.) contributor: fullname: I. P. Medvedev – start-page: 193 volume-title: Handbook of Coastal and Ocean Engineering year: 2009 ident: 6853_CR32 doi: 10.1142/9789812819307_0009 contributor: fullname: A. B. Rabinovich – ident: 6853_CR2 – volume: 4 start-page: 116 year: 1973 ident: 6853_CR20 publication-title: Vestn. Mosk. Univ., Ser. Geogr. contributor: fullname: A. B. Rabinovich – volume: 34 start-page: 801 year: 2009 ident: 6853_CR19 publication-title: Russ. Meteorol. Hydrol. doi: 10.3103/S106837390912005X contributor: fullname: S. K. Popov – volume-title: Satellite Altimetry of the Caspian Sea year: 2005 ident: 6853_CR11 contributor: fullname: S. A. Lebedev – volume: 33 start-page: 588 issue: 5 year: 1994 ident: 6853_CR12 publication-title: Okeanologiya (Engl. Transl.) contributor: fullname: A. S. Levyant – ident: 6853_CR6 – volume-title: Modeling of the Long-Term Water Level Oscillations in the Caspian Sea: Theory and Practice year: 2003 ident: 6853_CR24 contributor: fullname: A. V. Frolov – volume: 40 start-page: 737 year: 2004 ident: 6853_CR13 publication-title: Izv. Atmos. Ocean. Phys. contributor: fullname: A. A. 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Snippet | Long-term hourly data from 12 tide gauge stations were used to examine the character of tidal oscillations in the Caspian Sea. Diurnal and semidiurnal tidal... Long-term hourly data from 12 tide gauge stations were used to examine the character of Tidal oscillations in the Caspian Sea. Diurnal and semidiurnal tidal... |
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SubjectTerms | Amplitude Amplitudes Basins Diurnal variations Earth and Environmental Science Earth Sciences Fourier analysis Gravitation Gravity Harmonic analysis High resolution Marine Physics Ocean basins Oceanography Oscillations Physical oceanography Radiational tides Sea level Spectra Spectral analysis Stations Tidal constituents Tidal oscillations Tidal range Tide gauges Tides |
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Title | Tidal oscillations in the Caspian Sea |
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