Seasonal variations of tidal currents in the deep Timor Passage

Exact knowledge on the seasonal variations of main tidal constituents is beneficial for improving tidal prediction. The semi-annual cycles in K1 and S2 tides are abnormally exaggerated by astronomical P1 and K2 tides, which interferes with our understanding on tidal seasonality. The widely-used tida...

Full description

Bibliographic Details
Main Authors: Haidong Pan, Junchuan Sun, Tengfei Xu, Fei Teng, Zexun Wei
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-02-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2023.1135911/full
_version_ 1797905038615511040
author Haidong Pan
Haidong Pan
Haidong Pan
Haidong Pan
Junchuan Sun
Junchuan Sun
Junchuan Sun
Junchuan Sun
Tengfei Xu
Tengfei Xu
Tengfei Xu
Tengfei Xu
Fei Teng
Fei Teng
Fei Teng
Fei Teng
Zexun Wei
Zexun Wei
Zexun Wei
Zexun Wei
author_facet Haidong Pan
Haidong Pan
Haidong Pan
Haidong Pan
Junchuan Sun
Junchuan Sun
Junchuan Sun
Junchuan Sun
Tengfei Xu
Tengfei Xu
Tengfei Xu
Tengfei Xu
Fei Teng
Fei Teng
Fei Teng
Fei Teng
Zexun Wei
Zexun Wei
Zexun Wei
Zexun Wei
author_sort Haidong Pan
collection DOAJ
description Exact knowledge on the seasonal variations of main tidal constituents is beneficial for improving tidal prediction. The semi-annual cycles in K1 and S2 tides are abnormally exaggerated by astronomical P1 and K2 tides, which interferes with our understanding on tidal seasonality. The widely-used tidal inference method in previous studies cannot fully separate astronomical P1 and K2 tides from seasonal P1 and K2 tides due to inaccurate inference relationship. In this study, on the basis of the ‘credo of smoothness’ which indicates that tidal admittances are smooth functions of tidal frequencies, we develop a novel but simple method to address this intractable issue and applied this method to explore the seasonality of tidal currents observed in the deep Timor Passage at the depth of 1800m. We find that the timing and range of seasonal modulations of M2, S2, K1, and O1 tides are distinct. Annual variations in tidal currents are much stronger than semi-annual variations in tidal currents. The annual and semi-annual ranges of M2 tide can reach 2.69 cm/s and 1.51 cm/s, which are largest among main constituents. Although the annual range of K1 tide is only 1.85 cm/s, considering the relatively small amplitude of time-averaged K1 tide (2.87cm/s), K1 the most affected tide by the annual cycle. The seasonal cycles of semi-diurnal tides (M2 and S2) are basically synchronous while those of diurnal tides (K1 and O1) are generally out-of-phase. As a general method, the proposed method can be widely applied to other sea areas to explore local tidal seasonality.
first_indexed 2024-04-10T09:58:43Z
format Article
id doaj.art-48d7615bbb654f3b93ef85fddaedcbe4
institution Directory Open Access Journal
issn 2296-7745
language English
last_indexed 2024-04-10T09:58:43Z
publishDate 2023-02-01
publisher Frontiers Media S.A.
record_format Article
series Frontiers in Marine Science
spelling doaj.art-48d7615bbb654f3b93ef85fddaedcbe42023-02-16T11:27:12ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452023-02-011010.3389/fmars.2023.11359111135911Seasonal variations of tidal currents in the deep Timor PassageHaidong Pan0Haidong Pan1Haidong Pan2Haidong Pan3Junchuan Sun4Junchuan Sun5Junchuan Sun6Junchuan Sun7Tengfei Xu8Tengfei Xu9Tengfei Xu10Tengfei Xu11Fei Teng12Fei Teng13Fei Teng14Fei Teng15Zexun Wei16Zexun Wei17Zexun Wei18Zexun Wei19Key Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modeling, Qingdao, ChinaPilot National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modeling, Qingdao, ChinaKey Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modeling, Qingdao, ChinaPilot National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modeling, Qingdao, ChinaKey Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modeling, Qingdao, ChinaPilot National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modeling, Qingdao, ChinaKey Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modeling, Qingdao, ChinaPilot National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modeling, Qingdao, ChinaKey Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modeling, Qingdao, ChinaPilot National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modeling, Qingdao, ChinaExact knowledge on the seasonal variations of main tidal constituents is beneficial for improving tidal prediction. The semi-annual cycles in K1 and S2 tides are abnormally exaggerated by astronomical P1 and K2 tides, which interferes with our understanding on tidal seasonality. The widely-used tidal inference method in previous studies cannot fully separate astronomical P1 and K2 tides from seasonal P1 and K2 tides due to inaccurate inference relationship. In this study, on the basis of the ‘credo of smoothness’ which indicates that tidal admittances are smooth functions of tidal frequencies, we develop a novel but simple method to address this intractable issue and applied this method to explore the seasonality of tidal currents observed in the deep Timor Passage at the depth of 1800m. We find that the timing and range of seasonal modulations of M2, S2, K1, and O1 tides are distinct. Annual variations in tidal currents are much stronger than semi-annual variations in tidal currents. The annual and semi-annual ranges of M2 tide can reach 2.69 cm/s and 1.51 cm/s, which are largest among main constituents. Although the annual range of K1 tide is only 1.85 cm/s, considering the relatively small amplitude of time-averaged K1 tide (2.87cm/s), K1 the most affected tide by the annual cycle. The seasonal cycles of semi-diurnal tides (M2 and S2) are basically synchronous while those of diurnal tides (K1 and O1) are generally out-of-phase. As a general method, the proposed method can be widely applied to other sea areas to explore local tidal seasonality.https://www.frontiersin.org/articles/10.3389/fmars.2023.1135911/fullocean tidestidal currentsharmonic analysisseasonal modulationdeep ocean
spellingShingle Haidong Pan
Haidong Pan
Haidong Pan
Haidong Pan
Junchuan Sun
Junchuan Sun
Junchuan Sun
Junchuan Sun
Tengfei Xu
Tengfei Xu
Tengfei Xu
Tengfei Xu
Fei Teng
Fei Teng
Fei Teng
Fei Teng
Zexun Wei
Zexun Wei
Zexun Wei
Zexun Wei
Seasonal variations of tidal currents in the deep Timor Passage
Frontiers in Marine Science
ocean tides
tidal currents
harmonic analysis
seasonal modulation
deep ocean
title Seasonal variations of tidal currents in the deep Timor Passage
title_full Seasonal variations of tidal currents in the deep Timor Passage
title_fullStr Seasonal variations of tidal currents in the deep Timor Passage
title_full_unstemmed Seasonal variations of tidal currents in the deep Timor Passage
title_short Seasonal variations of tidal currents in the deep Timor Passage
title_sort seasonal variations of tidal currents in the deep timor passage
topic ocean tides
tidal currents
harmonic analysis
seasonal modulation
deep ocean
url https://www.frontiersin.org/articles/10.3389/fmars.2023.1135911/full
work_keys_str_mv AT haidongpan seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT haidongpan seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT haidongpan seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT haidongpan seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT junchuansun seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT junchuansun seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT junchuansun seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT junchuansun seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT tengfeixu seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT tengfeixu seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT tengfeixu seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT tengfeixu seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT feiteng seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT feiteng seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT feiteng seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT feiteng seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT zexunwei seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT zexunwei seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT zexunwei seasonalvariationsoftidalcurrentsinthedeeptimorpassage
AT zexunwei seasonalvariationsoftidalcurrentsinthedeeptimorpassage