Characteristics of Tidal in Surabaya

Engki Andri Kisnarti

doi:10.4028/www.scientific.net/AMM.862.46

Paper Titles

Characteristics of High Growth Casuarina equisetifolia and High Inundation of Tsunami when Propagating through Greenbelt Vertical Rod
p.21

Shoreline Changes Dynamics at Bangkalan Regency
p.27

Shoreline Changes in Tuban District in East Java Caused by Sea Level Rise Using Bruun Rule and Hennecke Methods
p.34

Analysis of East Surabaya Shoreline Determination Using Tidal Data, Image Satellite and RTK-GNSS
p.41

Characteristics of Tidal in Surabaya
p.46

Preliminary Assessment of Wave Energy Potential around Indonesia Sea
p.55

Oceanography Data Processing Online Using Internet
p.61

Seasonally Variation of Significant Wave Height for 25 Year Period Based on JMA/MRI-AGCM3.2 Wind Climate Data
p.67

Prediction of Significant Wave Height Using Neural Network in the Java Sea (North of Surabaya)
p.72

HomeApplied Mechanics and MaterialsApplied Mechanics and Materials Vol. 862Characteristics of Tidal in Surabaya

Characteristics of Tidal in Surabaya

Abstract:

Ocean tides are the result of gravitational and centrifugal effect. Tidal motion in certain places does not only depend on the gravity moon and sun, but also by non-astronomical factors. The purpose of this study is to analyze the characteristics of the tides in Surabaya. The Methodology of this research are data collection, calculation using admiralthy methods, harmonic analysis, and trend analysis. The results showed that the waters of Surabaya has a type of tidal mixed semi diurnal. Results of the analysis of the tides in the Port of Perak shows there has been a rise in the function y = 0.0164 (x) + 156.86 every month from January 1994 - December 2009 or 1.97 mm per year. The lowest Mean Sea Level (MSL) occurred in January 1998, which is 141 cm. MSL in Surabaya unstable to Western Monsoon ends. The highest MSL occurs in transition between Eastern Monsoon towards the Western Monsoon, April 2008 amounted to 179 cm.

You might also be interested in these eBooks

View Preview

Info:

Periodical:

Applied Mechanics and Materials (Volume 862)

Pages:

46-51

DOI:

https://doi.org/10.4028/www.scientific.net/AMM.862.46

Citation:

Cite this paper

Online since:

January 2017

Authors:

Engki Andri Kisnarti*

Keywords:

Monsoon, Tidal, Wind

Export:

RIS, BibTeX

Price:

Permissions CCC:

Request Permissions

Permissions PLS:

Request Permissions

Сopyright:

Citation:

* - Corresponding Author

References

[1] L. Kurniawan, Analisis Harmonik Pasang Surut Pantai Teluk Prigi, Jawa Timur (Upaya Antisipasi terhadap Tsunami), Jurnal Alami, 2000, Volume 5 No. 2, Jakarta.

Google Scholar

[2] J.I. Pariwono, Gaya Penggerak Pasang Surut dalam Pasang Surut, LIPI, Jakarta, (1989).

Google Scholar

[3] D. K. Mihardja, dan R. Setiadi, Analisis Pasang Surut di Daerah Cilacap dan Surabaya, Pusat Penelitian dan Pengembangan Oseanologi Lembaga Ilmu Pengetahuan Indonesia, Jakarta, (1989).

DOI: 10.30556/jtmb.vol16.no1.2020.1064

Google Scholar

[4] Haryono dan S. Narni, Karakteristik Pasang Surut Laut di Pulau Jawa. Forum Teknik. Vol. 28, No. 1 (Januari 2004) 1-5.

Google Scholar

[5] Hydrographer of the Navy, Tides and Tidal Streams, Admiralty of Hydrographic Surveying, Taunton, (1969).

Google Scholar

[6] K. Wyrtki, Physical Oceanography of Southeast Asean Waters, Naga Report Vol II, University of California, La Lolla. (1961).

Google Scholar

[7] A. Wijaya, Karakteristik Angin Permukaan Skala Bulanan Stasiun Meteorologi Perak 1 Surabaya Periode Tahun 2000-2014. Laporan BMKG, (2015).

Google Scholar

[8] A Wirasatriya, A. Hartoko, Suripin, Kajian Kenaikan Muka Laut sebagai Landasan Penanggulangan Rob di Pesisir Kota Semarang. Jurnal Pasir Laut. Vol. 1 No. 2 (Januari 2006) 31-42.

DOI: 10.15578/jkn.v14i3.7583

Google Scholar