BUKU BASA POLANDIA KAKAIT KARO «MAREOGRAM»
Temukaké kagunané saka
mareogram ing pilihan bibliografi iki. Buku kang kakait dening
mareogram lan pethikan cekak kang padha kanggo nyediyakaké panggunané ing sastra Basa Polandia.
1
Report on the Chilean Tsunami of May 24, 1960, as observed ...
The mareogram obtained in Matoya Bay was excluded as the arrival time is rather late. 3. The height of tsunamis on the 100-m isobathyc line. From the above description the height of tsunamis is considered constant in the direction parallel to ...
Committee for Field Investigation of the Chilean Tsunami of 1960,
1961
2
Bulletin [of the] Disaster Prevention Research Institute
The mareogram of the 1944 Tsunami at Kobe includes a variation which was caused by the relative motion of the tide gauge with the occurrence of the earthquake. Referring to this variation and the time of occurrence the earthquake, a time ...
Kyōto Daigaku. Bōsai Kenkyūjo,
1983
3
The Geodynamics of the Aegean and Anatolia - Strona 210
1 m mareogram amplitude. This could be due to a deep basin and sudden shelf break clearly reflected in the bathymetry. However, no significant sea-wave amplitudes were calculated at locations marked in (b) with filled circles and without ...
Tuncay Taymaz, Yücel Yilmaz, Yildirim Dilek,
2007
4
Chronique de L'U.G.G.I.: I.U.G.G. Chronicle
WDC-A's future activity will be directed at completing the tsunami mareogram and photograph files through various means. For example, with the endorsement and assistance of the International Hydrographic Bureau (IHB), an article ...
International Union of Geodesy and Geophysics,
1980
5
Chronique U.G.G.I. - Strona 557
WDC-A's future activity will be directed at completing the tsunami mareogram and photograph files through various means. For example, with the endorsement and assistance of the International Hydrographic Bureau (IHB), an article ...
International Union of Geodesy and Geophysics,
1980
6
Bulletin of the Imperial Earthquake Investigation Committee
To investigate the mode of propagation of sea-waves up the river course, the time of beginning of waves at each station was estimated from the mareogram as marked by a short vertical line in Fig. 2. The time of arrival thus obtained is plotted ...
Shinsai Yobō Chōsakai (Japan),
1932
7
Journal of the College of Science, Imperial University of ...
In order to see, if any 10ng wave corresponding to this result of calculation exists actually in record, the mareogram of Karang Kleta was analysed by means of the tide-rectifier. Eliminating the great parts of diurnal and semidiurnal components, ...
Tōkyō Daigaku. Rigakubu,
1908
8
An Investigation on the Secondary Undulations of Oceanic ...
In order to see, if any long wave corresponding to this result of calculation exists actually in record, the mareogram of Karang Kleta was analysed by means of the tide- rectifier. Eliminating the great parts of diurnal and semidiurnal components, ...
Shinsai Yobō Chōsakai (Japan),
1908
9
Publications of the Earthquake Investigation Committee in ...
In order to see, if any long wave corresponding to this result of calculation exists actually in record, the mareogram of Karang Kleta was analysed by means of the tide-rectifier. Eliminating the great parts of diurnal and semidiurnal components, ...
Shinsai Yobō Chōsakai (Japan),
1908
10
The Galapagos: A Natural Laboratory for the Earth Sciences
In our study, the mareogram analysis reveals the possible existence of trapped waves oscillating in the coastal shelf. This is the case, for example, with the waves that were found in this study with periods around ten to twelve minutes at Baltra.
Karen S. Harpp, Eric Mittelstaedt, Noémi d'Ozouville,
2014