Sentence examples for tsunami field from inspiring English sources

Details of the tsunami field survey are available in Yalçiner et al. (2017).

Because of the severity and wide extent of the tsunami damage, tsunami field surveys are still ongoing.

This special issue of Earth, Planets and Space contains fifteen contributions related to the 3rd International Tsunami Field Symposium Science, Technology, and Disaster Mitigation—, which was held at the Sakura Hall in the Tohoku University, Japan during April 10 11, 2010.

A note on normal and lognormal cumulative distribution functions (CDFs), commonly used in earthquake and tsunami fields to define infrastructure fragility functions (Rossetto et al. 2013; Tarbotton et al. 2015), is warranted.

This could also be evaluated through the measured data during the post-tsunami field surveys (Gelfenbaum and Jaffe, 2003; Narayana et al., 2007; Srini-vasalu et al., 2007; Pari et al., 2008).

For some stations, recording media and tsunami records were able to be retrieved after the event as part of JMA's post-tsunami field surveys (Ofunato of the Iwate prefecture, Miyako of the Iwate prefecture, and Ayukawa of the Miyagi prefecture).

Data collected during post-tsunami field surveys were crucial to establish the relationship between the observed damage level and tsunami flow depth and/or current velocity (Reese et al. 2007; Dias et al. 2009; Leone et al. 2011; Suppasri et al. 2012; Suppasri et al. 2013).

This chapter presents results from comprehensive tsunami forensic field surveys conducted by the authors immediately following three major tsunami events: 2004 Indian Ocean Indonesia and Thailandd), 2010 Chile, and 2011 Tohoku, Japan.

During the simulation, snapshots of the tsunami height field and time series at selected stations, and sequential animations of these snapshots are made (Fig. 6).

But he emphatically agrees with the authors of the Science Advances paper that the threat posed by collapsing volcanic slope and submarine landslides has been overlooked in the tsunami hazard field.

These equations enable us to interpret and analyze the records of the tsunami velocity field through the water and the records of the ocean-bottom pressure, whereas conventional equations cannot.