2018
DOI: 10.30730/978-5-6040621-1-1.2018-1
|View full text |Cite
|
Sign up to set email alerts
|

Investigation of the generation peculiarities of infragravity and edge waves in the coastal zone using the data of the field experiments

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
2
0

Year Published

2019
2019
2021
2021

Publication Types

Select...
2

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(2 citation statements)
references
References 0 publications
0
2
0
Order By: Relevance
“…The block diagram of the frequency meter is shown in figure 1. When conducting an experiment with several sensors, the equipment must provide the simultaneous measuring and recording of the values [6]. Usage of the personal or industrial computer could be the universal solution since modern processors have high frequency rate and software or hardware multithreading.…”
Section: Development Of the Dual-channel Frequency Meter 21 Block Diagrammentioning
confidence: 99%
“…The block diagram of the frequency meter is shown in figure 1. When conducting an experiment with several sensors, the equipment must provide the simultaneous measuring and recording of the values [6]. Usage of the personal or industrial computer could be the universal solution since modern processors have high frequency rate and software or hardware multithreading.…”
Section: Development Of the Dual-channel Frequency Meter 21 Block Diagrammentioning
confidence: 99%
“…It intensifies the Helmholtz mode in it and significantly attenuates the oscillation with a period of 36 min, which, in the presence of an adjacent bay, does not appear in Bay B. As can be seen from Table. 2, if the adjacent bay is taken into account, the Helmholtz mode of Bay B prevails over the other modes in the top of Bay B (points [12][13][14], when λ is 10 and 14 km. An increase in the width of the initial disturbance area to 16 km leads to the fact that oscillation with a period of 20 min (a standing wave arising from the interaction of an incident wave with a vertical wall) begins to prevail in Bay B.…”
Section: Periods Of Eigen-oscillations In the Baysmentioning
confidence: 99%