Author: O. Sibul
Publisher:
ISBN:
Category :
Languages : en
Pages : 50
Book Description
Laboratory Studies of Wind Tides in Shallow Water
Author: O. Sibul
Publisher:
ISBN:
Category :
Languages : en
Pages : 50
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages : 50
Book Description
Interim Report on Laboratory Studies of Wind Tides in Shallow Water
Author: Osvald Sibul
Publisher:
ISBN:
Category : Tides
Languages : en
Pages : 54
Book Description
Publisher:
ISBN:
Category : Tides
Languages : en
Pages : 54
Book Description
Laboratory Study of Wind Tides in Shallow Water
Author: Osvald J. Sibul
Publisher:
ISBN:
Category : Storm surges
Languages : en
Pages : 60
Book Description
Publisher:
ISBN:
Category : Storm surges
Languages : en
Pages : 60
Book Description
Interim Report
Author: Osvald Sibul
Publisher:
ISBN:
Category : Storm surges
Languages : en
Pages : 64
Book Description
Publisher:
ISBN:
Category : Storm surges
Languages : en
Pages : 64
Book Description
Laboratory Study of Wind Tides in Shallow Water
Author: Osvald Sibul
Publisher:
ISBN:
Category : Storm surges
Languages : en
Pages : 66
Book Description
Publisher:
ISBN:
Category : Storm surges
Languages : en
Pages : 66
Book Description
Laboratory Study of Wind Tides in Shallow Water
Author: O. J. Sibul
Publisher:
ISBN:
Category : Storm surges
Languages : en
Pages : 32
Book Description
Publisher:
ISBN:
Category : Storm surges
Languages : en
Pages : 32
Book Description
Transient Wind Tides in Shallow Water
Author: Ernest Glenn Tickner
Publisher:
ISBN:
Category : Beach erosion
Languages : en
Pages : 62
Book Description
Publisher:
ISBN:
Category : Beach erosion
Languages : en
Pages : 62
Book Description
Laboratory Study of the Generation of Wind Waves in Shallow Water (Classic Reprint)
Author: Osvald J. Sibul
Publisher: Forgotten Books
ISBN: 9781397356567
Category : Science
Languages : en
Pages : 44
Book Description
Excerpt from Laboratory Study of the Generation of Wind Waves in Shallow Water The prediction of wave characteristics in shallow water is of great importance along much of the Gulf Coast of the United States, as well as for many inland water areas (as Lake Okeechobee, Florida). This has been difficult in the past as the effect of the shallow bottom is considerable, particularly in reducing the wave height from what would be expected by use of the deep water wave prediction methods. This report gives the results of some laboratory studies of wave generation in shallow water in a small enclosed wind-wave tank. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
Publisher: Forgotten Books
ISBN: 9781397356567
Category : Science
Languages : en
Pages : 44
Book Description
Excerpt from Laboratory Study of the Generation of Wind Waves in Shallow Water The prediction of wave characteristics in shallow water is of great importance along much of the Gulf Coast of the United States, as well as for many inland water areas (as Lake Okeechobee, Florida). This has been difficult in the past as the effect of the shallow bottom is considerable, particularly in reducing the wave height from what would be expected by use of the deep water wave prediction methods. This report gives the results of some laboratory studies of wave generation in shallow water in a small enclosed wind-wave tank. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
Transient Wind Tides in Shallow Water
Author: Ernest Glenn Tickner
Publisher:
ISBN:
Category : Beach erosion
Languages : en
Pages : 64
Book Description
Publisher:
ISBN:
Category : Beach erosion
Languages : en
Pages : 64
Book Description
Transient Wind Tides in Shallow Water
Author: Ernest Glenn Tickner
Publisher:
ISBN:
Category : Storm surges
Languages : en
Pages : 1
Book Description
Transient wind tides were studied in a laboratory channel with various water depths and wind velocities. The transient wind tide studies were divided into two parts: (1) the surface time history, and (2) the transient water motion. The water surface set-up will overshoot its steady-state value by a factor of 2. This factor is slightly higher for the deeper water depth and smaller for the shallower water depths. The surface current reaches steadystate very quickly and has a value of 1/30 of the average wind velocity passing over the surface for a Reynolds number of 2000 or greater. The water also oscillates, and one can predict its oscillatory magnitude by using the standing wave equations with the wave height, the height of the maximum set-up. Finally, a return flow in the lower layers overcomes the slowly damped oscillatory motion and a steady-state flow is established. (Author).
Publisher:
ISBN:
Category : Storm surges
Languages : en
Pages : 1
Book Description
Transient wind tides were studied in a laboratory channel with various water depths and wind velocities. The transient wind tide studies were divided into two parts: (1) the surface time history, and (2) the transient water motion. The water surface set-up will overshoot its steady-state value by a factor of 2. This factor is slightly higher for the deeper water depth and smaller for the shallower water depths. The surface current reaches steadystate very quickly and has a value of 1/30 of the average wind velocity passing over the surface for a Reynolds number of 2000 or greater. The water also oscillates, and one can predict its oscillatory magnitude by using the standing wave equations with the wave height, the height of the maximum set-up. Finally, a return flow in the lower layers overcomes the slowly damped oscillatory motion and a steady-state flow is established. (Author).