Published 1977
by Costal Engineering Reserch Center, for sale by the National Technical Information Service in Fort Belvior, Va. : Dept. of Defense, Army, Corps of Engineers, Springfield, Va .
Written in English
Edition Notes
Statement | by Ralph Warren Abele, Jr. |
Series | Miscellaneous report - Coastal Engineering Research Center ; MR 77-5 |
Contributions | Coastal Engineering Research Center (U.S.) |
The Physical Object | |
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Pagination | 101 p. : |
Number of Pages | 101 |
ID Numbers | |
Open Library | OL17536654M |
An analysis of the relationship between wave and meteorological variables and beach morphology was undertaken during the summer and winter periods, , on Plum Island, Massachusetts. Variables were measured or computed bihourly, 24 hours per day, throughout both study by: 4. Analysis of short-term variations in beach morphology (and concurrent dynamic processes) for summer and winter periods, , Plum Island, Massachusetts () () Analysis of short-term variations in beach morphology (and concurrent dynamic processes) for summer and winter periods, , Plum Island, Massachusetts. To obtain Kelvin (K) readings, use formula: K = (5/9) (F ) + , ANALYSIS OF SHORT-TERM VARIATIONS IN BEACH MORPHOLOGY (AND CONCURRENT DYNAMIC PROCESSES) FOR SUMMER AND WINTER PERIODS, , PLUM ISLAND, . Analysis of short-term variations in beach morphology (and concurrent dynamic processes) for summer and winter periods, , Plum Island, Massachusetts / Related Titles. Series: Miscellaneous report - Coastal Engineering Research Center ; MR By. Abele, Ralph Warren.
Analysis of short-term variations in beach morphology (and concurrent dynamic processes) for summer and winter periods, , Plum Island, Massachusetts / by Ralph Warren Abele, : Ralph Warren. Abele. Trends of shoreline changes need a scientific study as erosion affects the coastal ecosystem and environment. This study focuses on the trends of shoreline changes along the Van Island, Gulf of Mannar, during the period from to using the Digital Shoreline Analysis System model of a tool in Arc Map. Shorelines were extracted from the Landsat OLI and ETM+ satellite data from the Cited by: 8. Continuous Argus video data and fortnightly measurements of subaerial morphology were obtained over a 3-year period from a steep macrotidal gravel beach on the southwest coast of the U.K. 1 Review. This is an updated and substantially revised edition of Peter Matthews's well-known Morphology, first published in It includes chapters on inflectional and lexical morphology, derivational processes and productivity, compounds, paradigms, and much new material on markedness and other aspects of iconicity.5/5(1).
In this study, variogram modelling and ordinary kriging were used to determine short-term changes in beach morphology and sand budget, based on daily surveys of 16 beach profiles along a m. Beach Morphology Analysis Package (BMAP) Version 1 [COASTAL ENGINEERING RESEARCH CENTER VICKSBURG MS] on *FREE* shipping on qualifying offers. Beach Morphology Analysis Package (BMAP) Version 1Author: COASTAL ENGINEERING RESEARCH CENTER VICKSBURG MS. Management of sandy beaches 7. This article discusses the morphology and morphodynamics of sandy beach environments. Sandy beach morphology is characterized by a sloping profile with secondary morphological features superimposed, including nearshore bars, swash bars, rip channels, beach cusps. The most marked beach profile variations were recorded on the lower shoreface, between the MSL and MLWS (mean low water spring). On the upper part of the profile, beach cusps and transverse bars were identified, especially during May Erosion prevailed between May and February (Fig. 7).