GLORIA

GEOMAR Library Ocean Research Information Access

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Online Resource
    Online Resource
    Institute of Electrical and Electronics Engineers (IEEE) ; 2017
    In:  IEEE Transactions on Geoscience and Remote Sensing Vol. 55, No. 2 ( 2017-2), p. 1106-1116
    In: IEEE Transactions on Geoscience and Remote Sensing, Institute of Electrical and Electronics Engineers (IEEE), Vol. 55, No. 2 ( 2017-2), p. 1106-1116
    Type of Medium: Online Resource
    ISSN: 0196-2892 , 1558-0644
    Language: Unknown
    Publisher: Institute of Electrical and Electronics Engineers (IEEE)
    Publication Date: 2017
    detail.hit.zdb_id: 2027520-1
    SSG: 16,13
    SSG: 13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Online Resource
    Online Resource
    Wiley ; 2016
    In:  Earth Surface Processes and Landforms Vol. 41, No. 14 ( 2016-11), p. 2085-2097
    In: Earth Surface Processes and Landforms, Wiley, Vol. 41, No. 14 ( 2016-11), p. 2085-2097
    Abstract: We report on a 6‐year nearshore bathymetric dataset from the Danube Delta (Romanian Black Sea coast) that comprises 16 km of erosive, stable and accumulative low‐lying micro‐tidal beaches northward of Sf. Gheorghe arm mouth. Two to three two‐dimensional longshore sandbars exhibit a net multi‐annual cyclic (2.8–5.5 years) offshore migration (20–50 m yr −1 ) in a similar way to other coasts worldwide. Bar morphology and behavior on the sediment‐rich accretionary (dissipative) sector differ substantially from that on the erosive (intermediate) sector. Shoreface slope is the most important factor controlling sandbar number and behavior. It determines different wave‐breaking patterns in the surf zone, translated into different offshore sediment transport and bar zone widths along the study site. Additionally, sediment availability, as a result of the distance from the arm mouth and of the long‐term evolution of the coast, controls the sandbar volume variability. These are all ultimately reflected in the variations of sandbar migration rates and cycle periods. A non‐dimensional morpho‐sedimentary parameter is finally presented, which expresses the bar system change potential as offshore sediment transport potential across the bar zone. Copyright © 2016 John Wiley & Sons, Ltd.
    Type of Medium: Online Resource
    ISSN: 0197-9337 , 1096-9837
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2016
    detail.hit.zdb_id: 1479188-2
    SSG: 14
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Online Resource
    Online Resource
    Wiley ; 2019
    In:  Earth Surface Processes and Landforms Vol. 44, No. 1 ( 2019-01), p. 317-330
    In: Earth Surface Processes and Landforms, Wiley, Vol. 44, No. 1 ( 2019-01), p. 317-330
    Abstract: The moisture content w s of a beach surface strongly controls the availability of sand for aeolian transport. Our predictive capability of the spatiotemporal variability in w s , which depends to a large extent on water table depth, is, however, limited. Here we show that water table fluctuations and surface moisture content observed during a 10‐day period on a medium‐grained (365 μ m) planar (1:30) beach can be predicted well with the nonlinear Boussinesq equation extended to include run‐up infiltration and a soil–water retention curve under the assumption of hydrostatic equilibrium. On the intertidal part of the beach the water table is observed and predicted to continuously fall from the moment the beach surface emerges from the falling tide to just before it is submerged by the incoming tide. We find that on the lower 30% of the intertidal beach the water table remains within 0.1–0.2 m from the surface and that the sand is always saturated ( w s ≈20 % , by mass). Higher up on the intertidal beach, the surface can dry to about 5% when the water table has fallen to 0.4–0.5 m beneath the surface. Above the high‐tide level the water table is always too deep ( 〉 0.5 m) to affect surface moisture and, without precipitation, the sand is dry ( w s   〈  5 − 8 % ). Because the water table depth on the emerged part of the intertidal beach increases with time irrespective of whether the (ocean) tide falls or rises, we find no need to include hysteresis (wetting and drying) effects in the surface‐moisture modelling. Model simulations suggest that at the present planar beach only the part well above mean sea level can dry sufficiently ( w s   〈  10 % ) for sand to become available for aeolian transport. ©2018 The Authors. Earth Surface Processes and Landforms published by John Wiley & Sons Ltd.
    Type of Medium: Online Resource
    ISSN: 0197-9337 , 1096-9837
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2019
    detail.hit.zdb_id: 1479188-2
    SSG: 14
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Online Resource
    Online Resource
    Wiley ; 2022
    In:  Earth Surface Processes and Landforms Vol. 47, No. 7 ( 2022-06-15), p. 1845-1859
    In: Earth Surface Processes and Landforms, Wiley, Vol. 47, No. 7 ( 2022-06-15), p. 1845-1859
    Abstract: An open‐source quantitative model for predicting coastal foredune growth at monthly to multi‐annual (meso)temporal scales is developed. The model builds on the established fetch framework as a surrogate for the complex micro‐scale aeolian processes on the beach, to which rain and groundwater‐induced spatiotemporal surface moisture dynamics are added as factors limiting aeolian sand supply to foredunes. The model shows great skill in an application at Egmond aan Zee, The Netherlands, with a predicted growth of 16.5 m 3 /m/yr comparing favourably to the observed growth of 17.3 m 3 /m/yr. Rain, surface moisture dynamics as well as beach width reduction by storm‐induced elevated sea levels are shown to be important factors that jointly reduce meso‐scale sand supply below the potential (i.e., unlimited) maximum, in our case study by almost 5 m 3 /m/yr. These factors are most relevant for strong (here, above 15.5 m/s) onshore winds. Consistent with expectations from the literature, meso‐scale foredune growth results primarily from moderately strong (9.5–12.5 m/s) shore‐oblique winds, which are frequent and do not result in supply‐limited conditions. At the study site these winds are most common in winter and hence foredune growth is predicted to vary seasonally, consistent with the observations. Because of the promising results we believe that our model has potential for quantifying how quickly a foredune can recover after an episodic erosion event because of storm waves.
    Type of Medium: Online Resource
    ISSN: 0197-9337 , 1096-9837
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2022
    detail.hit.zdb_id: 1479188-2
    SSG: 14
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    Online Resource
    Online Resource
    Wiley ; 2022
    In:  Earth Surface Processes and Landforms Vol. 47, No. 10 ( 2022-08), p. 2500-2517
    In: Earth Surface Processes and Landforms, Wiley, Vol. 47, No. 10 ( 2022-08), p. 2500-2517
    Abstract: For the development of climate‐resilient coastal management strategies, which focus on challenges in the decades to come, it is critical to incorporate spatial and temporal variability of coastline changes. This is particularly true for the mud‐dominated coastline of Suriname, part of the Guianas, where migrating subtidal mudbanks cause a cyclic instability of erosion and accretion of the coast that can be directly related to interbank and bank phases. The coastline hosts extensive mangrove forests, providing valuable ecosystem services to local communities. Recent studies on mudbank dynamics in Suriname predominantly focused on large‐scale trends without accounting for local variability, or on local changes considering the dynamics of a single mudbank over relatively short time scales. Here we use a remote sensing approach, with sufficient spatial and temporal resolution and full spatial and temporal coverage, to quantify the influence of mudbank migration on spatiotemporal coastline dynamics along the entire coast of Suriname. We show that migration of six to eight subtidal mudbanks in front of the Suriname coast has a strong imprint on local coastline dynamics between 1986 and 2020, with an average 32 m/yr accretion during mudbank presence and 4 m/yr retreat of the coastline during mudbank absence. Yet, coastal erosion can still occur when mudbanks are present and coastal aggregation may happen in the absence of mudbanks, exemplifying local variability and thus suggesting the importance of other drivers of coastline changes. The novel remote sensing workflow allowed us to analyse local spatial and temporal variations in the magnitude and timing of expanding and retreating trajectories. Our results demonstrate that it is essential that all coastal behaviours, including changes that cannot be explained by the migration of mudbanks, are included in multi‐decadal management frameworks that try to explain current variability, and predict future coastline changes in Suriname.
    Type of Medium: Online Resource
    ISSN: 0197-9337 , 1096-9837
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2022
    detail.hit.zdb_id: 1479188-2
    SSG: 14
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2021
    In:  Journal of Geophysical Research: Earth Surface Vol. 126, No. 6 ( 2021-06)
    In: Journal of Geophysical Research: Earth Surface, American Geophysical Union (AGU), Vol. 126, No. 6 ( 2021-06)
    Abstract: New analytical theory compares overwashing flow against barrier volume to predict breaching and washover deposition We test our theory against Delft3D simulations and Hurricane Sandy observations: vegetation and island elevation help to prevent breaching Developed barrier islands do not follow predicted trends, suggesting alternative controls on overwashing and breaching
    Type of Medium: Online Resource
    ISSN: 2169-9003 , 2169-9011
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2021
    detail.hit.zdb_id: 3094104-0
    detail.hit.zdb_id: 2130824-X
    detail.hit.zdb_id: 2138320-0
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    Online Resource
    Online Resource
    Coastal Engineering Research Council ; 2011
    In:  Coastal Engineering Proceedings , No. 32 ( 2011-01-31), p. 2-
    In: Coastal Engineering Proceedings, Coastal Engineering Research Council, , No. 32 ( 2011-01-31), p. 2-
    Abstract: To study onshore bar migration and the accompanying intra-wave sediment transport a wave flume experiment was conducted. The wave flume had a rigid bottom with a single bar profile. The focus of the experiment was to measure the hydrodynamics in the wave bottom boundary layer. The results show that the skewness of bottom stress is not only related to wave skewness but also to wave asymmetry.
    Type of Medium: Online Resource
    ISSN: 2156-1028 , 0589-087X
    Language: Unknown
    Publisher: Coastal Engineering Research Council
    Publication Date: 2011
    detail.hit.zdb_id: 2628774-2
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Online Resource
    Online Resource
    Coastal Education and Research Foundation ; 2013
    In:  Journal of Coastal Research Vol. 165 ( 2013-01-03), p. 1745-1750
    In: Journal of Coastal Research, Coastal Education and Research Foundation, Vol. 165 ( 2013-01-03), p. 1745-1750
    Type of Medium: Online Resource
    ISSN: 0749-0208 , 1551-5036
    Language: English
    Publisher: Coastal Education and Research Foundation
    Publication Date: 2013
    detail.hit.zdb_id: 53639-8
    detail.hit.zdb_id: 2156089-4
    SSG: 14
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Online Resource
    Online Resource
    MDPI AG ; 2016
    In:  Journal of Marine Science and Engineering Vol. 4, No. 1 ( 2016-02-25), p. 15-
    In: Journal of Marine Science and Engineering, MDPI AG, Vol. 4, No. 1 ( 2016-02-25), p. 15-
    Type of Medium: Online Resource
    ISSN: 2077-1312
    Language: English
    Publisher: MDPI AG
    Publication Date: 2016
    detail.hit.zdb_id: 2738390-8
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    Online Resource
    Online Resource
    MDPI AG ; 2018
    In:  Journal of Marine Science and Engineering Vol. 6, No. 4 ( 2018-10-30), p. 126-
    In: Journal of Marine Science and Engineering, MDPI AG, Vol. 6, No. 4 ( 2018-10-30), p. 126-
    Abstract: Coastal foredunes are highly dynamic landforms because of rapid erosion by waves and currents during storm surges in combination with gradual accretion by aeolian transport during more quiescent conditions. While our knowledge into the mechanisms behind foredune erosion have reached considerable maturity, this is not the case for foredune growth. High resolution spatio-temporal data sets of beach and foredune topography, which are needed to increase our understanding of mechanisms behind aeolian transport in coastal environments and to develop predictive dune-accretion models, are scarce. Here we aim to illustrate that repeated Mobile Laser Scanning (MLS) surveys provide an accurate and robust method to study detailed changes in dune volume on the timescales of months to years. An MLS system attached to an inertial navigation system with RTK-GPS (INS-GPS) was used to carry out 13 surveys along a 3.5-km Dutch beach over a 2.5-year period. The height observations were post-processed and averaged into 1 × 1 m Digital Elevation Models (DEMs). Comparison with airborne LiDAR and RTK-GPS data revealed that the obtained DEMs were accurate and robust up to a height of 15 m in the foredune above which dense vegetation hampers the MLS to see the sand surface. Estimates of dune volume change of the lower 13 m of the foredune have an uncertainty of about 0.25 m 3 /m. Time series of dune volume change show that at our study site the foredune accretes throughout the year at similar rates (10 m 3 /m/year), while marine erosion is obviously confined to storm surges. Foredune accretion and erosion vary spatially, which can, in part, be related to variations in beach width.
    Type of Medium: Online Resource
    ISSN: 2077-1312
    Language: English
    Publisher: MDPI AG
    Publication Date: 2018
    detail.hit.zdb_id: 2738390-8
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...