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  • Geophysical and geological flows  (1)
  • Mediterranean Sea  (1)
  • Cambridge University Press  (2)
  • Periodicals Archive Online (PAO)
  • 2015-2019  (2)
  • 1960-1964
  • 1950-1954
  • 1
    Publication Date: 2020-12-14
    Description: We reconstructed the late Holocene relative sea-level (RSL) evolution of the ancient harbour of Naples, one of the largest coastal conurbations in the Mediterranean. We carried out multiproxy investigations, coupling archaeological evidence with biological indicators. Our data robustly constrain 2000 yr of non-monotonic changes in sea level, chiefly controlled by the complex volcano-tectonic processes that characterize the area. Between ∼200 BC and AD ∼0, a subsidence rate of more than ∼1.5 mm/yr enhanced the postglacial RSL rise, while negligible or moderate land uplift 〈 ∼0.5 mm/yr triggered a RSL stabilization during the Roman period (first five centuries AD). This stabilization was followed by a post-Roman enhancement of the sea-level rise when ground motion was negative, attested by a subsidence rate of ∼0.5 to ∼1 mm/yr. Our analysis seems to indicate very minor impacts of this nonmonotonic RSL evolution on the activities of the ancient harbour of Naples, which peaked from the third century BC to the second century AD. After this period, the progressive silting of the harbour basin made it impossible to safely navigate within the basin, leading to the progressive decline of the harbour.
    Description: Published
    Description: 284-298
    Description: 1V. Storia eruttiva
    Description: JCR Journal
    Keywords: Geo-archeology ; Sea-level changes ; Ancient harbours ; Naples ; Volcano-tectonics ; Mediterranean Sea ; Parthenope-Neapolis
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2022-05-25
    Description: © Cambridge University Press, 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Journal of Fluid Mechanics 786 (2016): R1, doi:10.1017/jfm.2015.642.
    Description: The onset of monami – the synchronous waving of seagrass beds driven by a steady flow – is modelled as a linear instability of the flow. Unlike previous works, our model considers the drag exerted by the grass in establishing the steady flow profile, and in damping out perturbations to it. We find two distinct modes of instability, which we label modes 1 and 2. Mode 1 is closely related to Kelvin–Helmholtz instability modified by vegetation drag, whereas mode 2 is unrelated to Kelvin–Helmholtz instability and arises from an interaction between the flow in the vegetated and unvegetated layers. The vegetation damping, according to our model, leads to a finite threshold flow for both of these modes. Experimental observations for the onset and frequency of waving compare well with model predictions for the instability onset criteria and the imaginary part of the complex growth rate respectively, but experiments lie in a parameter regime where the two modes can not be distinguished.
    Description: M.M.B. was supported by the Collective Interactions Unit, OIST Graduate University, while visiting Brown University. A.M. was supported by NSF 1131393.
    Keywords: Coastal engineering ; Geophysical and geological flows ; Instability
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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