Sentence examples for over fluvial from inspiring English sources

Encroachment of riparian vegetation into regulated river channels exerts control over fluvial processes, channel morphology, and aquatic ecology.

The development of large-statured terrestrial vegetation in channels results in a reciprocal relationship with hydrogeomorphic processes (Corenblit and others 2007), with encroachment exerting control over fluvial processes, and in turn, channel morphology, and aquatic ecology (Hickin 1984).

And just when it was thought that all great challenges of fluvial exploration were over, there was one more: the river Bure in Norfolk.

The results reveal brief periods of fluvial deposition over the past 26 kyr.

This paper describes developments in the analysis and interpretation of Holocene fluvial chronologies over the past 25 years.

This paper proposes a simple subdivision of reduced-complexity models of river behaviour into two categories that mirror methodological developments in fluvial geomorphology over the past 50 years.

Despite these complications, these problems must be solved, as bioturbators such as crayfish and bioconsolidators such as silk-spinning caddisflies may locally modify (i) rates of transport of fluvial sediments over three orders of magnitude and (ii) frequencies of mass transport events over five orders of magnitude.

It is argued that by improving physical modelling capabilities and coupling physical and numerical models, it should be possible to improve understanding of the complex interactions and processes induced by variable forcing within fluvial systems over a broader range of time scales.

The erosional morphology preserved at the sea bed in the eastern English Channel dominantly records denudation of the continental shelf by fluvial processes over multiple glacial interglacial sea-level cycles rather than by catastrophic flooding through the Straits of Dover during the mid-Quaternary.

With this paper, we consider influences on the MRS over Neogene timescales, integrate fluvial and marine processes with the valley to shelf to deepwater regions, discuss MRS evolution through the late Pleistocene and Holocene, and conclude with an evaluation of Anthropocene MRS morphodynamics and source-to-sink connectivity in a time of profound human alteration of the system.

An important gap in existing capabilities identified in this study is the representation of fluvial systems over time scales relevant for managing the immediate impacts of global climatic change; 101 – 102 years, the representation of variable forcing (e.g. storms), and the representation of biological processes.