scholarly journals Storm surge development in the Southern North Sea and the Elbe river in Europe during the last century and its practical application

MAUSAM ◽  
2021 ◽  
Vol 48 (4) ◽  
pp. 499-514
Author(s):  
GABRIELE GONNERT ◽  
WINFRIED SIEFERT

ABSTRACT. The development of storm surges during the last century in the European North Sea and the Elbe River is presented. The results show an increase in the number of the storm tides and the storm surge curves, but no increase in the level. The reason for the increase of the storm surge curves - especially those with more than one storm tide crest - must be an increase of the wind duration. With the analyses of the storm surge curve and the storm surge peak, it is possible to calculate the design dike level.    

Chemosphere ◽  
2001 ◽  
Vol 45 (3) ◽  
pp. 245-259 ◽  
Author(s):  
O.P Heemken ◽  
H Reincke ◽  
B Stachel ◽  
N Theobald

2021 ◽  
Author(s):  
Elke M. I. Meyer ◽  
Ralf Weisse ◽  
Iris Grabemann ◽  
Birger Tinz ◽  
Robert Scholz

Abstract. Storm tides represent a major threat to the low-lying German North Sea coast. Knowledge of extremes is essential for the design of reliable and robust coastal defences. A storm tide that occurred on 12–13 March 1906 along the German Bight coastline still represents one of the strongest events on record. For this event, detailed knowledge of atmospheric and hydrodynamic conditions is still lacking. To assess the potential impact of such an event on today’s coastline, century-long atmospheric reanalysis data together with a manual synoptic reconstruction based on archived weather data were used to drive a tide-surge model and to simulate water levels during the event. Sensitivity experiments were performed to estimate potential amplification of water levels that could have been caused by different time lags between the storm and the astronomical tide. Comparison between the model results and the limited available observational data indicated, that the water levels could be reasonably reconstructed using wind fields from the manual synoptic approach and some of the reanalysis ensemble members. The amplification potential was found to be low because the storm occurred during spring tide and shifts in the phase of the astronomic tide yielded only small changes in total water levels. To summarize, if pressure data are available at relevant locations, historical storm surges can be simulated with reanalysis products and also with a manual synoptic reconstruction.


2015 ◽  
Vol 146 ◽  
pp. 120-145 ◽  
Author(s):  
Thomas Spencer ◽  
Susan M. Brooks ◽  
Ben R. Evans ◽  
James A. Tempest ◽  
Iris Möller

Author(s):  
David F. Kelly ◽  
Ewelina Luczko ◽  
Michael Fullarton ◽  
Yahia Kala

In this paper we present the results of a multimodel approach to simulating the recent storm surges due to hurricanes Irma and Maria. The study focuses on Puerto Rico which, as a consequence of hurricane Maria, experienced storm surge around the entire perimeter of the island. In this study the storm tide is modeled using a variety of state-of-the-art 2DH numerical models. All models are based on the long wave assumption and employ the Non-Linear Shallow Water (NLSW) equations. The models vary according to the form of the governing NLSW equations that they employ. Differences include linearization and primitive variable or conserved variable (divergence) form. The numerical solution techniques used to solve the governing equations, as well as the options available for the wind, pressure, tidal forcing terms and wetting/drying techniques also vary between (and within) the models.


Author(s):  
Park Mao

A storm surge, storm flood or storm tide is a coastal flood or tsunami-like phenomenon of rising water commonly associated with low pressure weather systems (such as tropical cyclones and strong extra-tropical cyclones), the severity of which is affected by the shallowness and orientation of the water body relative to storm path, as well as the timing of tides. Most casualties during tropical cyclones occur as the result of storm surges. It is a measure of the rise of water beyond what would be expected by the normal movement related to tides. The two main meteorological factors contributing to a storm surge are a long fetch of winds spiraling inward toward the storm, and a low-pressure-induced dome of water drawn up under and trailing the storm's center.


2021 ◽  
Author(s):  
Holger Brix ◽  
Norbert Kamjunke ◽  
Ingeborg Bussmann ◽  
Eric Achterberg ◽  
Peter Dietrich ◽  
...  

<p>Understanding river-sea-systems requires a thorough understanding of processes that span different Earth system compartments. To overcome issues related to the interaction of different scientific disciplines and compartments, such as different measurement and calibration standards, quality control approaches and data formats for specific environmental parameters, joint measurement campaigns have been initiated within the Helmholtz Association’s MOSES (Modular Observation Solutions for Earth Systems) project. Following multiple senor comparison and intercalibration campaigns in 2019, MOSES’ Hydrological Extremes event chain working group initiated joint field campaigns in summer 2020 covering the Elbe river from the Czech-German border to the tidal Elbe and further on into the estuary and the German Bight.</p><p>The fundamental objective was to establish scientifically sound and resilient multi-ship applicable sampling procedures and to create reference data for the main environmental parameters for future investigation of extreme events such as flooding and drought and their overall impact on the catchment region and the adjacent estuarine area of a large European fresh water / marine system. The campaign involved four research vessels, four research centers and spanned nearly two months. Measurements included standard hydrological and oceanographic parameters, as well as quantities relevant to the nutrient and carbonate system. Furthermore, selected water quality indicators and atmospheric measurements were performed. In the fresh water section of the Elbe river measurements were taken while drifting with the water mass. In the tidal section of the river sampling was done against the ebb current while in the North Sea a grid covering a large part of the German exclusive economic zone (EEZ) was sampled.</p><p>We detected a longitudinal increase of phytoplankton biomass along the 585 km freshwater part of the river towards the tidal system. In contrast, concentrations of dissolved nitrate and phosphate decreased to low values due the uptake by planktonic algae. The concentration of dissolved CO<sub>2</sub> decreased caused by increasing photosynthesis while the concentration of methane increased along the river stretch, particularly in the most downstream part when sedimentation of phytoplankton increased the organic load of sediments. The tidal part of the transect showed a strong influence of Hamburg harbor on almost all quantities, while downstream towards the estuary, the effects of the tidal cycle dominated variabilities. In the marine area, elevated chlorophyll concentrations were mainly found near the west coast of Schleswig-Holstein, probably mostly influenced by the Eider river outflow or the adjacent tidal flats. While most of the measured parameters showed an expected behavior relative to their individual compartments, the transfer of quantities between the compartments revealed rather complex and sometimes difficult to understand behaviors and patterns, especially when considering a functional quantitative analysis. The first results of this trans-compartment campaign showed that a quantitative understanding of the fate and dynamics of water constituents across compartments from the spring to the sea needs enhanced scientific collaboration and awareness to finally come to a better integrated understanding of physical, biogeochemical and biological processes from the local to the global scale.</p>


2012 ◽  
Vol 191 (2) ◽  
pp. 569-578 ◽  
Author(s):  
Jianghui Geng ◽  
Simon D.P. Williams ◽  
Felix N. Teferle ◽  
Alan H. Dodson

A numerical model has been formulated to provide predictions of surge levels in the southern North Sea and River Thames. The model has been used to simulate the disastrous surge of January-February 1953. It is shown that the major surge component along the east coast of England was that propagating from the northern North Sea, whereas along the Dutch coast the major component was due to the wind effect over the southern North Sea. During the course of the storm there was a large net transport of water southwards through the Dover Strait. This residual flow was found to affect the surge levels at Southend. An investigation has been made of the effect of deploying the future Thames Barrier during the course of the storm. At Southend the amplitude of the reflected wave from the barrier was found to be negligible. The distribution of energy during the storm has been examined and a plot made of the spatial variation in energy dissipation by bed friction.


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