Moritz Zemann

Dr. Moritz Zemann

orcid

Research Focus & Metrics

Academic Career Length

4Years (2023-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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5 July 2024
Verified
Book Chapter
Closed access
PDF file
AAAndreas Abecker
Andreas Abecker
FFFrank Fuchs-Kittowski
Frank Fuchs-Kittowski
JJJulian Janßen
Julian Janßen
RMRuben Müller
Ruben Müller
BPBernd Pfützner
Bernd Pfützner
MZMoritz Zemann
Moritz Zemann

12 January 2023
Verified
Other
Open access
MZMoritz Zemann
Moritz Zemann
RLRoderick van der Linden
Roderick van der Linden
DCDan Trinh Cong
Dan Trinh Cong
VDVũ Hoàng Thái Dương
Vũ Hoàng Thái Dương
NNNguyet Minh Nguyen
Nguyet Minh Nguyen
AFAndreas H. Fink
Andreas H. Fink


12 January 2023 in EGUsphere
Verified
Preprint
Open access
PDF file
MZMoritz Zemann
Moritz Zemann
RLRoderick van der Linden
Roderick van der Linden
DCDan Trinh Cong
Dan Trinh Cong
VDVũ Hoàng Thái Dương
Vũ Hoàng Thái Dương
NNNguyet Minh Nguyen
Nguyet Minh Nguyen
AFAndreas H. Fink
Andreas H. Fink
Against the background of the rising sea level and land subsidence, protecting the progressively eroding coast along the Vietnam Mekong Delta becomes of tremendous importance. Within the presented work, design conditions for breakwaters were derived from offshore climate reanalysis data (ERA5), which were transferred to the nearshore by two numerical approaches, i.e. SwanOne and Delft3D, for different average and extreme wave and weather conditions. Within this process, design wave heights and periods at the nearshore could be determined for 10- to 100-year recurrence intervals. Both models thereby showed sufficient accuracy according to measurements in the field. Limitations must be made regarding the available spatio-temporal resolution, where reanalysis data showed a lack of short but high peak values compared to the observed measurements. Both numerical approaches showed their capabilities, where SwanOne offers a simple and fast calculation method, while it lacks of continuous effects like wind-generated swell or bottom friction. The Delft3D software on the other hand provides a more complete representation, not only of wave but also current dynamics, while it requires a much broader amount of input parameters and more complex boundary conditions. Within this study, the advantages and disadvantages of both models could be demonstrated, whereas for the final calculation of nearshore wave characteristics, only SwanOne was applicable based on the input parameters extracted from statistical analysis of long term ERA5 data.

Verified
Journal Article
Open access
PDF file
VDVũ Hoàng Thái Dương
Vũ Hoàng Thái Dương
MZMoritz Zemann
Moritz Zemann
RLRoderick van der Linden
Roderick van der Linden
DTDan Trinh
Dan Trinh
POPeter Oberle
Peter Oberle
TXTu Le Xuan
Tu Le Xuan
In the presented work, design conditions for breakwaters were derived from offshore climate reanalysis data (ERA5), which were downscaled to the nearshore by two numerical approaches, i.e., SwanOne and Delft3D, for different average and extreme wave and weather conditions. Model validation was performed using in situ measurements. The advantages and disadvantages of both numerical approaches were investigated. Both models showed sufficient accuracy according to measurements in the field, where SwanOne offers a simple and fast calculation method, while Delft3D provides a more complete representation, not only of waves but also current dynamics. However, it requires a much broader amount of input parameters and more complex boundary conditions. Then, SwanOne was applicable to calculate nearshore wave characteristics based on the input parameters extracted from the statistical analysis of long-term ERA5 data. Based on this process, design wave heights and periods at the nearshore were determined for 10- to 100-year return periods. For breakwater design on the west coast of the Mekong Delta, maximum wave heights in a range of 1.1 m to 1.3 m at a distance of 100 m to 300 m could be determined for a return period of 20 years, corresponding to water depths of 2.33 m and 2.88 m, respectively.

5 July 2024
Verified
Book Chapter
Closed access
PDF file
FBFabian Bressel
Fabian Bressel
FFFrank Fuchs-Kittowski
Frank Fuchs-Kittowski
TSTim Seegert
Tim Seegert
MDMaximilian Deharde
Maximilian Deharde
KBKonstantin Blank
Konstantin Blank
MZMoritz Zemann
Moritz Zemann