AIFENG TAO

Prof. Dr. AIFENG TAO

College of Harbour, Coastal and Offshore Engineering, Hohai University, Nanjing 210024, China

Research Focus & Metrics

Academic Career Length

14Years (2013-Present)

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

Representative Publications

View All Publications
1 March 2024 in Ocean Engineering
Verified
Journal Article
Closed access
WXWei Xu
Wei Xu
AIFENG TAOAIFENG TAO
AIFENG TAO
RWRisheng Wang
Risheng Wang
SQShufang Qin
Shufang Qin
JFJun Fan
Jun Fan
JZJinhai Zheng
Jinhai Zheng

1 February 2022 in China Ocean Engineering
Verified
Journal Article
Closed access
PDF file
JPJi Peng
Ji Peng
AIFENG TAOAIFENG TAO
AIFENG TAO
JFJun Fan
Jun Fan
JZJin-Hai Zheng
Jin-Hai Zheng
YLYu-Ming Liu
Yu-Ming Liu

Verified
Journal Article
Open access
PDF file
OOOlorunfemi OMONIGBEHIN
Olorunfemi OMONIGBEHIN
EEEmmanuel Eresanya
Emmanuel Eresanya
AIFENG TAOAIFENG TAO
AIFENG TAO
Victor Edem SetordjieVictor Edem Setordjie
Victor Edem Setordjie
SDSamuel Daramola
Samuel Daramola
AAAbiola Adebiyi
Abiola Adebiyi
Studies on the variability in ocean wave climate provide engineers and policy makers with information to plan, develop, and control coastal and offshore activities. Ocean waves bear climatic imprints through which the global climate system can be better understood. Using the recently updated ERA5 dataset, this study evaluated the spatiotemporal distribution and variability in significant wave height (SWH) in the Eastern Tropical Atlantic (ETA). The short-term trends and rates of change were obtained using the Mann–Kendall trend test and the Theil–Sen slope estimator, respectively, and decadal trends were assessed using wavelet transformation. Significant, positive monthly and yearly trends and a prevailing decadal trend were observed across the domain. Observed trends suggest that stronger waves are getting closer to the coast and are modulated by the Southern and Northern Atlantic mid-latitude storm fields. These observations have implications for the increasing coastal erosion rates on the eastern coast of the Tropical Atlantic.

Verified
Journal Article
Open access
PDF file
HZHaiming Zhang
Haiming Zhang
AIFENG TAOAIFENG TAO
AIFENG TAO
JTJunhao Tu
Junhao Tu
JSJunwei Su
Junwei Su
SXShuya Xie
Shuya Xie
Intensive wave reflection occurs when the wavelengths of the incident waves and bottom undulations are in a 2:1 ratio. Existing studies have included the Bragg resonance phenomenon of waves passing over a continuous undulating bottom parallel to and oblique to the shoreline. More generally, the Bragg resonance mechanism is used as a means of coastal protection, rather than wave power generation. To focus the wave energy in a specific area, here, we propose sinusoidal sandbars of a horizontal V-shaped pattern, which is formed by two continuous undulating bottoms inclined at an angle to each other and the center axis of the angle is perpendicular to the shoreline. Based on the high-order spectral (HOS) numerical model, both the characteristics of Bragg resonance induced by the regular waves and random waves are investigated. In the scenario of regular waves, it shows that the wave-focusing effect is related to the angle of the V-shaped undulating bottom, and the optimal angle of inclination for the V-shaped undulating bottom is 162.24°. On that basis, considering the interactions between the random waves and the V-shaped undulating bottom of 162.24°, the Bragg resonance characteristics of random waves are studied. The BFI factor combining wave steepness and spectrum width can evaluate the focusing intensity of the Bragg resonance of the random waves. For BFI, in the range of 0.15–1.0, the values of Hsmax/Hs0 linearly increase with the increase of BFI.

22 January 2025 in Ocean Engineering
Verified
Journal Article
Closed access
WXWei Xu
Wei Xu
AIFENG TAOAIFENG TAO
AIFENG TAO
JZJian Zeng
Jian Zeng
JFJun Fan
Jun Fan
Jianhao LiuJianhao Liu
Jianhao Liu
JZJinhai Zheng
Jinhai Zheng

1 October 2023 in China Ocean Engineering
Verified
Journal Article
Closed access
PDF file
ZZZhen Zhang
Zhen Zhang
AIFENG TAOAIFENG TAO
AIFENG TAO
QWQiao-Rui Wu
Qiao-Rui Wu
YXYong-He Xie
Yong-He Xie