Khan Faisal Ahmed, Khan Tariq Masood Ali, Ahmed Ali Najah, Afan Haitham Abdulmohsin, Sherif Mohsen, Sefelnasr Ahmed, El-Shafie Ahmed
Institute of Environmental Studies, University of Karachi, Karachi 75270, Pakistan.
Institute for Energy Infrastructure (IEI), Universiti Tenaga Nasional (UNITEN), Kajang 43000, Selangor, Malaysia.
Entropy (Basel). 2020 May 14;22(5):549. doi: 10.3390/e22050549.
In this study, the analysis of the extreme sea level was carried out by using 10 years (2007-2016) of hourly tide gauge data of Karachi port station along the Pakistan coast. Observations revealed that the magnitudes of the tides usually exceeded the storm surges at this station. The main observation for this duration and the subsequent analysis showed that in June 2007 a tropical Cyclone "Yemyin" hit the Pakistan coast. The joint probability method (JPM) and the annual maximum method (AMM) were used for statistical analysis to find out the return periods of different extreme sea levels. According to the achieved results, the AMM and JPM methods erre compatible with each other for the Karachi coast and remained well within the range of 95% confidence. For the JPM method, the highest astronomical tide (HAT) of the Karachi coast was considered as the threshold and the sea levels above it were considered extreme sea levels. The 10 annual observed sea level maxima, in the recent past, showed an increasing trend for extreme sea levels. In the study period, the increment rates of 3.6 mm/year and 2.1 mm/year were observed for mean sea level and extreme sea level, respectively, along the Karachi coast. Tidal analysis, for the Karachi tide gauge data, showed less dependency of the extreme sea levels on the non-tidal residuals. By applying the Merrifield criteria of mean annual maximum water level ratio, it was found that the Karachi coast was tidally dominated and the non-tidal residual contribution was just 10%. The examination of the highest water level event (13 June 2014) during the study period, further favored the tidal dominance as compared to the non-tidal component along the Karachi coast.
在本研究中,利用巴基斯坦沿海卡拉奇港站10年(2007 - 2016年)的每小时验潮仪数据对极端海平面进行了分析。观测结果表明,该站的潮汐幅度通常超过风暴潮。对这一时间段的主要观测及后续分析显示,2007年6月一场热带气旋“耶明”袭击了巴基斯坦海岸。采用联合概率法(JPM)和年最大值法(AMM)进行统计分析,以确定不同极端海平面的重现期。根据所得结果,AMM和JPM方法在卡拉奇海岸相互兼容,且均处于95%置信区间范围内。对于JPM方法,将卡拉奇海岸的最高天文潮(HAT)视为阈值,高于该值的海平面被视为极端海平面。过去10年观测到的年海平面最大值显示,极端海平面呈上升趋势。在研究期内,卡拉奇海岸平均海平面和极端海平面的上升速率分别为3.6毫米/年和2.1毫米/年。对卡拉奇验潮仪数据的潮汐分析表明,极端海平面对非潮汐残差的依赖性较小。通过应用平均年最大水位比的梅里菲尔德准则,发现卡拉奇海岸以潮汐为主,非潮汐残差的贡献仅为10%。对研究期内最高水位事件(2014年6月13日)的考察进一步表明,与卡拉奇海岸的非潮汐分量相比,潮汐占主导地位。