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SEA LEVEL CHANGES ALONG THE COAST OF SANDAKAN TOWN, SABAH, MALAYSIA: PROJECTION AND INUNDATION COVERAGE

机译:沿沙坂镇海岸的海平面变化,马来西亚沙巴:投影和淹没覆盖范围

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Increase in the frequency and severity of extreme weather conditions witnessed in recent years are ostensibly linked to changing climate. Coastal areas are particularly bearing the brunt of this change. An issue that deserves serious study is the Sea Level Rise (SLR) in coastal districts, especially those with low lying areas such as Sandakan on the east coast of Sabah. Analysis of recent climate change scenario has indicated a great deal of uncertainty at global scale observation, requiring intensive examination at local level to understand vulnerability and develop adaptive capabilities. The Mean Sea Level (MSL) and sea level trends were determined from the 18 years Sandakan tidal data from the year 1994 to 2011. The analysis followed Pivot Table tools and trend line Analysis where daily average sea level trends were used to forecast the future sea level for the year 2100. MIKE 21 Flexible Mesh (FM) is the numerical model tools used to assess the hydrodynamic condition incorporated with the projected water level obtained from the regression model. Digital Terrain Model (DTM) with resolution of 30 m and approximate 300 m width from water edge was integrate with the model bathymetry to produce detail and updated bathymetry profile. The model also calibrated with measured water level data deployed at site from 10th to 22 May 2012. Geographic Information System (GIS) were used to draw the inundation map and calculate the area impacted. It is indicated MSL is at 2.706 m with sea level trends for daily is 5.3 mm/yr. The projected water level for the year 2040 and 2080 is estimated to be around 2983 mm and 3175 mm forecasted by regression model of Minitab 16 software. The numerical model simulation for the years 2020, 2040 and 2060 has indicated significant water level increment inside Sandakan Bay. Total potential inundated area for the year 2040 and 2080 are 2.41 km~2 and 2.67 km~2 respectively. The study pointed out the necessity of incorporating other factors of day-to-day influences and extreme events phenomenon with the inundation area based on tidal data analysis outcome to obtained more realistic flood inundation profiles in accordance to SLR. Evidently, sea level rise has severely creates potential future threats in term of inundation, possible flooding and erosion along the coastal area of Sandakan town.
机译:近年来目睹了极端天气条件的频率和严重程度的增加与不断变化的气候有关。沿海地区尤其符合这种变化的冲突。一个值得严肃的研究的问题是沿海地区的海平面上升(SLR),特别是那些拥有沙巴东海岸等撒巴山等低洼地区的地区。近期气候变化的分析表明了全球规模观察的大量不确定性,需要在地方一级进行密集检查以了解脆弱性和发展自适应能力。平均海平面(MSL)和海平面趋势是从1994年至2011年到2011年的18年的桑帕坎潮汐数据确定。分析遵循枢轴表工具和趋势线分析,其中日常平均海平趋势用于预测未来的海洋2100年级。迈克21灵活网格(FM)是用于评估从回归模型中获得的投影水位的流体动力学条件的数值模型工具。数字地形模型(DTM)具有30米的分辨率和从水边缘的宽度约为300米的宽度与模型沐浴浴,以产生细节和更新的沐浴曲线概况。该模型还校准了在2012年5月10日至22日在现场部署的测量水位数据。地理信息系统(GIS)用于绘制淹没地图并计算受影响的区域。它表示MSL为2.706米,每日海平面趋势为5.3毫米/年。预计2040年和2080年的投影水位估计是Minitab 16软件的回归模型预测的约2983毫米和3175毫米。 2020,2040和2060年的数值模型仿真在山羊湾内显示出显着的水位增量。 2040年和2080年的总潜在洪水区分别为2.41 km〜2和2.67 km〜2。该研究指出了基于潮汐数据分析结果基于潮汐数据分析结果的淹没面积纳入日常影响和极端事件现象的必要性,以根据SLR获得更现实的洪水淹没型材。显然,海平面上升已经严重创造了洪水沿海地区的淹没,可能的洪水和侵蚀期限的潜在未来威胁。

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