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Remote Sensing and GIS analysis for demarcation of coastal hazard line along the highly eroding Krishna-Godavari delta front

机译:沿高度侵蚀的克里希纳-哥达瓦里三角洲锋线划分海岸带危险线的遥感和GIS分析

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Coastal regions, especially river deltas are highly resourceful and hence densely populated; but these extremely low-lying lands are vulnerable to rising sea levels due to global warming threatening the life and property in these regions. Recent IPCC (2013) predictions of 26-82cm global sea level rise are now considered conservative as subsequent investigations such as by Met Office, UK indicated a vertical rise of about 190cm, which would displace 10% of the world's population living within 10 meters above the sea level. Therefore, predictive models showing the hazard line are necessary for efficient coastal zone management. Remote sensing and GIS technologies form the mainstay of such predictive models on coastal retreat and inundation to future sea-level rise. This study is an attempt to estimate the varying trends along the Krishna-Godavari (K-G) delta region. Detailed maps showing various coastal landforms in the K-G delta region were prepared using the IRS-P6 LISS 3 images. The rate of shoreline shift during a 31-year period along different sectors of the 330km long K-G delta coast was estimated using Landsat-2 and IRS-P6 LISS 3 images between 1977 and 2008. With reference to a selected baseline from along an inland position, End Point Rate (EPR), Shoreline Change Envelope (SCE) and Net Shoreline Movement (NSM) were calculated, using a GIS-based Digital Shoreline Analysis System (DSAS). The results showed that the shoreline migrated landward up to a maximum distance of 3.13km resulting in a net loss of about 42.10km~2 area during this 31-year period. Further, considering the nature of landforms and EPR, the future hazard line is predicted for the area, which also indicated a net erosion of about 57.68km~2 along the K-G delta coast by 2050 AD.
机译:沿海地区,尤其是河三角洲,资源丰富,因此人口稠密。但是由于全球变暖威胁着这些地区的生命和财产,这些地势低洼的土地容易受到海平面上升的影响。 IPCC(2013年)对全球海平面上升26-82厘米的最新预测现在被认为是保守的,因为随后的调查(如英国气象局)表明垂直上升约190厘米,这将使世界上10%的居民生活在海拔10米以内海平面。因此,显示危险线的预测模型对于有效的沿海地区管理是必要的。遥感和GIS技术构成了这种关于沿海撤退和未来海平面上升的淹没的预测模型的主体。这项研究试图估计克里希纳-戈达瓦里(K-G)三角洲地区的变化趋势。使用IRS-P6 LISS 3图像准备了详细的地图,显示了K-G三角洲地区的各种沿海地貌。使用1977年至2008年之间的Landsat-2和IRS-P6 LISS 3图像估算了31年期间沿330公里长的KG三角洲海岸不同地区的海岸线移动速率。参考从内陆位置选择的基线,使用基于GIS的数字海岸线分析系统(DSAS)计算了终点速率(EPR),海岸线变化包络(SCE)和净海岸线运动(NSM)。结果表明,在这31年的时间里,海岸线向陆地上移动的最大距离为3.13km,导致净损失约42.10km〜2。此外,考虑到地貌和EPR的性质,该地区未来的危险线已被预测,这也表明到2050年沿K-G三角洲海岸的净侵蚀量约为57.68km〜2。

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