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首页> 外文期刊>Indian Journal of Marine Sciences >Morpho-dynamic evolution of Ekakula spit of Odisha coast, India using satellite data
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Morpho-dynamic evolution of Ekakula spit of Odisha coast, India using satellite data

机译:利用卫星数据对印度奥里萨哈海岸Ekakula吐水的形态动力学演变

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摘要

Ekakula spit is at the northern end of Gahirmatha coast in the state of Odisha, India. This spit is located at the mouth of Maipura river, which is falling in the northern side of Mahanadi delta region. This spit is a prominent and important for many reasons because it triggers interests to the coastal managers and environmentalists because of its nature. Multi temporal satellite images (1999-2009) were used to study the Morpho-dynamic evolution of this spit. Results show that the spit grows towards northeast mainly by the deposition of sand brought by the littoral drift from the south. In the past, it got fragmented and detached portion moved away towards the offshore. Temporal satellite images revealed the progressive evolution of the spit. Spit appears to have undergone growth and fragmentation over the years and accordingly the Maipura river mouth shifted back and forth. The growth of the spit forces the river to shift its mouth and the river causes the fragmentation by breaching the spit during heavy floods. Ekakula spit lost about 306 m when compared its position in 1973 (SOI toposheet) to the satellite image of 1999. The year-wise length of the Ekakula spit was estimated using satellite data for the period 1999-2009 from a base point selected for this purpose. Ekakula spit length increased since 1999 by 2710 m by 2008 and little reduced to 2431 m during 2008-2009. Spit appears to be growing steadily by the deposition of sediment brought from south by the littoral drift except during 2003 and 2009 when it suffered some erosion. Maximum increase in length was during 2004-2005 followed by 2000-2001 and 1999-2000. Minimum was during 2004-2005. Erosion was minimal during 2002-2003.
机译:Ekakula唾液位于印度奥里萨邦Gahirmatha海岸的北端。该唾液位于Maipura河口处,该河落在Mahanadi三角洲地区的北侧。由于许多原因,这种吐痰是突出和重要的,因为它的性质会引起沿海管理者和环保主义者的兴趣。使用多时相卫星图像(1999-2009年)来研究该唾液的形态动力学演化。结果表明,该唾液向东北方向生长主要是由于从南部沿岸漂流带来的沙子沉积。过去,它的碎片和分离部分移向了海上。时间卫星图像显示了唾液的逐渐发展。多年来,唾液似乎经历了生长和破碎,因此迈普拉河河口来回移动。吐口水的增长迫使河流向河口方向移动,在大洪水期间,河流因冲破吐口水而导致支离破碎。与1973年的卫星图像相比,埃卡库拉(Ekakula)唾液损失了1973年(SOI拓扑表)的位置,与1999年的卫星图像相比损失了约306 m。使用从1999-2009年为此选择的基准点的卫星数据估算了埃卡库拉(Ekakula)唾液的年长度目的。自1999年以来,Ekakula的吐水口长度到2008年增加了2710 m,而在2008-2009年间几乎没有减少到2431 m。除沿岸漂流从南部带来的沉积物沉积外,沙嘴似乎正在稳定增长,除非在2003年和2009年期间遭受了一些侵蚀。长度的最大增加是2004-2005年,其次是2000-2001年和1999-2000年。最低要求是2004-2005年。在2002-2003年期间,侵蚀最小。

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