دانلود مقاله ISI انگلیسی شماره 143744
ترجمه فارسی عنوان مقاله

تأثیرات فانتالای سیلندر 5 گانه 5 طبقه (آوریل 2016) در آتکل فرخار، جزایر سیشل، اقیانوس هند

عنوان انگلیسی
Impacts of category 5 tropical cyclone Fantala (April 2016) on Farquhar Atoll, Seychelles Islands, Indian Ocean
کد مقاله سال انتشار تعداد صفحات مقاله انگلیسی
143744 2017 64 صفحه PDF
منبع

Publisher : Elsevier - Science Direct (الزویر - ساینس دایرکت)

Journal : Geomorphology, Volume 298, 1 December 2017, Pages 41-62

ترجمه کلمات کلیدی
جزایر صخره ای آتال، اثرات سیکلون گرمسیری، تغییرات ساحلی، مسیرهای انتقال رسوب، تجزیه و تحلیل تصویر ماهواره ای، جزایر سیشل،
کلمات کلیدی انگلیسی
Atoll reef islands; Tropical cyclone impacts; Shoreline changes; Sediment transport pathways; Satellite image analysis; Seychelles Islands;
پیش نمایش مقاله
پیش نمایش مقاله  تأثیرات فانتالای سیلندر 5 گانه 5 طبقه (آوریل 2016) در آتکل فرخار، جزایر سیشل، اقیانوس هند

چکیده انگلیسی

This paper provides new insights on the impacts of a category 5 tropical cyclone on Indian Ocean atoll reef islands. Using multi-date aerial imagery and field observations, the contribution of tropical cyclone Fantala to shoreline and island change, and to sediment production and transport, was assessed on Farquhar Atoll, Seychelles Islands. Results show that the two largest islands (> 3 km2) only suffered limited land loss (− 1.19 to − 8.35%) while small islets lost 13.17 to 28.45% of their initial land area. Islands and islets exhibited contrasting responses depending on their location, topography and vegetation type. Depending on islands, the retreat of the vegetation line occurred either along all shorelines, or along ocean shoreline only. The structure (wooded vs. grassy) and origin (native vs. introduced) of the vegetation played a major role in island response. Five days after the cyclone, beach width and beach area were multiplied by 1.5 to 10, depending on the setting, and were interpreted as resulting from both sediment reworking and the supply of large amounts of fresh sediments by the reef outer slopes to the island system. Fourth months after the cyclone, extended sheets of loose sediments were still present on the reef flat and in inter-islet channels and shallow lagoon waters, indicating continuing sediment transfer to islands.