地理科学 ›› 2017, Vol. 37 ›› Issue (8): 1243-1250.doi: 10.13249/j.cnki.sgs.2017.08.015
杨林1(), 董玉祥1,2(
), 黄德全1, 张雪琴1, 杜建会1
收稿日期:
2016-09-08
修回日期:
2016-11-30
出版日期:
2017-08-15
发布日期:
2017-08-15
作者简介:
作者简介:杨林(1987-),男,江西赣州人,博士研究生,主要从事海岸风沙地貌研究。E-mail:
基金资助:
Lin Yang1(), Yuxiang Dong1,2(
), Dequan Huang1, Xueqin Zhang1, Jianhui Du1
Received:
2016-09-08
Revised:
2016-11-30
Online:
2017-08-15
Published:
2017-08-15
Supported by:
摘要:
依据2014年第10号强台风“麦德姆”登陆前后福建平潭岛典型海岸沙席的形态观测与近表层沉积物粒度数据,综合分析了海岸沙席对台风的响应特征。结果表明:① 海岸沙席形态对“麦德姆”的响应明显,主要表现为沙席前缘高程降低(最大侵蚀深度为0.40 m),中部变化较小(-0.06~0.09 m),后缘明显升高(最大堆积厚度为1.62 m),沙席体积增大2.02%。② 海岸沙席近表层沉积物粒度受“麦德姆”影响较小,其粒度参数在台风前后并无质的等级性变化。③ 海岸沙席的台风响应特征主要因台风过程中大风的非选择性侵蚀和搬运及海岸沙席与海滩沙粒度的相近性所造成的,同时也受到周边地势及植被等的影响。
中图分类号:
杨林, 董玉祥, 黄德全, 张雪琴, 杜建会. 海岸沙席形态及近表层沉积物粒度对台风的响应[J]. 地理科学, 2017, 37(8): 1243-1250.
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