The 20th July 2017 Bodrum–Kos Tsunami Field Survey

被引：0
作者：
Gozde Guney Dogan
Alessandro Annunziato
Gerassimos A. Papadopoulos
Hasan Gokhan Guler
Ahmet Cevdet Yalciner
Tarık Eray Cakir
Ceren Ozer Sozdinler
Ergin Ulutas
Taro Arikawa
Mehmet Lutfi Suzen
Isikhan Guler
Pamela Probst
Utku Kânoğlu
Costas Synolakis
机构：
[1] Middle East Technical University,Ocean Engineering Research Center, Department of Civil Engineering
[2] European Commission,Joint Research Centre
[3] National Observatory of Athens,Institute of Geodynamics
[4] Turkish Chamber of Civil Engineers,Department of Geophysics, Kandilli Observatory and Earthquake Research Institute
[5] Bogazici University,Institute of Education, Research and Regional Cooperation for Crisis Management Shikoku
[6] Kagawa University,Department of Geophysical Engineering
[7] Kocaeli University,Department of Civil and Environmental Engineering
[8] Chuo University,Department of Geological Engineering
[9] Middle East Technical University,Department of Aerospace Engineering
[10] Middle East Technical University,undefined
[11] USC,undefined
[12] Technical University of Crete,undefined
来源：
Pure and Applied Geophysics | 2019年 / 176卷
关键词：
Bodrum; Kos; earthquake; tsunami; post-tsunami field survey; tsunami effects; tsunami runup;
D O I：
暂无
中图分类号：
学科分类号：
摘要：
The July 20, 2017 Bodrum–Kos Earthquake caused tsunami wave motions and damage in the south of Bodrum Peninsula, Turkey, and on Kos Island, Greece. Immediately after the earthquake, we conducted several post-tsunami field surveys including interviews in coastal zones impacted by the tsunami, i.e., the coastlines of Bodrum Peninsula, Karaada Islet and Akyaka Town in Gökova Bay, Turkey, and eastern Kos Island, Greece. We present observations and measurements to document the variation of the tsunami effects along the coast. The largest tsunami runup was about 1.9 m and observed at the mouth of a small dry streambed at Gumbet Bay, Bodrum. No significant water motions were reported at the northern and western coasts of Bodrum Peninsula. The tsunami runup distribution along the coast of eastern Kos was overall regular, with runup not exceeding 1 m except in the Port of Kos where a 1.5 m tsunami runup was measured.
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页码：2925 / 2949
页数：24
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