{"refrec":{"BRefID":230238,"RR":"<b>Kaistrenko, V.; Razjigaeva, N.; Kharlamov, A.; Shishkin, A.</b> (2013). Manifestation of the 2011 great Tohoku tsunami on the coast of the Kuril Islands: a tsunami with ice. <i>Pure Appl. Geophys. 170(6-8)</i>: 1103-1114. <a href=\"https://dx.doi.org/10.1007/s00024-012-0546-9\" target=\"_blank\">https://dx.doi.org/10.1007/s00024-012-0546-9</a>","BEntID":221953,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Pure Appl. Geophys. 170(6-8)</i>: 1103-1114. <a href=\"https://dx.doi.org/10.1007/s00024-012-0546-9\" target=\"_blank\">https://dx.doi.org/10.1007/s00024-012-0546-9</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Kaistrenko, V.; Razjigaeva, N.; Kharlamov, A.; Shishkin, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Kaistrenko, V. <i>et al.</i>","Englishabstract":"The tsunami generated by the 2011 Tohoku Earthquake (<em class=\"a-plus-plus\">M</em> <sub class=\"a-plus-plus\">w</sub> = 9.0) reached maximum heights of about 5 m along the coast of the Kuril Islands. The most essential feature of this event was sea ice about 0.5 m thick moved by the ocean water. The tsunami did not cause any essential damage on the Kuril Islands, but significantly affected coastal zones and produced interesting effects. 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