RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES4004, doi:10.2205/2017ES000608, 2017
Points | Surge height, m | Total surge numbers | Contribution of surge height to the total sea level, % | |||
$\leq 54$% | 55–74 | 75–99 | $\geq 100$ % | |||
White Sea | ||||||
Solovki | $\leq 0.3$ | 196 | 26 (13) | 40 (20) | 28 (14) | 102 (53) |
Onega Bay | $\leq 0.5 $ | 171 | 41 (24) | 71 (42) | 3 (1) | 56 (33) |
Severodvinsk | $\leq 0.5 $ | 107 | 3 (3) | 39 (36) | 38 (36) | 27 (25) |
Barents Sea | ||||||
Pechora Bay | $\leq 0.7 $ | 103 | 22 (21) | 45 (44) | 36 (35) | |
Chyosha Bay | $\leq 0.8 $ | 117 | 41 (35) | 9 (8) | 6 (5) | 61 (52) |
Varandey | $\leq 1.0 $ | 76 | 15 (20) | 26 (34) | 35 (46) | |
Khaypudyr Bay | $\leq 1.0 $ | 207 | 53 (25) | 78 (38) | 76 (37) |
Citation: Korablina A. D., A. T. Kondrin, V. S. Arkhipkin (2017), Numerical simulations and statistics of surges in the White and Barents seas, Russ. J. Earth Sci., 17, ES4004, doi:10.2205/2017ES000608.
Copyright 2017 by the Geophysical Center RAS.