Reccurence of strong floods on western sakhalin and intensity of cyclogenesis in middle-late holocene

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The geological record of extreme floods associated with the passage of strongest typhoons and deep extratropical cyclones over the past 6370 years has been restored in Western Sakhalin (the Yablochnaya River basin). A section of peat bog with numerous layers of loam formed during extreme floods was used for the reconstructions. A recent analogue of such events is Typhoon Phyllis (1981), total rainfall reached 300 mm. Ash content was tested for identification of mineral component that was input to the peat during floods. According to the “age-depth” model, we has determined the ages of 38 extreme floods and periods of weaker floods when organomineral sediments accumulated. During periods of active cyclogenesis, the frequency of extreme floods was once every 10—30 years. The paleoclimatic background of events has been analyzed. Long periods with extreme floods were identified 6470—5490, 4300—3670 years ago, and the last 3110 years ago severe floods were rare events. We compare the records of strong floods that occurred on the western and eastern coast of South Sakhalin and in other regions of East Asia. It has been established that periods with frequent strong paleotyphoons and deep extratropical cyclones do not always coincide in time, which could be due to different trajectories of cyclones under different climatic situations. As in the modern period, the increase in the intensity of cyclogenesis and the frequency of typhoons in the Middle-Late Holocene was closely related to warm pool in the western tropical zone of the Pacific Ocean, anomalies of El Niño and atmospheric centers of action.

Sobre autores

N. Razjigaeva

Pacific Geographical Institute FEB RAS

Autor responsável pela correspondência
Email: nadyar@tigdvo.ru
Rússia, Vladivostok

L. Ganzey

Pacific Geographical Institute FEB RAS

Email: nadyar@tigdvo.ru
Rússia, Vladivostok

T. Grebennikova

Pacific Geographical Institute FEB RAS

Email: nadyar@tigdvo.ru
Rússia, Vladivostok

V. Ponomarev

Institute of Marine Geology and Geophysics FEB RAS

Email: nadyar@tigdvo.ru
Rússia, Yuzhno-Sakhalinsk

V. Afanasiev

Institute of Marine Geology and Geophysics FEB RAS

Email: nadyar@tigdvo.ru
Rússia, Yuzhno-Sakhalinsk

A. Gorbunov

Institute of Marine Geology and Geophysics FEB RAS

Email: nadyar@tigdvo.ru
Rússia, Yuzhno-Sakhalinsk

M. Kliminc

Institute of Water and Ecological Problems FEB RAS

Email: nadyar@tigdvo.ru
Rússia, Khabarovsk

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2. Fig. 1. Study area. (a) — position of Sakhalin Island; (б) — Southern Sakhalin with position if study area and section with flood traces on eastern coast of the island; (в) — Yablochnaya River valley and position of studied section of peatbog № 322 with loam layers, deposited during strong floods. 1 — studied sections.

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3. Fig. 2. Section of the peatbog in Yablochnaya River valley. 1 — peat; 2 — organic-mineral sediments; 3 — loam; 4 — soil; 5 — wood.

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4. Fig. 3. Age-depth model with ages of strong floods (grey bars). ¹⁴C dates with standard deviations are shown in blue, the gray curve shows the 95 % confidence interval.

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5. Fig. 4. Recurrence of supertyphoons and deep cyclones, associated with strong floods in western coast of South Sakhalin in Middle-Late Holocene (a) and thickness of loam layers, deposited by different-age floods (б).

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6. Fig. 5. Reconstruction of the periods with strong floods compared with paleoclimatic data for Southern Sakhalin and paleogeographical records for Western Pacific. (а) — paleoclimatic data for Southern Sakhalin (Mikishin, Gvozdeva, 2017, 2019; Mikishin et al., 2021); (б) — ash content of the peat in the section in Yablochnaya River valley (A) and Naiba River basin (Б); (в) — periods of different intensity floods (western coast, Yablochnaya River basin); (г) — periods of strong floods (eastern coast, Naiba River basin); (д) — LOI of the peatbogs within Ishikari River basin, Western Hokkaido and period with strong floods, A, Б — section located near the river channel, В — section located further from the river channel (Ishii et al., 2017); (е) — periods of extreme floods on south of the Honshu Island (Suzuki et al., 2021); (ж) — periods of high storm activity, Kamikoshiki Island, South Japan (Woodruff et al., 2009); (з) — frequency (per 100 years) of El Niño events (Moy et al., 2002); (и) — sea surface temperature (SST) records, Okinawa Trough regions, °C (Sun et al., 2005); (к) — SST records in the western tropical zone of the Pacific Ocean, °C (Stott et al., 2002; Park et al., 2021).

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