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Hydrological Consequences of Typhoon Hinnamnor in Primorsky Krai in September 2022
by
Shkolnaya, D. K.
, Semakov, V. A.
, Shkolnyi, D. I.
, Bakhareva, E. I.
, Yatsumira, D. A.
in
Atmospheric Sciences
/ Cell migration
/ Channels
/ Creeks & streams
/ Cyclones
/ Debris flow
/ Earth and Environmental Science
/ Earth Sciences
/ Floodplains
/ Floods
/ Hurricanes
/ Hydrology
/ Meteorology
/ Mudflows
/ Precipitation
/ River channels
/ Rivers
/ Sediment transport
/ Spatial distribution
/ Storm damage
/ Storms
/ Typhoons
/ Valleys
/ Water levels
2024
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Hydrological Consequences of Typhoon Hinnamnor in Primorsky Krai in September 2022
by
Shkolnaya, D. K.
, Semakov, V. A.
, Shkolnyi, D. I.
, Bakhareva, E. I.
, Yatsumira, D. A.
in
Atmospheric Sciences
/ Cell migration
/ Channels
/ Creeks & streams
/ Cyclones
/ Debris flow
/ Earth and Environmental Science
/ Earth Sciences
/ Floodplains
/ Floods
/ Hurricanes
/ Hydrology
/ Meteorology
/ Mudflows
/ Precipitation
/ River channels
/ Rivers
/ Sediment transport
/ Spatial distribution
/ Storm damage
/ Storms
/ Typhoons
/ Valleys
/ Water levels
2024
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Hydrological Consequences of Typhoon Hinnamnor in Primorsky Krai in September 2022
by
Shkolnaya, D. K.
, Semakov, V. A.
, Shkolnyi, D. I.
, Bakhareva, E. I.
, Yatsumira, D. A.
in
Atmospheric Sciences
/ Cell migration
/ Channels
/ Creeks & streams
/ Cyclones
/ Debris flow
/ Earth and Environmental Science
/ Earth Sciences
/ Floodplains
/ Floods
/ Hurricanes
/ Hydrology
/ Meteorology
/ Mudflows
/ Precipitation
/ River channels
/ Rivers
/ Sediment transport
/ Spatial distribution
/ Storm damage
/ Storms
/ Typhoons
/ Valleys
/ Water levels
2024
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Hydrological Consequences of Typhoon Hinnamnor in Primorsky Krai in September 2022
Journal Article
Hydrological Consequences of Typhoon Hinnamnor in Primorsky Krai in September 2022
2024
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Overview
The features of precipitation and its spatial distribution over the territory of the Primorsky krai during the passage of Typhoon Hinnamnor (September 4–7, 2022), as well as the characteristics of the flood caused by the typhoon, are studied based on ground observational data and the ERA5-Land reanalysis. A list of the settlements affected by the flood and an assessment of the impact of the disaster on transport infrastructure are given. The relationship between the precipitation maxima and the movement of storm cells is shown. Deformations were recorded for 30% of the length of the Primorsky krai river channels as a result of the typhoon passage. The relationship among the changes in the channels, spatial characteristics of precipitation (including their intensity) and the slope of the catchment were determined. Areas of extreme channel deformations (including mudflows) and their magnitudes on rivers of different scales are described.
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