Japan Geoscience Union Meeting 2022

Presentation information

[E] Poster

A (Atmospheric and Hydrospheric Sciences ) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS01] Extreme weathers and disasters in urban environments in East Asia, related to climate change

Sun. May 29, 2022 11:00 AM - 1:00 PM Online Poster Zoom Room (6) (Ch.06)

convener:Masaru Inatsu(Faculty of Science, Hokkaido University), convener:Yukari Takayabu(Atmosphere and Ocean Research Institute, the University of Tokyo), Chairperson:Masaru Inatsu(Faculty of Science, Hokkaido University)

11:00 AM - 1:00 PM

[AAS01-P02] Trends and projection of heavy snowfall in Hokkaido, Japan, as an application of self-organizing map

*Masaru Inatsu1, Sho Kawazoe1, Masato Mori2 (1.Faculty of Science, Hokkaido University, 2.Research Institute for Applied Mechanics, Kyushu University)

Keywords:snowfall, weather pattern, SOM

This paper showed the frequency of local-scale heavy winter snowfall in Hokkaido, Japan, its historical change, and its response to global warming using self-organizing maps (SOM) of synoptic-scale sea level pressure anomaly. Heavy snowfall days were here defined as days on which the snowfall exceeded 10mmin water equivalent. It was shown that the SOMs can be grouped into three categories for heavy snowfall days: 1) a passage of extratropical cyclones to the south of Hokkaido, 2) a pressure pattern between the Siberian high and the Aleutian low, and 3) a low pressure anomaly just to the east of Hokkaido. Groups 1 and 2 were associated with heavy snowfall in Hiroo (located in southeastern Hokkaido) and in Iwamizawa (western Hokkaido), respectively, and heavy snowfall in Sapporo (western Hokkaido) was related to group 3. The large-ensemble historical simulation reproduced the observed increasing trend in group 2, and future projections revealed that group 2 was related to a negative phase of the western Pacific pattern and that the frequency of this group would increase in the future. Heavy snowfall days associated with SOM group 2 would also increase as a result of the increase in water vapor and preferable weather patterns in a globally warming climate, in contrast to the decrease of heavy snowfall days at other sites associated with SOM group 1.