JpGU-AGU Joint Meeting 2020

講演情報

[J] 口頭発表

セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS24] 山の科学

コンビーナ:鈴木 啓助(信州大学山の環境研究センター)、苅谷 愛彦(専修大学文学部環境地理学科)、佐々木 明彦(国士舘大学文学部史学地理学科 地理・環境コース)、奈良間 千之(新潟大学理学部理学科)

[MIS24-12] Long-term Measurements of Atmospheric Aerosol, Cloud and Snow at Mt. Tateyama

★Invited Papers

*青木 一真1島田 亙1 (1.富山大学)

キーワード:山の科学、立山、エアロゾル、雲、雪、地球環境

The aerosol, cloud and snow play an important role in the earth environment at high mountain region (Aoki and Watanabe, 2009). Especially, it is important in the free troposphere, that the aerosol particles are very low. However, our mountain observation sites has shown that large quantities of anthropogenic aerosols, Asian dust, and Siberia forest fire from the Asian continent are transported through the source region to the Mt.Tateyama region. We were studied at the Mt.Tateyama areas, Tateyama Research Laboratory (University of Toyama Mountain observatory) located on top of the Mt.Jodo, Toyama, Japan (36.57°N, 137.61°E, 2839 m asl.) and at the Murododaira, Toyama, Japan (36.58°N, 137.60°E, 2450 m asl.). Mt. Tateyama, the Northern Japan Alps, is located in southeastern Toyama Prefecture, near the Toyama bay on the coast of Sea of Japan. Horizontal distance is about 30 km from Mountain to Sea. We conducted the measurements of weather, remote sensing of aerosol and cloud, the analysis of snow layer sampled and so on. Furthermore, we measured weather and the aerosol optical properties by using sky radiometer in the city of Toyama (Aoki et al., 2013), our University on the top of roof (36.70°N, 137.19°E, 30 m asl.). We started the long-term monitoring of snow layer from Murododaira since 1970’s every mid of April (This season is the maximum snow depth, about six or seven meter every year). The plied snow layers exhibit the chronology of transport and deposition of atmosphere during autumn to spring. It was found that the physical and chemical properties of snow (e.g. Aoki and Watanabe, 2009, Mochizuki et al., 2016, Hayakawa et al., 2019), bio-aerosols (e.g. Maki et al., 2018) and simulation of snow amounts (Kawase et al., 2018). Furthermore, we measured the aerosol optical properties by using sky radiometer at Mt.Jodo and University of Toyama (vertical distance is about 3000 m.). The aerosol optical properties have a significant vertical characteristic. We provide the information, in the presentation, on the mountain science with respect to their temporal and spatial variability of aerosol, cloud and snow on the Mt.Tateyama areas.