日本地球惑星科学連合2019年大会

講演情報

[J] 口頭発表

セッション記号 A (大気水圏科学) » A-CG 大気海洋・環境科学複合領域・一般

[A-CG37] 北極域の科学

2019年5月30日(木) 10:45 〜 12:15 303 (3F)

コンビーナ:漢那 直也(北海道大学北極域研究センター)、庭野 匡思(気象研究所)、中村 哲(北海道大学大学院地球環境科学研究院)、鄭 峻介(北海道大学 北極域研究センター)、座長:鄭 俊介(北海道大学 北極域研究センター)、庭野 匡思(気象研究所)

11:45 〜 12:00

[ACG37-11] グリーンランド北西部のシオラパルク付近におけるおろし風の出現頻度

*橋本 明弘1山崎 哲秀2青木 輝夫3,1庭野 匡思1山口 悟4 (1.気象研究所、2.アバンナット北極プロジェクト、3.岡山大学 大学院自然科学研究科、4.防災科学技術研究所 雪氷防災研究センター)

キーワード:グリーンランド、おろし風、非静力学モデル

In early April 2018, Niwano et al. (2018) conducted the scientific traverse expedition “Snow impurity and glacial microbe effect on the abrupt warming in the Arctic (SIGMA) Traverse 2018”. The expedition crews had initially planned to depart Siorapaluk on April 2, 2018. However, their departure was delayed by four days because of strong winds and snow blocking the way. Numerical experiment showed that the strong wind had characteristics of a lee-side downslope wind (Hashimoto et al., 2018). Matoba and Yamasaki (2018) reported a sea ice outflow event and its damage to fishery along the coast of Qaanaaq (50-km southeast of Siorapaluk) in early December 2016, which was the first time experience for residents of Qaanaaq over the last 30 years. They assumed that northeasterly winds of more than 30 ms-1on 6-hour average dispersed sea ice from the coast, based on observation data at Qaanaaq airport.

These strong wind events seriously affected the scientific activity and residents’ living, which motivate the authors to study occurrence characteristics of strong winds in the northwest Greenland. According to observation performed during 2016-2017 and 2017-2018 winter seasons in Siorapaluk, strong winds more than 15 ms-1occur in several times. These winds are always from the north-northeast to the observation point, which means that these winds blow beyond the ridgeline in the north of Siorapaluk. Year-round observation in Qaanaaq shows that strong winds appear also in summer as well as in winter. Some strong wind events are found to occur simultaneously in Siorapaluk and Qaanaaq. Numerical simulations are conducted for the period from May 2017 to April 2018 by using the Japan Meteorological Agency’s non-hydrostatic model (JMA-NHM) with the 1-km horizontal resolution to reveal temporal and spatial distributions of strong winds and mechanisms causing them. Statistical features of strong winds and dynamical connections between synoptic and local wind systems will be presented in the meeting.

References
Matoba, S. and T. Yamasaki, 2018: Sea ice outflow damage to fishery in Qaanaaq, northwestern Greenland in December 2016. – Changes of the livelihood associated with social and environmental changes – . Snow and Ice in Hokkaido, 37, 51-54.(in Japanese)
Niwano, M., T. Yamasaki and S. Yamaguchi, 2018: Arctic dog-sled expedition 2018, Seppyo, 80, 588-592. (in Japanese)
Hashimoto, A., M. Niwano, S. Yamaguchi, T. Yamasaki and T. Aoki, 2018: Numerical simulation of lee-side downslope winds near Siorapaluk in northwest Greenland. CAS/JSC WGNE Research Activities in Atmospheric and Oceanic Modelling, 48, 5.05-5.06.

Acknowledgements
This work was partly supported by the Joint Research Program of the Institute of Low Temperature Science, Hokkaido University, Japan, and JSPS KAKENHI Grant Numbers, JP15H01733, JP16H01772, and JP17K12817.