日本地球惑星科学連合2014年大会

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セッション記号 P (宇宙惑星科学) » P-EM 太陽地球系科学・宇宙電磁気学・宇宙環境

[P-EM09_29AM2] VarSITI - Variability of the Sun and Its Terrestrial Impact

2014年4月29日(火) 11:00 〜 12:45 501 (5F)

コンビーナ:*塩川 和夫(名古屋大学太陽地球環境研究所)、坂尾 太郎(独立行政法人宇宙航空研究開発機構 宇宙科学研究所 太陽系科学研究系)、廣岡 俊彦(九州大学大学院理学研究院地球惑星科学部門)、座長:江尻 省(国立極地研究所)、鈴木 臣(名古屋大学太陽地球環境研究所)

12:30 〜 12:45

[PEM09-35] 太陽活動の変動に伴うグリーンランド気温の変化

*小端 拓郎1川村 賢二1東 久美子1 (1.国立極地研究所)

キーワード:太陽活動, グリーンランド, 気温, 氷床コア, 気候変動

During the past decades, Greenland climate has undergone rapid warming and ice sheet ablation in coastal region with a nearly 1 mm/y sea level contribution. For sea level projection, it is critical to understand the mechanisms of Greenland temperature variability. Greenland temperature is known to be affected by the North Atlantic Oscillation (NAO), and it is also highly correlated with North Atlantic average temperature. Using the Greenland temperature reconstructed from argon and nitrogen isotopes in occluded air in GISP2 ice core (Kobashi et al., 2011), we found Greenland temperature deviated negatively (positively) from North Hemispheric (NH) temperature trend during stronger (weaker) solar activity over the past 800 years (Kobashi et al., 2013b). We also confirmed this effects continued over the past 4000 years (Kobashi et al., 2013a). Climate modeling suggests that the deviation was caused by solar induced atmospheric circulation changes (like NAO). The model also suggests that Atlantic meridional circulation weakens during the stronger sun by similar processes as enhanced greenhouse effect (Kobashi et al., 2013b). From the past relation between Greenland temperature anomaly and solar variability, it can be speculated that future gland solar minimum may induce additional 2 ⁰C warming in Greenland with increased melting of the ice-sheet. Kobashi, T., Kawamura, K., Severinghaus, J. P., Barnola, J.-M., Nakaegawa, T., Vinther, B. M., Johnsen, S. J., and Box, J. E.: High variability of Greenland surface temperature over the past 4000 years estimated from trapped air in an ice core, Geophysical Research Letters, 38, 10.1029/2011GL049444, 2011.Kobashi, T., Goto-Azuma, K., Box, J. E., Gao, C.-C., and Nakaegawa, T.: Causes of Greenland temperature variability over the past 4000 years: Implications for Northern Hemispheric temperature change Climate of the Past, 9, 2299-2317, 2013a.Kobashi, T., Shindell, D. T., Kodera, K., Box, J. E., Nakaegawa, T., and Kawamura, K.: On the origin of Greenland temperature anomalies over the past 800 years, Climate of the Past, 9, 583-596, 2013b.