JpGU-AGU Joint Meeting 2017

講演情報

[JJ] ポスター発表

セッション記号 A (大気水圏科学) » A-TT 計測技術・研究手法

[A-TT42] [JJ] 飛行艇を用いた臨床地球惑星科学の創成

2017年5月23日(火) 13:45 〜 15:15 ポスター会場 (国際展示場 7ホール)

コンビーナ:角皆 潤(名古屋大学大学院環境学研究科)、植松 光夫(東京大学大気海洋研究所)、谷本 浩志(国立環境研究所)、篠原 宏志(産業技術総合研究所活断層・火山研究部門)

[ATT42-P02] 海洋−大気−陸の観測ネットワークによる強まる北極水循環の実態解明

*朴 昊澤1植村 立2一柳 錦平3 (1.海洋研究開発機構、2.琉球大学、3.熊本大学)

キーワード:北極、海氷減少、同位体、飛行艇

The areal extent and thickness of the Arctic sea ice have significantly decreased during recent decades. The shrunk sea ice cover and reduced sea ice thickness apparently increase heat and moisture fluxes from the ocean to atmosphere mainly in autumn and early winter, which may locally increase air temperature, moisture, and cloud cover, and in turn remotely cause anomalous climate and weather, such as cold and snowy winters, in the subarctic and mid-latitude terrestrial regions. Consequently, there might be related changes in the hydrological regime and its thermal conditions. In fact, the declined sea ice induced snowy winters contributed to increases in summer river discharge, whose relationships had identified by statistical analysis and model simulations. However, there were no yet observations demonstrating the feedback of the declining sea ice to the Arctic hydrologic regimes. Isotope is a useful tool to figure out the questioned realities. We have an observational plan that simultaneously monitors oxygen and hydrogen isotope ratios of water vapor in both ocean by research vessel and land. Although the observations help understanding about the variations of isotopic ratio of the moisture in individual areas, it is limited in tracking the routes that moisture flows to the terrestrial area from the ocean. Therein, observations by flying boat can specify dynamics and transporting routes in the atmosphere of water vapor sourced from the oceanic surface. Dynamics of the moisture in the terrestrial system will be identified by a land surface model coupling an isotope model for water flux. Moreover, the combination of global isotope climatic model with the observational network makes it possible to assess the sea-ice decline induced changes in the Arctic hydrologic system. This research plan is probably the first challenge to explain the amplification of the Arctic hydrologic system under climate changes, based on the observational results.