日本地球惑星科学連合2024年大会

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[J] 口頭発表

セッション記号 A (大気水圏科学) » A-OS 海洋科学・海洋環境

[A-OS15] 海洋化学・生物学

2024年5月26日(日) 15:30 〜 16:45 101 (幕張メッセ国際会議場)

コンビーナ:安中 さやか(東北大学)、渡部 裕美(海洋研究開発機構)、座長:安中 さやか(東北大学)、渡部 裕美(海洋研究開発機構)

16:15 〜 16:30

[AOS15-04] Is the high droplet number density of late spring Arctic water clouds an indication of snow/ice algae – cloud – Arctic melting feedback?

*yongxiang hu1 (1.NASA Langley Research Center)

キーワード:Arctic ice algal bloom, cloud microphysics, feedback, lidar measurements, CALIPSO

Water cloud droplet number density, Nd, together with other cloud microphysical properties such as liquid water content, can be accurately estimated from CALIPSO measurements (Hu et al., 2021, https://www.frontiersin.org/articles/10.3389/frsen.2021.724615/full ) from 2006 to 2023.

One interesting findings from the new droplet number density statistics is the huge Nd values of boundary layer clouds in the springtime Arctic. Comparing Nd with chlorophyll biomass of snow/ice algae calculated from high resolution Arctic models, we found excellent spatial/temporal correlations between the two. I will introduce the lidar measurements of water cloud microphysical properties, the spatial and temporal correlation between the cloud properties and ice algal biomass, and a hypothesis of a positive feedback mechanism of springtime Arctic snow/ice algae, biological aerosols and Arctic clouds.

I will also introduce the ongoing ICESAT-2 data analysis of snow properties (Hu et al., 2022, https://www.frontiersin.org/articles/10.3389/frsen.2022.855159/abstract ) and the sea-ice cover that may help evaluate the atmosphere, snow/ice and springtime ice algal bloom feedback mechanisms.