Summary: https://ppt.cc/fvEW4x

摘要：https://ppt.cc/fvEW4x

https://meet.google.com/npt-vwnn-bfb

臺大大氣系將於 2 月 23 日（週五）12：30 - 13：45，於大氣系 B105 教室舉辦 2024 年「大學生暑期研究計畫」說明會。

當天將邀請系上老師介紹他的研究主題，歡迎大學部同學們踴躍參加，或透過同步直播參與

直播連結： https://www.youtube.com/playlist?list=PLKC_WAwt1IlIvTsoEXx9-p4AmlSuCUlyC

後續的報名訊息及相關時程，將盡快公布於大氣系網頁

若有相關問題，可寫信至 Email住址會使用灌水程式保護機制。你需要啟動Javascript才能觀看它 詢問

https://meet.google.com/npt-vwnn-bfb 

https://meet.google.com/npt-vwnn-bfb 

https://meet.google.com/npt-vwnn-bfb 

https://meet.google.com/npt-vwnn-bfb 

 Y.-T. Hwang, S.-P. Xie, P.-J. Chen, H.-Y. Tseng, C. Deser, Contribution of anthropogenic aerosols to persistent La Niña-like conditions in the early 21st century. Proc. Natl. Acad. Sci. U.S.A.121, e2315124121 (2024). https://www.pnas.org/doi/full/10.1073/pnas.2315124121

• Figure 6. A schematic illustrating the distinct characteristics of and the interplay between the fast component of aerosol emission reduction and the slow component of aerosol emission increase. Shadings represent anomalous oceanic potential temperature. Arrows in the two vertical planes are the anomalous cross-equatorial Hadley Cell and the anomalous oceanic STC. The thick arrows in the Top panel A illustrates intensified trades and the thin blue arrows illustrate the associated air-sea fluxes. The thick arrows in the Bottom panel B illustrate how the intensified STC induces cold water, which converges in west Pacific subtropics and upwells in the east.