Hung, C.-w. and H.-H. Hsu, 2008: The First
Transition of the Asian Summer Monsoon, Intraseasonal Oscillation, and Taiwan Meiyu. J. Climate. 21, 1552–1568. (SCI)
之後呢,我們陸續又把臺灣不同季節跟MJO的相關給釐清,有關冬半年的部分,在這篇文章有詳細說明: Hung, C.-w., H.-J.
Lin and H.-H. Hsu, 2014: Madden–Julian Oscillation and the Winter Rainfall in
Taiwan. J. Climate. 27, 4521-4530. DOI: 10.1175/JCLI-D-13-00435.1
(SCI)
最後,則是台灣夏季降雨,西北太平洋颱風跟MJO,喔不,要改用BISIO的指數來看,一樣有關,也就是這次得獎得論文: Hung C.-w. ,H.-J. Lin,
P.-k. Kao, M.-f. Shih, W.-y. Fong, 2016:Impact of the Boreal Summer
Intraseasonal Oscillation on the Western North Pacific Typhoons and Rainfall in
Taiwan Terr.
Atmos. Ocean. Sci.
(SCI)
This study
discusses the boreal summer intraseasonal oscillation (BSISO) impact on the
western North Pacific (WNP) typhoons and the summer rainfall in Taiwan. The
real time BSISO1 and BISISO2 indices are created using the first two and the
third and fourth principal components of the multivariate empirical orthogonal
function analysis, based on outgoing long-wave radiation and zonal wind at 850
hPa from Lee et al. (2013). The results show that heavy rainfall in Taiwan and
the associated WNP typhoon frequency patterns are closely related to the 10 -
30 days BSISO2 phases during the typhoon season (July - October). Taiwan has
larger rainfall during BSISO2 phases 3, 4, and 5 when the major BSISO2
convection moves northwestward from the Philippine Sea to the Taiwan area.
During phases 3 and 4 the anomalous low-level cyclonic flow and the increased
typhoon frequency directly result in larger rainfall in Taiwan. Phase 5
exhibits enhanced low-level southwesterly flow which transports the moisture to
Taiwan responsible for more summer rainfall on the island.
其實今天的年會,還有頒發周佳學術論文獎,年度論文是我跟許晃雄老師指導的高培根博士獲得,而周佳這位我在UCLA非常照顧我的學長的愛徒陳昭安也得到研究新秀獎。我想,今天周佳一定也很替這些他的後輩們高興吧~ 就讓我們Rich get richer吧!