By Jai Ho Oh
This priceless quantity set of Advances in Geosciences maintains the superb culture of the Asia-Oceania medical group in supplying the main up to date examine effects on quite a lot of geosciences and environmental technological know-how. the data is key to the knowledge of the results of weather switch, severe weathers at the so much populated areas and quickest relocating economies on the planet. along with, those volumes additionally spotlight unique papers from many prestigious learn associations that are doing innovative research in atmospheric physics, hydrological technology and water source, ocean technological know-how and coastal learn, planetary exploration and sun procedure technology, seismology, tsunamis, top atmospheric physics and area technological know-how.
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Additional resources for Atmospheric Science (Advances in Geosciences)
1962]. The authors made similar discovery but in diﬀerent regions that extreme precipitation events occurred less/more frequently a few days before/after a full moon (Bowen’s signal). Adderley and Bowen  suggested that the Moon perhaps modulates the amount of meteor dust collected by the Earth. Lethbridge  further indicated that the disturbance of magnetosphere could be the reason. By focusing on the spatial progression over the United States in the phase of lunar-precipitation relationship, Hanson et al.
Associated with the SPA characteristics, Chen and Chen  indicated that the northeasterly monsoon ﬂow over Taiwan generally reaches the maximum intensity in winter. 5◦N, 121◦ E) in early January. In late January, the west Paciﬁc subtropical high axis at the 850 hPa level extends westward and weakens the SPA. In the upper levels, the westerly jet axis reaches its southernmost position in January when the monsoon cold surges are most frequent [Yeh and Chen, 1984]. 53-day period is exactly at ∼63◦ heliocentric latitude.
M. Lau, Biennial oscillation associated with the East Asian monsoon and tropical sea surface temperatures, J. Meteorol. Soc. Japan 73 (1995) 105–124. Changma and Shifting Peak in Summer Rainfall of Korea 45 12. Y. Wang, B. Wang and J. H. Oh, Impact of the preceding El Ni˜ no on the East Asian summer atmosphere circulation, J. Meteorol. Soc. Jap. 79 (2001) 575–588. 13. B. Wang, R. Wu and X. Fu, Paciﬁc-East Asian teleconnection: How does ENSO aﬀect East Asian climate? J. Climate 13 (2000) 1517–1536.