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pro vyhledávání: '"Jenq-Dar Tsay"'
Autor:
Jenq-Dar Tsay, 蔡政達
87
In this investigation, FT-IR and 13C-NMR spectroscopy were used to study the synthesis of barium titanate powder by the citrate process. The experimental parameter of initial barium titanium citric solution, the properties and thermal decompo
In this investigation, FT-IR and 13C-NMR spectroscopy were used to study the synthesis of barium titanate powder by the citrate process. The experimental parameter of initial barium titanium citric solution, the properties and thermal decompo
Externí odkaz:
http://ndltd.ncl.edu.tw/handle/44439624696855944422
Publikováno v:
International Journal of Climatology. 43:1293-1313
Publikováno v:
Monthly Weather Review. Dec2017, Vol. 145 Issue 12, p4949-4976. 28p.
Publikováno v:
Journal of Climate. Jan2017, Vol. 30 Issue 2, p669-688. 20p. 6 Charts, 10 Graphs, 3 Maps.
Publikováno v:
Monthly Weather Review. 145:4949-4976
During May and June, the monsoon rainfall in northern Southeast Asia is primarily produced by rainstorms. At the mature stage, these storms, coupled with a midtropospheric subsynoptic-scale trough, produce rainfall ≥50 mm (6 h)−1and exhibit a cyc
Publikováno v:
Journal of Climate. 30:7909-7931
A northwest–southeast-oriented summer monsoon trough exists between northern Indochina and northwestern Borneo. Ahead of this the South China Sea (SCS) trough is located at a convergent center west of the Philippines, which provides an environment
Publikováno v:
Weather and Forecasting. 32:925-947
After the onset of the Southeast Asian summer monsoon in mid-May, the South China Sea (SCS) trough is deepened by the intensified monsoon westerlies to facilitate the development of a synoptic cyclonic shear flow. This shear flow forms an environment
Publikováno v:
Weather and Forecasting. 32:797-819
The peak intensity occurrence frequency over the life cycles of parent cold-surge vortices (CSVs) for heavy rainfall/flood (HRF) events is classified into two types depending on their life cycles having two or three peak intensities, denoted as HRF2
Publikováno v:
Journal of Climate. 30:669-688
During 15 November–31 December, a cold-season rainfall center appears in the southern part of the South China Sea (SCS) north of northwestern Borneo and juxtaposed along the southwest–northeast direction with rainfall centers for the Malay Penins
Publikováno v:
Weather and Forecasting. 31:531-552
Summer is a dry season in northern Taiwan. By contrast, the Taipei basin, located in this region, has its maximum rainfall during summer (15 June–31 August), when 78% of this rainfall is contributed by afternoon thunderstorms. This thunderstorm act