Zobrazeno 1 - 10
of 235
pro vyhledávání: '"Tsing‐Chang Chen"'
Publikováno v:
International Journal of Climatology. 43:1293-1313
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::926302af91fd4863af85d8f464c8331a
https://doi.org/10.1002/joc.7913
https://doi.org/10.1002/joc.7913
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::24392145ebbd66daf623b6066fb1d47a
https://doi.org/10.1175/mwr-d-17-0059.1
https://doi.org/10.1175/mwr-d-17-0059.1
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3d8c74943406e4b64e64858abc45486c
https://doi.org/10.1175/jcli-d-16-0889.1
https://doi.org/10.1175/jcli-d-16-0889.1
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c9756fd47b870cc70465ce231d0062b
https://doi.org/10.1175/waf-d-16-0189.1
https://doi.org/10.1175/waf-d-16-0189.1
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4dc9af1330991a55804feea54ad36c8
https://doi.org/10.1175/waf-d-16-0148.1
https://doi.org/10.1175/waf-d-16-0148.1
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::84aa73d66c4815f45e58ec979768121c
https://doi.org/10.1175/jcli-d-16-0419.1
https://doi.org/10.1175/jcli-d-16-0419.1
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bc9d1ab875cd235bc226ed97f24fb3a3
https://doi.org/10.1175/waf-d-15-0082.1
https://doi.org/10.1175/waf-d-15-0082.1
Publikováno v:
Journal of Climate. 28:1417-1443
Examination of the development of cold season heavy rainfall/flood (HRF) events around the South China Sea (SCS) from their parent cold surge vortices (CSVs) shows three new development processes. First, the formation mechanism of the parent CSV of a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::df172eac6264652462686a3563f7dc57
https://doi.org/10.1175/jcli-d-14-00170.1
https://doi.org/10.1175/jcli-d-14-00170.1