Monthly Weather Review EARLY ONLINE RELEASE This is a preliminary PDF of the author-produced manuscript that has been peer-reviewed and accepted for publication.. This preliminary vers
Trang 1Monthly Weather Review
EARLY ONLINE RELEASE
This is a preliminary PDF of the author-produced
manuscript that has been peer-reviewed and
accepted for publication Since it is being posted
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The DOI for this manuscript is doi: 10.1175/MWR-D-15-0265.1
The final published version of this manuscript will replace the preliminary version at the above DOI once it is available.
If you would like to cite this EOR in a separate work, please use the following full citation:
van der Linden, R., A Fink, T Phan-Van, and L Trinh-Tuan, 2016: Dynamic Analysis of Early Dry-Season Rainfall Events in the Vietnamese Central Highlands Mon Wea Rev doi:10.1175/MWR-D-15-0265.1, in press
Synoptic-© 2016 American Meteorological Society
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Trang 2Synoptic-Dynamic Analysis of Early Dry-Season Rainfall Events in the
1 Corresponding author address: Roderick van der Linden, Institute for Geophysics and
Meteorology, University of Cologne, Pohligstr 3, 50969 Cologne, Germany
E-mail: rvdlinde@uni-koeln.de
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Trang 5and N4 in Nguyen et al 2013) Contrary to the Vietnamese Central Highlands where an
Trang 6describe a January 2010 case in which the Borneo Vortex moved northwestward and
Trang 7lead to rainfall in Vietnam’s most important coffee-growing region In Section 2, data and
Trang 8To describe the evolution of deep convection, three-hourly Gridded Satellite
Trang 9(case III), and “cold surge with Borneo Vortex” (case IV) The reasons for the naming are
Trang 10center located over the Yellow Sea on 09 November 1982 at 1800 UTC (Figure 3a) At this
Trang 11As a consequence of the strong surface anticyclogenesis over China, the MSLP
Trang 12Highlands southward and in the southern portion of the SCS (Figure 4b), suggesting potential
Trang 13show a cyclonic circulation over the Western Pacific on 26 November 1986 that was
Trang 14by previous studies (e.g., Roundy 2008; Schreck and Molinari 2011; and Schreck 2015) the
Trang 15The high Froude number is one explanation that explains why rainfall reached
Trang 16was located exceptionally far west with its center located above the Sea of Okhotsk and the
Trang 17scale wave diagnostics were employed to obtain a thorough description of the synoptic
Trang 18While case I shows some similarities to the cold surge event of 02–03 November 1999
Trang 19Given the data paucity over the Central Highlands and the relatively coarse resolution of
Trang 22China Sea Part I: Formation and Propagation of Cold Surge Vortex J Climate, 28,
Trang 23Jeong, J.-H., T Ou, H W Linderholm, B.-M Kim, S.-J Kim, J.-S Kug, and D Chen, 2011:
Trang 24Liebmann, B., and C A Smith, 1996: Description of a Complete (Interpolated) Outgoing
Trang 25Schreck, C J., and J Molinari, 2011: Tropical Cyclogenesis Associated with Kelvin Waves
Trang 26based on a Dense Network of Rain Gauges Bull Amer Meteor Soc., 93, 1401–1415,
Trang 29Figure 4 Influence of the cold front on Vietnam on 10 November 1982, 0600 UTC (a)
Trang 30Figure 8 TD-type disturbance reaching Vietnam on 02 December 1986, 0600 UTC (a)
Trang 31wind (colors), 10 m wind (vectors), and SF-CAPE (stippling) (c) Topography (colors),
Trang 35flux (vectors), humidity flux convergence (colors) and GridSat brightness temperatures
706
(stippling)
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