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DSpace at VNU: Synoptic-Dynamic Analysis of Early Dry-Season Rainfall Events in the Vietnamese Central Highlands

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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

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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 Since it is being posted

so soon after acceptance, it has not yet been

copyedited, formatted, or processed by AMS

Publications This preliminary version of the

manuscript may be downloaded, distributed, and

cited, but please be aware that there will be visual

differences and possibly some content differences

between this version and the final published version.

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

AMERICAN

SOCIETY

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Synoptic-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

Manuscript (non-LaTeX) Click here to download Manuscript (non-LaTeX)

MWR-D-15-0265_Revision3.docx

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and N4 in Nguyen et al 2013) Contrary to the Vietnamese Central Highlands where an

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describe a January 2010 case in which the Borneo Vortex moved northwestward and

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lead to rainfall in Vietnam’s most important coffee-growing region In Section 2, data and

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To describe the evolution of deep convection, three-hourly Gridded Satellite

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(case III), and “cold surge with Borneo Vortex” (case IV) The reasons for the naming are

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center located over the Yellow Sea on 09 November 1982 at 1800 UTC (Figure 3a) At this

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As a consequence of the strong surface anticyclogenesis over China, the MSLP

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Highlands southward and in the southern portion of the SCS (Figure 4b), suggesting potential

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show a cyclonic circulation over the Western Pacific on 26 November 1986 that was

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by previous studies (e.g., Roundy 2008; Schreck and Molinari 2011; and Schreck 2015) the

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The high Froude number is one explanation that explains why rainfall reached

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was located exceptionally far west with its center located above the Sea of Okhotsk and the

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scale wave diagnostics were employed to obtain a thorough description of the synoptic

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While case I shows some similarities to the cold surge event of 02–03 November 1999

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Given the data paucity over the Central Highlands and the relatively coarse resolution of

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China Sea Part I: Formation and Propagation of Cold Surge Vortex J Climate, 28,

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Jeong, J.-H., T Ou, H W Linderholm, B.-M Kim, S.-J Kim, J.-S Kug, and D Chen, 2011:

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Liebmann, B., and C A Smith, 1996: Description of a Complete (Interpolated) Outgoing

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Schreck, C J., and J Molinari, 2011: Tropical Cyclogenesis Associated with Kelvin Waves

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based on a Dense Network of Rain Gauges Bull Amer Meteor Soc., 93, 1401–1415,

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Figure 4 Influence of the cold front on Vietnam on 10 November 1982, 0600 UTC (a)

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Figure 8 TD-type disturbance reaching Vietnam on 02 December 1986, 0600 UTC (a)

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wind (colors), 10 m wind (vectors), and SF-CAPE (stippling) (c) Topography (colors),

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flux (vectors), humidity flux convergence (colors) and GridSat brightness temperatures

706

(stippling)

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