The Heavy Rainfall Mechanism Revealed by a Terrain-Resolving 4DVar Data Assimilation System—A Case Study
Abstract
In this study, a newly developed terrain-resolving four-dimensional variational (4DVar)-based data assimilation system, Immersed Boundary Method_Variational Doppler Radar Analysis System (IBM_VDRAS), is applied to investigate the mechanisms leading to a heavy precipitation event that occurred in Taiwan during the Southwesterly Monsoon Experiment (SoWMEX) conducted in 2008. The multivariate analyses using IBM_VDRAS and surface observations reveal that the warm and moist southwesterly flow from the ocean decelerates after making landfall, forming a surface convergence zone along the coast, which is further strengthened during the passage of a prefrontal rainband. The flow ascends as it advances inland until reaching the mountains, producing persistent precipitation and the enhancement of evaporative cooling as well as a widespread high pressure zone. A very shallow (<0.4 km) layer of offshore flow can be identified over the southwestern plain, which helps to generate a quasi-stationary convergence zone near the coast. Furthermore, sensitivity studies are carried out to quantify the relative importance of the contributions made by topographic blockage, evaporative cooling, and their nonlinear interaction, to the evolution of this type of convective system. The influence of the topography is identified as the dominant factor in modulating the flow structure of the rainfall system. However, it is themore »
- Authors:
-
- Pacific Northwest National Lab. (PNNL), Richland, WA (United States); National Central Univ., Taoyuan (Taiwan)
- National Central Univ., Taoyuan (Taiwan)
- National Center for Atmospheric Research, Boulder, CO (United States)
- Publication Date:
- Research Org.:
- Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
- Sponsoring Org.:
- USDOE; Ministry of Science and Technology of Taiwan; Central Weather Bureau
- OSTI Identifier:
- 1638962
- Report Number(s):
- PNNL-SA-152383
Journal ID: ISSN 0027-0644
- Grant/Contract Number:
- AC05-76RL01830; MOST107-2111-M-008-040; MOST107-2625-M-008-008; MOTC-CWB-107-M-02
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Monthly Weather Review
- Additional Journal Information:
- Journal Volume: 148; Journal Issue: 6; Journal ID: ISSN 0027-0644
- Publisher:
- American Meteorological Society
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; Orographic effects; precipitation; squall lines; radars; radar observations; data assimilation
Citation Formats
Tai, Sheng-Lun, Liou, Yu-Chieng, Chang, Shao-Fan, and Sun, Juanzhen. The Heavy Rainfall Mechanism Revealed by a Terrain-Resolving 4DVar Data Assimilation System—A Case Study. United States: N. p., 2020.
Web. doi:10.1175/mwr-d-19-0244.1.
Tai, Sheng-Lun, Liou, Yu-Chieng, Chang, Shao-Fan, & Sun, Juanzhen. The Heavy Rainfall Mechanism Revealed by a Terrain-Resolving 4DVar Data Assimilation System—A Case Study. United States. https://doi.org/10.1175/mwr-d-19-0244.1
Tai, Sheng-Lun, Liou, Yu-Chieng, Chang, Shao-Fan, and Sun, Juanzhen. Thu .
"The Heavy Rainfall Mechanism Revealed by a Terrain-Resolving 4DVar Data Assimilation System—A Case Study". United States. https://doi.org/10.1175/mwr-d-19-0244.1. https://www.osti.gov/servlets/purl/1638962.
@article{osti_1638962,
title = {The Heavy Rainfall Mechanism Revealed by a Terrain-Resolving 4DVar Data Assimilation System—A Case Study},
author = {Tai, Sheng-Lun and Liou, Yu-Chieng and Chang, Shao-Fan and Sun, Juanzhen},
abstractNote = {In this study, a newly developed terrain-resolving four-dimensional variational (4DVar)-based data assimilation system, Immersed Boundary Method_Variational Doppler Radar Analysis System (IBM_VDRAS), is applied to investigate the mechanisms leading to a heavy precipitation event that occurred in Taiwan during the Southwesterly Monsoon Experiment (SoWMEX) conducted in 2008. The multivariate analyses using IBM_VDRAS and surface observations reveal that the warm and moist southwesterly flow from the ocean decelerates after making landfall, forming a surface convergence zone along the coast, which is further strengthened during the passage of a prefrontal rainband. The flow ascends as it advances inland until reaching the mountains, producing persistent precipitation and the enhancement of evaporative cooling as well as a widespread high pressure zone. A very shallow (<0.4 km) layer of offshore flow can be identified over the southwestern plain, which helps to generate a quasi-stationary convergence zone near the coast. Furthermore, sensitivity studies are carried out to quantify the relative importance of the contributions made by topographic blockage, evaporative cooling, and their nonlinear interaction, to the evolution of this type of convective system. The influence of the topography is identified as the dominant factor in modulating the flow structure of the rainfall system. However, it is the nonlinear interaction between terrain and evaporation that determines the distribution of the temperature and pressure fields.},
doi = {10.1175/mwr-d-19-0244.1},
journal = {Monthly Weather Review},
number = 6,
volume = 148,
place = {United States},
year = {Thu May 07 00:00:00 EDT 2020},
month = {Thu May 07 00:00:00 EDT 2020}
}
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