Convective Cold Pool Associated with Offshore Propagation of Convection System over the East Coast of Southern Sumatra, Indonesia

The cold pool outflow has been previously shown to be generated by decaying Mesoscale Convective Complexes (MCCs) in the Maritime Continent. The cold pool also has a main role in the development processes of oceanic convective systems inducing heavy rainfall. This study investigated a cold pool even...

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Main Authors: Erma Yulihastin, Ibnu Fathrio, Trismidianto, Fadli Nauval, Elfira Saufina, Wendi Harjupa, Didi Satiadi, Danang Eko Nuryanto
Format: Article
Language:English
Published: Wiley 2021-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2021/2047609
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author Erma Yulihastin
Ibnu Fathrio
Trismidianto
Fadli Nauval
Elfira Saufina
Wendi Harjupa
Didi Satiadi
Danang Eko Nuryanto
author_facet Erma Yulihastin
Ibnu Fathrio
Trismidianto
Fadli Nauval
Elfira Saufina
Wendi Harjupa
Didi Satiadi
Danang Eko Nuryanto
author_sort Erma Yulihastin
collection DOAJ
description The cold pool outflow has been previously shown to be generated by decaying Mesoscale Convective Complexes (MCCs) in the Maritime Continent. The cold pool also has a main role in the development processes of oceanic convective systems inducing heavy rainfall. This study investigated a cold pool event (January 1-2, 2021) related to a heavy rainfall system over the coastal region of Lampung, Southern Sumatra, within a high-resolution model simulation using a regional numerical weather prediction of the Weather Research and Forecasting (WRF) with convection permitting of 1 km spatial resolution, which was validated by satellite and radar data observations. It is important to note that the intensity, duration, timing, and structure of heavy rainfall simulated were in good agreement with satellite-observed rainfall. The results also showed that a cold pool (CP) plays an important role in inducing Mesoscale Convective Complex (MCC) and was responsible for the development of an offshore propagation of land-based convective systems due to the late afternoon rainfall over inland. This study also suggests that the propagation speed of the CP 8.8 m·s−1 occurring over the seaside of the coastal region, the so-called CP-coastal, is a plausible mechanism for the speed of the offshore-propagating convection, which is dependent on both the background prevailing wind and outflow. These conditions help to maintain the near-surface low temperatures and inhibit cold pool dissipation, which has implications for the development of consecutive convection.
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institution Kabale University
issn 1687-9309
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language English
publishDate 2021-01-01
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spelling doaj-art-add91b8a43404aa19450d9700d2ea68a2025-02-03T01:25:15ZengWileyAdvances in Meteorology1687-93091687-93172021-01-01202110.1155/2021/20476092047609Convective Cold Pool Associated with Offshore Propagation of Convection System over the East Coast of Southern Sumatra, IndonesiaErma Yulihastin0Ibnu Fathrio1Trismidianto2Fadli Nauval3Elfira Saufina4Wendi Harjupa5Didi Satiadi6Danang Eko Nuryanto7Research Center of Atmospheric Science and Technology, Research Organization of Aeronautics and Space, National Research and Innovation Agency, Bandung, West Java 40173, IndonesiaResearch Center of Atmospheric Science and Technology, Research Organization of Aeronautics and Space, National Research and Innovation Agency, Bandung, West Java 40173, IndonesiaResearch Center of Atmospheric Science and Technology, Research Organization of Aeronautics and Space, National Research and Innovation Agency, Bandung, West Java 40173, IndonesiaResearch Center of Atmospheric Science and Technology, Research Organization of Aeronautics and Space, National Research and Innovation Agency, Bandung, West Java 40173, IndonesiaResearch Center of Atmospheric Science and Technology, Research Organization of Aeronautics and Space, National Research and Innovation Agency, Bandung, West Java 40173, IndonesiaResearch Center of Atmospheric Science and Technology, Research Organization of Aeronautics and Space, National Research and Innovation Agency, Bandung, West Java 40173, IndonesiaResearch Center of Atmospheric Science and Technology, Research Organization of Aeronautics and Space, National Research and Innovation Agency, Bandung, West Java 40173, IndonesiaResearch and Development Center, Indonesian Agency for Meteorology Climatology and Geophysics, Jakarta Pusat 10720, IndonesiaThe cold pool outflow has been previously shown to be generated by decaying Mesoscale Convective Complexes (MCCs) in the Maritime Continent. The cold pool also has a main role in the development processes of oceanic convective systems inducing heavy rainfall. This study investigated a cold pool event (January 1-2, 2021) related to a heavy rainfall system over the coastal region of Lampung, Southern Sumatra, within a high-resolution model simulation using a regional numerical weather prediction of the Weather Research and Forecasting (WRF) with convection permitting of 1 km spatial resolution, which was validated by satellite and radar data observations. It is important to note that the intensity, duration, timing, and structure of heavy rainfall simulated were in good agreement with satellite-observed rainfall. The results also showed that a cold pool (CP) plays an important role in inducing Mesoscale Convective Complex (MCC) and was responsible for the development of an offshore propagation of land-based convective systems due to the late afternoon rainfall over inland. This study also suggests that the propagation speed of the CP 8.8 m·s−1 occurring over the seaside of the coastal region, the so-called CP-coastal, is a plausible mechanism for the speed of the offshore-propagating convection, which is dependent on both the background prevailing wind and outflow. These conditions help to maintain the near-surface low temperatures and inhibit cold pool dissipation, which has implications for the development of consecutive convection.http://dx.doi.org/10.1155/2021/2047609
spellingShingle Erma Yulihastin
Ibnu Fathrio
Trismidianto
Fadli Nauval
Elfira Saufina
Wendi Harjupa
Didi Satiadi
Danang Eko Nuryanto
Convective Cold Pool Associated with Offshore Propagation of Convection System over the East Coast of Southern Sumatra, Indonesia
Advances in Meteorology
title Convective Cold Pool Associated with Offshore Propagation of Convection System over the East Coast of Southern Sumatra, Indonesia
title_full Convective Cold Pool Associated with Offshore Propagation of Convection System over the East Coast of Southern Sumatra, Indonesia
title_fullStr Convective Cold Pool Associated with Offshore Propagation of Convection System over the East Coast of Southern Sumatra, Indonesia
title_full_unstemmed Convective Cold Pool Associated with Offshore Propagation of Convection System over the East Coast of Southern Sumatra, Indonesia
title_short Convective Cold Pool Associated with Offshore Propagation of Convection System over the East Coast of Southern Sumatra, Indonesia
title_sort convective cold pool associated with offshore propagation of convection system over the east coast of southern sumatra indonesia
url http://dx.doi.org/10.1155/2021/2047609
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