Climatology of Planetary Boundary Layer Height-Controlling Meteorological Parameters Over the Korean Peninsula

Planetary boundary layer (PBL) height plays a significant role in climate modeling, weather forecasting, air quality prediction, and pollution transport processes. This study examined the climatology of PBL-associated meteorological parameters over the Korean peninsula and surrounding sea using data...

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Main Authors: Shaik Allabakash, Sanghun Lim
Format: Article
Language:English
Published: MDPI AG 2020-08-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/16/2571
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spelling doaj-a4d22ea9ff4846ff812b8275cf6521812020-11-25T03:37:11ZengMDPI AGRemote Sensing2072-42922020-08-01122571257110.3390/rs12162571Climatology of Planetary Boundary Layer Height-Controlling Meteorological Parameters Over the Korean PeninsulaShaik Allabakash0Sanghun Lim1Korea Institute of Civil Engineering and Building Technology, Ilsan 10223, KoreaKorea Institute of Civil Engineering and Building Technology, Ilsan 10223, KoreaPlanetary boundary layer (PBL) height plays a significant role in climate modeling, weather forecasting, air quality prediction, and pollution transport processes. This study examined the climatology of PBL-associated meteorological parameters over the Korean peninsula and surrounding sea using data from the ERA5 dataset produced by the European Centre for Medium-range Weather Forecasts (ECMWF). The data covered the period from 2008 to 2017. The bulk Richardson number methodology was used to determine the PBL height (PBLH). The PBLH obtained from the ERA5 data agreed well with that derived from sounding and Global Positioning System Radio Occultation datasets. Significant diurnal and seasonal variability in PBLH was observed. The PBLH increases from morning to late afternoon, decreases in the evening, and is lowest at night. It is high in the summer, lower in spring and autumn, and lowest in winter. The variability of the PBLH with respect to temperature, relative humidity, surface pressure, wind speed, lower tropospheric stability, soil moisture, and surface fluxes was also examined. The growth of the PBLH was high in the spring and in southern regions due to the low soil moisture content of the surface. A high PBLH pattern is evident in high-elevation regions. Increasing trends of the surface temperature and accordingly PBLH were observed from 2008 to 2017.https://www.mdpi.com/2072-4292/12/16/2571climatologyKorean peninsulaplanetary boundary layer heightsurface meteorological parameters
collection DOAJ
language English
format Article
sources DOAJ
author Shaik Allabakash
Sanghun Lim
spellingShingle Shaik Allabakash
Sanghun Lim
Climatology of Planetary Boundary Layer Height-Controlling Meteorological Parameters Over the Korean Peninsula
Remote Sensing
climatology
Korean peninsula
planetary boundary layer height
surface meteorological parameters
author_facet Shaik Allabakash
Sanghun Lim
author_sort Shaik Allabakash
title Climatology of Planetary Boundary Layer Height-Controlling Meteorological Parameters Over the Korean Peninsula
title_short Climatology of Planetary Boundary Layer Height-Controlling Meteorological Parameters Over the Korean Peninsula
title_full Climatology of Planetary Boundary Layer Height-Controlling Meteorological Parameters Over the Korean Peninsula
title_fullStr Climatology of Planetary Boundary Layer Height-Controlling Meteorological Parameters Over the Korean Peninsula
title_full_unstemmed Climatology of Planetary Boundary Layer Height-Controlling Meteorological Parameters Over the Korean Peninsula
title_sort climatology of planetary boundary layer height-controlling meteorological parameters over the korean peninsula
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2020-08-01
description Planetary boundary layer (PBL) height plays a significant role in climate modeling, weather forecasting, air quality prediction, and pollution transport processes. This study examined the climatology of PBL-associated meteorological parameters over the Korean peninsula and surrounding sea using data from the ERA5 dataset produced by the European Centre for Medium-range Weather Forecasts (ECMWF). The data covered the period from 2008 to 2017. The bulk Richardson number methodology was used to determine the PBL height (PBLH). The PBLH obtained from the ERA5 data agreed well with that derived from sounding and Global Positioning System Radio Occultation datasets. Significant diurnal and seasonal variability in PBLH was observed. The PBLH increases from morning to late afternoon, decreases in the evening, and is lowest at night. It is high in the summer, lower in spring and autumn, and lowest in winter. The variability of the PBLH with respect to temperature, relative humidity, surface pressure, wind speed, lower tropospheric stability, soil moisture, and surface fluxes was also examined. The growth of the PBLH was high in the spring and in southern regions due to the low soil moisture content of the surface. A high PBLH pattern is evident in high-elevation regions. Increasing trends of the surface temperature and accordingly PBLH were observed from 2008 to 2017.
topic climatology
Korean peninsula
planetary boundary layer height
surface meteorological parameters
url https://www.mdpi.com/2072-4292/12/16/2571
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