Observational study on melting layer characteristics over Palau in Pacific Ocean

U. V.Murali Krishna; K. Krishna Reddy; R. Mastanaiah; Ryuichi Shirooka; Chen Jeih Pan

doi:10.1016/j.jastp.2014.09.015

Observational study on melting layer characteristics over Palau in Pacific Ocean

U. V.Murali Krishna, K. Krishna Reddy, R. Mastanaiah, Ryuichi Shirooka, Chen Jeih Pan

太空科學與工程學系

研究成果: 雜誌貢獻 › 期刊論文 › 同行評審

5 引文斯高帕斯（Scopus）

摘要

In this paper, four years (April, 2003-March, 2007) of wind profiler radar (WPR) observations, Tropical Rainfall Measuring Mission measurements, radiosonde and automatic weather station data are utilized to characterize melting layer/bright band (caused due to the melting of hydrometeors when the precipitation has a significant stratiform cloud contribution) variability during easterly and westerly monsoon periods over Palau in Western Pacific Ocean. Four years observational results show that presence of stratiform precipitation is more in Westerly monsoon compared to Easterly monsoon. However, bright band height (BBH) is lower in Westerly monsoon. It is also observed that the BBH during the year 2006 is higher than 2005 possibly due to El Nino effect.

原文	???core.languages.en_GB???
頁（從 - 到）	132-140
頁數	9
期刊	Journal of Atmospheric and Solar-Terrestrial Physics
卷	121
發行號	PA
DOIs	https://doi.org/10.1016/j.jastp.2014.09.015
出版狀態	已出版 - 1 12月 2014

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10.1016/j.jastp.2014.09.015

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title = "Observational study on melting layer characteristics over Palau in Pacific Ocean",

abstract = "In this paper, four years (April, 2003-March, 2007) of wind profiler radar (WPR) observations, Tropical Rainfall Measuring Mission measurements, radiosonde and automatic weather station data are utilized to characterize melting layer/bright band (caused due to the melting of hydrometeors when the precipitation has a significant stratiform cloud contribution) variability during easterly and westerly monsoon periods over Palau in Western Pacific Ocean. Four years observational results show that presence of stratiform precipitation is more in Westerly monsoon compared to Easterly monsoon. However, bright band height (BBH) is lower in Westerly monsoon. It is also observed that the BBH during the year 2006 is higher than 2005 possibly due to El Nino effect.",

keywords = "Bright band, Radar reflectivity, Radiosonde, TRMM PR Radar, Wind profiler radar",

author = "Krishna, {U. V.Murali} and Reddy, {K. Krishna} and R. Mastanaiah and Ryuichi Shirooka and Pan, {Chen Jeih}",

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TY - JOUR

T1 - Observational study on melting layer characteristics over Palau in Pacific Ocean

AU - Krishna, U. V.Murali

AU - Reddy, K. Krishna

AU - Mastanaiah, R.

AU - Shirooka, Ryuichi

AU - Pan, Chen Jeih

PY - 2014/12/1

Y1 - 2014/12/1

N2 - In this paper, four years (April, 2003-March, 2007) of wind profiler radar (WPR) observations, Tropical Rainfall Measuring Mission measurements, radiosonde and automatic weather station data are utilized to characterize melting layer/bright band (caused due to the melting of hydrometeors when the precipitation has a significant stratiform cloud contribution) variability during easterly and westerly monsoon periods over Palau in Western Pacific Ocean. Four years observational results show that presence of stratiform precipitation is more in Westerly monsoon compared to Easterly monsoon. However, bright band height (BBH) is lower in Westerly monsoon. It is also observed that the BBH during the year 2006 is higher than 2005 possibly due to El Nino effect.

AB - In this paper, four years (April, 2003-March, 2007) of wind profiler radar (WPR) observations, Tropical Rainfall Measuring Mission measurements, radiosonde and automatic weather station data are utilized to characterize melting layer/bright band (caused due to the melting of hydrometeors when the precipitation has a significant stratiform cloud contribution) variability during easterly and westerly monsoon periods over Palau in Western Pacific Ocean. Four years observational results show that presence of stratiform precipitation is more in Westerly monsoon compared to Easterly monsoon. However, bright band height (BBH) is lower in Westerly monsoon. It is also observed that the BBH during the year 2006 is higher than 2005 possibly due to El Nino effect.

KW - Bright band

KW - Radar reflectivity

KW - Radiosonde

KW - TRMM PR Radar

KW - Wind profiler radar

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M3 - 期刊論文

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SN - 1364-6826

VL - 121

SP - 132

EP - 140

JO - Journal of Atmospheric and Solar-Terrestrial Physics

JF - Journal of Atmospheric and Solar-Terrestrial Physics

IS - PA

ER -

Observational study on melting layer characteristics over Palau in Pacific Ocean

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