2011Unpublished venueRequires access

Characteristics of GPS precipitable water vapor during a heavy rain of western Pacific subtropical high

Yun Sun

Open publisher page 0 citations

Abstract

Based on precipitable water vapor received from ground-based GPS,data of dense surface automatical meteorological stations,and conventional sounding data in Shijiazhuang on August 2010,this paper studied the evolution tendency of GPS precipitable water vapor and potential pseudo-equivalent temperature during a heavy rain induced by the advance and retreat of the west Pacific subtropical high.The results show:(1)Rainfall usually occurs when the GPS precipitable water vapor is higher than the average value,especially near its maximum value.The heavy rain period is corresponding to the maximum stage of GPS precipitable water vapor.Upper-level trough is helpful to the occurrence of the convective heavy precipitation at the late period of GPS precipitable water vapor increasing.Weak precipitation will continue at the early period of GPS precipitable water vapor decreasing.(2)In the stability precipitation process,the GPS precipitable water vapor shows a multi-peak wave shape,and its amplitude is relatively small.The heavy rain period is corresponding to the maximum stage of GPS precipitable water vapor.In the convective precipitation process,the GPS precipitable water vapor changes dramatically,and the peaks of GPS precipitable water vapor and actual precipitation are exactly corresponding.(3)Rainfall easily occurs when the deviation coefficient of GPS precipitable water vapor is positive,and the heavy rainfall generally happens while the deviation coefficient is higher than one.The deviation coefficient of convective thunderstorm or shower is slightly smaller than that of stability precipitation.(4)The prophase high-energy accumulation is a necessary condition of rainfall.The rainfall of subtropical high usually occurs in the rapid decline phase of potential pseudo-equivalent temperature or its valley areas.The precipitation will be stronger when the potential pseudo-equivalent temperature is at higher peak with more sharp movement and longer duration of high value.

About this research paper

What this paper is about

Based on precipitable water vapor received from ground-based GPS,data of dense surface automatical meteorological stations,and conventional sounding data in Shijiazhuang on August 2010,this paper studied the evolution tendency of GPS precipitable water vapor and potential pseudo-equivalent temperature during a heavy rain induced by the advance and retreat of the west Pacific subtropical high.The results show:(1)Rainfall usually occurs when the GPS precipitable water vapor is higher than the average value,especially near its maximum value.The heavy rain period is corresponding to the maximum stage of GPS precipitable water vapor.Upper-level trough is helpful to the occurrence of the convective heavy precipitation at the late period of GPS precipitable water vapor increasing.Weak precipitation will continue at the early period of GPS precipitable water vapor decreasing.(2)In the stability precipitation process,the GPS precipitable water vapor shows a multi-peak wave shape,and its amplitude is relatively small.The heavy rain period is corresponding to the maximum stage of GPS precipitable water vapor.In the convective precipitation process,the GPS precipitable water vapor changes dramatically,and the peaks of GPS precipitable water vapor and actual precipitation are exactly corresponding.(3)Rainfall easily occurs when the deviation coefficient of GPS precipitable water vapor is positive,and the heavy rainfall generally happens while the deviation coefficient is higher than one.The deviation coefficient of convective thunderstorm or shower is slightly smaller than that of stability precipitation.(4)The prophase high-energy accumulation is a necessary condition of rainfall.The rainfall of subtropical high usually occurs in the rapid decline phase of potential pseudo-equivalent temperature or its valley areas.The precipitation will be stronger when the potential pseudo-equivalent temperature is at higher peak with more sharp movement and longer duration of high value.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Based on precipitable water vapor received from ground-based GPS,data of dense surface automatical meteorological stations,and conventional sounding data in Shijiazhuang on August 2010,this paper studied the evolution tendency of GPS precipitable water vapor and potential pseudo-equivalent temperature during a heavy rain induced by the advance and retreat of the west Pacific subtropical high.The results show:(1)Rainfall usually occurs when the GPS precipitable water vapor is higher than the average value,especially near its maximum value.The heavy rain period is corresponding to the maximum stage of GPS precipitable water vapor.Upper-level trough is helpful to the occurrence of the convective heavy precipitation at the late period of GPS precipitable water vapor increasing.Weak precipitation will continue at the early period of GPS precipitable water vapor decreasing.(2)In the stability precipitation process,the GPS precipitable water vapor shows a multi-peak wave shape,and its amplitude is relatively small.The heavy rain period is corresponding to the maximum stage of GPS precipitable water vapor.In the convective precipitation process,the GPS precipitable water vapor changes dramatically,and the peaks of GPS precipitable water vapor and actual precipitation are exactly corresponding.(3)Rainfall easily occurs when the deviation coefficient of GPS precipitable water vapor is positive,and the heavy rainfall generally happens while the deviation coefficient is higher than one.The deviation coefficient of convective thunderstorm or shower is slightly smaller than that of stability precipitation.(4)The prophase high-energy accumulation is a necessary condition of rainfall.The rainfall of subtropical high usually occurs in the rapid decline phase of potential pseudo-equivalent temperature or its valley areas.The precipitation will be stronger when the potential pseudo-equivalent temperature is at higher peak with more sharp movement and longer duration of high value.

Key concepts: Precipitable water, Environmental science, Precipitation, Water vapor, Atmospheric sciences, Subtropical ridge, Meteorology, Climatology

Related papers

Back to paper searchBrowse research topicsOriginal source
Characteristics of GPS precipitable water vapor during a heavy rain of western Pacific subtropical high — Research Paper | ScholarLens