2008Torrential Rain and DisastersRequires access

Influence of Physical Features on Heavy Rain Region in the Middle Part of Henan Province

Lei Zhe

Open publisher page 0 citations

Abstract

The heavy rain process in the middle part of Henan province during 4-6 July 2007 is diagnosed with routine meteorological observations and NCEP 1°×1° 6 h reanalysis data.The influence of physical features on the heavy rain is mainly analyzed.Results indicate that the steady Subtropical High over the West Pacific,the trough at middle level of the troposphere and the shear line at low level are the main influencing systems.The southwesterly jet at low level provides the abundant water vapor and the instability energy.The heavy rain region is located at the north side of the exit area of the jet axis.The southerly component of the wind speed has a greater impact on the precipitation intensity.The release of instability energy is rapidly triggered by the cyclonic convergence at the middle low level and the anticyclonic divergence at the upper level.The rainstorm region is exactly coincident with the thick ascending motions.

About this research paper

What this paper is about

The heavy rain process in the middle part of Henan province during 4-6 July 2007 is diagnosed with routine meteorological observations and NCEP 1°×1° 6 h reanalysis data.The influence of physical features on the heavy rain is mainly analyzed.Results indicate that the steady Subtropical High over the West Pacific,the trough at middle level of the troposphere and the shear line at low level are the main influencing systems.The southwesterly jet at low level provides the abundant water vapor and the instability energy.The heavy rain region is located at the north side of the exit area of the jet axis.The southerly component of the wind speed has a greater impact on the precipitation intensity.The release of instability energy is rapidly triggered by the cyclonic convergence at the middle low level and the anticyclonic divergence at the upper level.The rainstorm region is exactly coincident with the thick ascending motions.

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

The heavy rain process in the middle part of Henan province during 4-6 July 2007 is diagnosed with routine meteorological observations and NCEP 1°×1° 6 h reanalysis data.The influence of physical features on the heavy rain is mainly analyzed.Results indicate that the steady Subtropical High over the West Pacific,the trough at middle level of the troposphere and the shear line at low level are the main influencing systems.The southwesterly jet at low level provides the abundant water vapor and the instability energy.The heavy rain region is located at the north side of the exit area of the jet axis.The southerly component of the wind speed has a greater impact on the precipitation intensity.The release of instability energy is rapidly triggered by the cyclonic convergence at the middle low level and the anticyclonic divergence at the upper level.The rainstorm region is exactly coincident with the thick ascending motions.

Key concepts: Trough (economics), Subtropical ridge, Troposphere, Anticyclone, Climatology, Precipitation, Jet stream, Geography

Related papers

Back to paper searchBrowse research topicsOriginal source
Influence of Physical Features on Heavy Rain Region in the Middle Part of Henan Province — Research Paper | ScholarLens