Features and Causality Analysis on the Unusual Rainstorm in Guangzhou during October,2011
Feng Hou-wen
Abstract
Feng Hou-wen
Abstract
Causality analysis on an unusual rainstorm in Guangzhou during 13-14 October,2011 is conducted from the perspective of background circulation,radar signatures and physical elements with the data of doppler radar,boudary layer wind profiler,mesoscale automatic weather station and the NCEP reanalysis data(1×1deg).Results show that cold air instrusion,movement of the sutropical high ridge triggered the heavy torrential rain event;vertical motion above Guagnzhou,convergence of perstistent southwest moisture jet ahead of westerly trough and the southeast watervapor transportation to the south of low level shear are favorable for the initialization and the maintenance of the heavy rainfall.The start(end) of clockwize rotation of wind direction and the rapid strengthening(Weakening) of wind speed in mid-low layers agreed well with the start(end) of rainfall event;and the covergence of cold and warm air brought the peak of the rainstorm.
OpenAlex reports 2 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Causality analysis on an unusual rainstorm in Guangzhou during 13-14 October,2011 is conducted from the perspective of background circulation,radar signatures and physical elements with the data of doppler radar,boudary layer wind profiler,mesoscale automatic weather station and the NCEP reanalysis data(1×1deg).Results show that cold air instrusion,movement of the sutropical high ridge triggered the heavy torrential rain event;vertical motion above Guagnzhou,convergence of perstistent southwest moisture jet ahead of westerly trough and the southeast watervapor transportation to the south of low level shear are favorable for the initialization and the maintenance of the heavy rainfall.The start(end) of clockwize rotation of wind direction and the rapid strengthening(Weakening) of wind speed in mid-low layers agreed well with the start(end) of rainfall event;and the covergence of cold and warm air brought the peak of the rainstorm.
Key concepts: Mesoscale meteorology, Environmental science, Climatology, Meteorology, Cold front, Doppler radar, Trough (economics), Warm front