Relationship between intraseasonal oscillation and diurnal variation of summer rainfall over the South China Sea

2008 ◽  
Vol 35 (3) ◽  
Author(s):  
Chang-Hoi Ho ◽  
Myung-Sook Park ◽  
Yong-Sang Choi ◽  
Yukari N. Takayabu
Keyword(s):  
South China Sea ◽  
Diurnal Variation ◽  
South China ◽  
Intraseasonal Oscillation ◽  
Summer Rainfall ◽  
The South China Sea ◽  
The South ◽  
China Sea

Signals of the South China Sea summer rainfall variability in the Indian Ocean

2015 ◽  
Vol 46 (9-10) ◽  
pp. 3181-3195 ◽  
Author(s):  
Zhuoqi He ◽  
Renguang Wu ◽  
Weiqiang Wang
Keyword(s):  
Indian Ocean ◽  
South China Sea ◽  
South China ◽  
Rainfall Variability ◽  
Summer Rainfall ◽  
The South China Sea ◽  
The South ◽  
China Sea ◽  
The Indian Ocean

scholarly journals Mechanisms of Northward-Propagating Intraseasonal Oscillation over the South China Sea during the Pre-Monsoon Period

2019 ◽  
Vol 32 (11) ◽  
pp. 3297-3311 ◽  
Author(s):  
Bin Zheng ◽  
Yanyan Huang
Keyword(s):  
South China Sea ◽  
South China ◽  
Intraseasonal Oscillation ◽  
The South China Sea ◽  
Boreal Summer ◽  
The South ◽  
China Sea ◽  
Northward Propagation ◽  
The Mean ◽  
Barotropic Vorticity

Abstract In the present study, the spatiotemporal structures of the northward-propagating intraseasonal oscillation (ISO) over the South China Sea (SCS) in the premonsoon period are analyzed by using the TropFlux air–sea flux and the JRA-55 reanalysis datasets. It is found that the SCS ISO is significant in the premonsoon season with a strong component of the northward propagation and that the mean state is different from that of summertime. Moreover, there are similar structures to those of a boreal summer ISO event except for the perturbation vorticity with no obvious phase leading. An internal atmospheric dynamics mechanism is proposed to understand the cause of the northward propagation of the ISO during the premonsoon period based on the spatial and temporal structures of the ISOs. The key process associated with this mechanism is the barotropic vorticity advection by the mean barotropic southerly winds, and the main barotropic vorticity around the convection center can be induced by the vertical advection of the mean vorticity. Low-level moisture convergence caused by anomalous flow is a supplementary mechanism to drive the ISOs northward during the premonsoon period, particularly over the northern SCS. In this mechanism, the SST-induced wind anomalies play a more important role than the convection-induced wind anomalies. The summer monsoon circulation has not built up during the premonsoon period, and thus the vertical wind shear effect and the barotropic vorticity effect associated with the meridional advection of baroclinic vorticity are not essential to cause the northward propagation of the ISOs over the SCS.

scholarly journals The Effect of Boreal Summer Intraseasonal Oscillation on Evaporation Duct and Electromagnetic Propagation over the South China Sea

Atmosphere ◽  
2020 ◽  
Vol 11 (12) ◽  
pp. 1298
Author(s):  
Wentao Jia ◽  
Weimin Zhang ◽  
Jiahua Zhu ◽  
Jilin Sun
Keyword(s):  
South China Sea ◽  
South China ◽  
Dominant Role ◽  
Intraseasonal Oscillation ◽  
The South China Sea ◽  
Boreal Summer ◽  
The South ◽  
Boreal Summer Intraseasonal Oscillation ◽  
China Sea ◽  
Evaporation Duct

Intraseasonal oscillation of the evaporation duct, lasting 30–60 days, has been identified over the South China Sea (SCS) summer monsoon region based on multiple reanalyses and observational data. The boreal summer intraseasonal oscillation (BSISO) causes anomalies at the air–sea boundary and thus plays a dominant role in modulating the variation of the evaporation duct. The height and strength of the duct enhance/suppress during the negative/positive phase of the BSISO over the SCS. This results from the fact that active BSISO convection reduces solar radiation reaching the sea surface by increasing cumulus cloud cover, whereupon precipitation and water vapor transported by the enhanced southwest jet increase humidity over the air–sea boundary. Reduced air–sea temperatures and humidity differences lead to a weaker evaporation duct. Usually, the temporal evolution of the evaporation duct lags 2–4 days behind the BSISO, with the center of evaporation duct anomalies farther south than the BSISO. Simulated electromagnetic fields substantively influence the condition of the evaporation duct, with obvious over-the-horizon and radar blind spot effects in the typical negative phase of the BSISO, which is very different from standard atmospheric conditions.

Impact of intraseasonal oscillation on the tropical cyclone track in the South China Sea

2014 ◽  
Vol 44 (5-6) ◽  
pp. 1505-1519 ◽  
Author(s):  
Lei Yang ◽  
Yan Du ◽  
Dongxiao Wang ◽  
Chunzai Wang ◽  
Xin Wang
Keyword(s):  
Tropical Cyclone ◽  
South China Sea ◽  
South China ◽  
Intraseasonal Oscillation ◽  
The South China Sea ◽  
Cyclone Track ◽  
The South ◽  
Tropical Cyclone Track ◽  
China Sea
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