In the early 1990s, the mei-yu rainfall over South China in early boreal summer exhibited an
abrupt change and northward extension. This change altered the pattern of East Asian …

East Asian summer rainfall is affected by both the continental northern East Asian low
(NEAL) and the western North Pacific subtropical high (WNPSH) in the lower troposphere …

Abstract The Northwest Pacific Subtropical High (hereinafter referred to as the subtropical
high, NWPSH) is a large-scale circulation system affecting China climate. To further …

Previous studies revealed the double-peak mode (DPM) in South China precipitation,
corresponding to the two stages in the rainy season, ie the first rainy stage (FRS) and the …

The rapid warming trend during the last deglaciation triggered significant global climate
instabilities due to a complex non-linear response of the climate system to the gradual …

Abstract The South Asian high (SAH) and the North Pacific subtropical high (NPSH) are two
crucial systems affecting the summer rainfall over East Asia. Features of the relative vorticity …

The impact of anomalous sea surface temperature (SST) warming in the Kuroshio Extension
in the previous winter on the East Asian summer monsoon (EASM) was investigated by …

This study investigates the features of eastward extension of the South Asian high (SAH)
and its connection with diabatic heating and rainfall over eastern Asia on subseasonal time …

The summer rainfall over the middle‐lower valley of the Yangtze River and over the whole
eastern China experienced a notable regime shift in about 1979. This change is consistent …

West China autumn precipitation (WCAP) is the final stage of the rainy season in mainland
China and is characterized as the secondary peak in annual cycle of precipitation in West …