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Diurnal cycle of marine atmospheric boundary layer during the 1998 summer monsoon onset over South China Sea

Severe weather phenomena that can affect Hong Kong include tropical cyclones, strong winter and summer monsoon winds,monsoon troughs and thunderstorms with associated squalls that are most frequent from April to September.

Furthermore, the heat storage anomaly of December in the SCS can be used as a predictor for the onset of the SCS summer monsoon.

Further, the east Asian summer monsoon is closely positively related with the summer Pacific High intensity and with the second mode of northern SLP on the scale of more than 30 years.

Heavy rains occur during a summer monsoon.

Evolution character of flow field during onset phase of the Indian summer monsoon

The results show that the summer monsoon of Nansha sea surface came from the west path and south path from the monsoon air current of this sea area.

Huang shisong tang mingmin. the early summer flood periods of southern china and the summer monsoon circulation of east asia. journal of tropical meteorolog.

The variations of weather situations and meteorological characters and air-sea fluxes were obvious during the summer monsoon along with th…

I have been comforting myself, and the nightmare like the past has been drifting away with the summer monsoon, but once it is mentioned, it happens again on the eve of yesterday.

Characteristics of the water vapor transporting path in strong and weak SCS summer monsoon years

Gentler but more persistent bad weather - the downpours of the summer monsoon - is also being taken into account.

Most of India’s crucial rain is brought by the summer monsoon, which falls, with luck, in just a few weeks between June and September.

Definition and features of the north edge of Asian summer monsoon

The Indian summer monsoon starts in the 32nd pentad (5~10 th of June) and ends in the 49 th pentad (1~5 th of September).

summer monsoon造句

The results of the analysis indicate that:1)North China has more summer rainfall during strong East Asian summer monsoon years but less summer rainfall during weak East Asian summer monsoon years.

Historical weather patterns do, however, suggest linkages across the Northern Hemisphere's middle latitudes, intermittently coupled in turn to India's summer monsoon cycles.

The summer monsoon reliably delivers an intense abundance of water, swelling rivers, lakes and flooding water-courses incredibly fast.

The negative correlation between the interannual variability of IODM and that of SCS summer monsoon is significant during the warm phase of long-term trend but insignificant during the cool phase.

The previously winter Kuroshio SSTA relates greatly to the East Asian summer monsoon (EASM).

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