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- W2371911849 abstract "Due to the higher temporal and spatial resolution and the better integrality of long-term satellite infrared(IR) temperature of black body(TBB) data,a climatology of deep convection during summer over South China and adjacent seas is presented in this paper based on the 1-hourly IR TBB data during June—August of 1996—2007(except 2004).The results show that the climatological characteristics of deep convection denoted by TBB ≤-52 ℃ over South China and adjacent seas are basically consistent with those previous statistical studies based on the surface thunderstorm observations and the low-orbit satellite lightning observations.The monthly variations,ten-day variations,five-day variations and diurnal variations of deep convection over South China and adjacent seas are focused on in this paper.The results show that there are 5 active deep-convection areas in South China and adjacent seas during the period of June—August.The monthly variations of the deep convection over South China and adjacent seas are closely associated with the large-scale atmospheric circulation.The deep convection over the land in South China is more active in June,while that over South China Sea is more active in July and August.The development of the deep convection over South China and adjacent seas has a characteristic of intermittence,and its period is about 3～5 five-day.However,the deep convection over the neighboring areas of coastline in South China remains more active during summer,and has no obvious intermittence characteristic.The ten-day and five-day variations of deep convection show that there are different variations of deep convection over different areas in South China and adjacent seas.The tendency of the deep convection over the land in South China is negatively correlated with that over South China Sea.The diurnal variations of the deep convection over South China and adjacent seas show that the sea-land breeze caused by the thermal difference between land and sea and the mountain-valley breeze caused by the thermal difference between mountains and plains or basins make the deep convection propagate from sea to land in the afternoon and from land to sea after midnight,and the convection over mountains propagate from mountains to plains after midnight.The different diurnal variations of deep convection over different underlying surfaces show that not only there are general mountain deep convection,marine deep convection and multi-peak deep convection,but also there is longer-duration deep convection over coastal land and sea and other deep convection triggered and developed by larger-scale synoptic systems in South China during summer." @default.
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- W2371911849 date "2011-01-01" @default.
- W2371911849 modified "2023-09-23" @default.
- W2371911849 title "A CLIMATOLOGY OF DEEP CONVECTION OVER SOUTH CHINA AND ADJACENT SEAS DURING SUMMER" @default.
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