Daily climate data at 110 stations during 1961-2010 were selected to examine the changing characteristics of climate factors and extreme climate events in South China. The annual mean surface air temperature has incre...Daily climate data at 110 stations during 1961-2010 were selected to examine the changing characteristics of climate factors and extreme climate events in South China. The annual mean surface air temperature has increased significantly by 0.16℃ per decade, most notably in the Pearl River Delta and in winter. The increase rate of the annual extreme minimum temperature (0.48℃ per decade) is over twice that of the annual extreme maximum temperature (0.20℃ per decade), and the increase of the mean temperature is mainly the result of the increase of the extreme minimum temperature. The increase rate of high-temperature days (1.1 d per decade) is close to the decrease rate of low-temperature days (-1.3 d per decade). The rainfall has not shown any significant trend, but the number of rainy days has decreased and the rain intensity has increased. The regional mean sunshine duration has a significant decreasing trend of -40.9 h per decade, and the number of hazy days has a significant increasing trend of 6.3 d per decade. The decrease of sunshine duration is mainly caused by the increase of total cloud, not by the increase of hazy days in South China. Both the regional mean pan evaporation and mean wind speed have significant decreasing trends of -65.9 mm per decade and -0.11 m s-1 per decade, respectively. The decrease of both sunshine duration and mean wind speed plays an important role in the decrease of pan evaporation. The number of landing tropical cyclones has an insignificant decreasing trend of -0.6 per decade, but their intensities show a weak increasing trend. The formation location of tropical cyclones landing in South China has converged towards 10-19°N, and the landing position has shown a northward trend. The date of the first landfall tropical cyclone postpones 1.8 d per decade, and the date of the last landfall advances 3.6 d per decade, resulting in reduction of the typhoon season by 5.4 d per decade.展开更多
Built by the royal family in the Ming Dynasty,the Da Bao En Temple is known as the greatest temple in ancient Nanjing,whose predecessor is the Chang Gan Temple built in the Six Dynasties.Archaeological excavations of ...Built by the royal family in the Ming Dynasty,the Da Bao En Temple is known as the greatest temple in ancient Nanjing,whose predecessor is the Chang Gan Temple built in the Six Dynasties.Archaeological excavations of the Da Bao En Temple and the underground palace of Chang Gan Temple built in the North Song Dynasty(AD960 AD1127) have been appraised as one of the 10 greatest archaeological discoveries in 2010 in China.Many artefacts discovered in the underground palace have shown their important historical meanings and scientific values,such as the Qibao King Asoka Tower,golden and silver coffins,Buddhist relics,the silk textiles,glasses,and spices etc.In this paper,stereomicroscope,SEM-EDS and LA-ICP-AES are used to investigate chemical composition,microstructure and current preservation status for the unearthed glasswares.The results indicate that the glass bottle coded as TH1 and the glass calyx coded as TN5 are made of lead-silicate glass,while the chemical composition of the glass bottle coded as TN9 is quite distinct from that of native glasswares.All three articles have been weathered in some degrees.Given the shape,it is deduced that TH1 is a typical glassware used in burying Buddhist relics at that time,TN5 a domestic glassware with typical Sassanian style,and TN9 an imported Islamic glass,providing important information about culture exchanges between China and the foreign countries in the North Song Dynasty.展开更多
基金supported by the Special Climate Change Research Program of China Meteorological Administration (No. CCSF-09-11, CCSF-09-03, CCSF2011-25, and CCSF201211)the Science and Technology Planning Project of Guangdong province (No.2011A030200021)
文摘Daily climate data at 110 stations during 1961-2010 were selected to examine the changing characteristics of climate factors and extreme climate events in South China. The annual mean surface air temperature has increased significantly by 0.16℃ per decade, most notably in the Pearl River Delta and in winter. The increase rate of the annual extreme minimum temperature (0.48℃ per decade) is over twice that of the annual extreme maximum temperature (0.20℃ per decade), and the increase of the mean temperature is mainly the result of the increase of the extreme minimum temperature. The increase rate of high-temperature days (1.1 d per decade) is close to the decrease rate of low-temperature days (-1.3 d per decade). The rainfall has not shown any significant trend, but the number of rainy days has decreased and the rain intensity has increased. The regional mean sunshine duration has a significant decreasing trend of -40.9 h per decade, and the number of hazy days has a significant increasing trend of 6.3 d per decade. The decrease of sunshine duration is mainly caused by the increase of total cloud, not by the increase of hazy days in South China. Both the regional mean pan evaporation and mean wind speed have significant decreasing trends of -65.9 mm per decade and -0.11 m s-1 per decade, respectively. The decrease of both sunshine duration and mean wind speed plays an important role in the decrease of pan evaporation. The number of landing tropical cyclones has an insignificant decreasing trend of -0.6 per decade, but their intensities show a weak increasing trend. The formation location of tropical cyclones landing in South China has converged towards 10-19°N, and the landing position has shown a northward trend. The date of the first landfall tropical cyclone postpones 1.8 d per decade, and the date of the last landfall advances 3.6 d per decade, resulting in reduction of the typhoon season by 5.4 d per decade.
基金supported by State Administration of Cultural Heritage for "Research of Protection Technology for Nanjing Da Bao En Temple"the Innovation Key Program of the Chinese Academy of Sciences (GrantNo. KZCX2-EW-QN607)
文摘Built by the royal family in the Ming Dynasty,the Da Bao En Temple is known as the greatest temple in ancient Nanjing,whose predecessor is the Chang Gan Temple built in the Six Dynasties.Archaeological excavations of the Da Bao En Temple and the underground palace of Chang Gan Temple built in the North Song Dynasty(AD960 AD1127) have been appraised as one of the 10 greatest archaeological discoveries in 2010 in China.Many artefacts discovered in the underground palace have shown their important historical meanings and scientific values,such as the Qibao King Asoka Tower,golden and silver coffins,Buddhist relics,the silk textiles,glasses,and spices etc.In this paper,stereomicroscope,SEM-EDS and LA-ICP-AES are used to investigate chemical composition,microstructure and current preservation status for the unearthed glasswares.The results indicate that the glass bottle coded as TH1 and the glass calyx coded as TN5 are made of lead-silicate glass,while the chemical composition of the glass bottle coded as TN9 is quite distinct from that of native glasswares.All three articles have been weathered in some degrees.Given the shape,it is deduced that TH1 is a typical glassware used in burying Buddhist relics at that time,TN5 a domestic glassware with typical Sassanian style,and TN9 an imported Islamic glass,providing important information about culture exchanges between China and the foreign countries in the North Song Dynasty.
