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| 1 | Trends in Extremes of Surface Humidity, Temperature, and Summertime Heat Stress in China显示文摘In the past half century, the mean summertime temperature in China has increased, with nights warm- ing more than days. Using surface station observations, we show that the frequency of extreme heat-stress events in China, caused by extremely hot and humid days as well as by heatwaves lasting for a few days, has increased over the period from 1951 to 1994 When humidity is high, hot weather can cause heat stress in humans. The increased heatrstress trend may pose a public health | Julian X.L. Wang and Dian J. Gaffen NOAA/ Air Resources Laboratory, Silver Spring, MD, 20910, USA | 2001 | Advances in Atmospheric Sciences2001，18，5： | 6 |
| 2 | Influenza A virus-associated acute necrotizing encephalopathy in the United States 显示文摘 | Weitkamp JH Spring MD Brogan T | 2004 | Pediatri Infect Dis J2004，23，3： | 1 |
| 3 | High prevalence of sessile serrated adenomas with BRAF mutation:A prospective study of patients undergoing colonoscopy显示文摘 | SPRING KJ KARAMATIC R WALSH MD | 2006 | Gastroenterology2006，131，5： | 1 |
| 4 | Influenza A virus-associated acute necrotizing encephalopathy in the United States显示文摘 | Weitkamp JH Spring MD Brogan T | 2004 | Pediatr Infect Dis J2004，23，3： | 1 |
| 5 | Influenza A virus-associated acute necrotizing encephalopathy in the United States显示文摘 | Weitkamp J-H Spring MD Brogan T | 2004 | Pediatr Infect Dis J2004，23，3： | 1 |
| 6 | Surface ozone trend details and interpretations in Beijing, 2001-2006显示文摘 | NOAA Air Resources Laboratory Silver Spring MD Tang G Li X Wang Y | 2009 | Atmospheric Chemistry and Physics2009，9，： | 1 |
| 7 | Recombinant Liver Stage Antigen-1 (LSA-1) formulated with AS01 or AS02 is safe,elicits high titer antibody and induces IFN-gamma/IL-2 CD4+T cells but does not protect against experimental Plasmodium falciparum infection显示文摘 | Cummings JF Spring MD Schwenk RJ | 2010 | Vaccine2010，28，31： | 1 |
| 8 | Influenza A,virus-associated acute necrotizing encephalopathy in the United States显示文摘 | Weitkarmp JH Spring MD Brogan T | 2004 | Pediatr Infect2004，23，2： | 1 |
| 9 | Cloud microphysical and rainfall responses to zonal perturbations of sea surface temperature:A cloud-resolving modeling study显示文摘The cloud microphysical and rainfall responses to zonal perturbations of sea surface temperature (SST) are investigated by analyzing the equilibrium simulation data (from day 31-40) obtained from a series of two-dimensional cloud-resolving simulations with a zonal model domain of 768 km. Four experiments imposed by zonal SST perturbations of wavenumbers 1 (SST29Z1), 2 (SST29Z2), 4 (SST29Z4), and 8 (SST29Z8) are compared to the control experiment imposed by zonally uniform SST (SST29). The model domain mean SST is 29 °C, and the two-dimensional cloud-resolving model with a cyclic lateral boundary is also imposed by zero vertical velocity and constant zonal wind. The time and model domain mean surface rain rates in SST29Z1, SST29Z2, and SST29Z8 are about 10% larger than those in SST29, whereas the mean surface rain rates in SST29Z4 and SST29 are similar. The analysis of mean surface rainfall budgets shows that local water vapor and hydrometeor changes play important roles in determining the differences and similarities in mean surface rain rate between the perturbation experiments and the control experiment. Both convective and stratiform rain rates are larger in SST29Z1 and SST29Z2 than in SST29 due to the smaller advection of rain from convective regions into raining stratiform regions and the larger vapor condensation rates associated with the larger water vapor convergence over raining stratiform regions in SST29Z1 and SST29Z2. The convective rain rates are larger in SST29Z4 and SST29Z8 than in SST29 because of the larger condensation rates associated with the larger water vapor convergence over convective regions in SST29Z4 and SST29Z8. The stratiform rain rates in SST29Z4 and SST29Z8 are smaller than in SST29 due to the smaller vapor condensation rates and smaller collection rates of cloud water by rain over raining stratiform regions in SST29Z4 and SST29Z8. | Xiaopeng Cuia, Xiaofan Lib, Zhiping Zongc a Laboratory of Cloud-Precipitation Physics and Severe Storms (LACS), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China b Joint Center for Satellite Data Assimilation and NOAA/NESDIS/Office of Research and Applications, Camp Springs, MD, USA c National Meteorological Center, China Meteorological Administration, Beijing 100081, China | 2009 | Progress in Natural Science:Materials International2009，19，5： | 1 |
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