南海北部航次观测资料显示南海北部表层盐度在2004—2012年期间缓慢降低,2012年盐度达到最低。客观分析数据EN4(the UK Met Office EN.4.0.2 objective analyses)以及OFES(ocean general circulation model for the Earth Simulator)模...南海北部航次观测资料显示南海北部表层盐度在2004—2012年期间缓慢降低,2012年盐度达到最低。客观分析数据EN4(the UK Met Office EN.4.0.2 objective analyses)以及OFES(ocean general circulation model for the Earth Simulator)模式结果都显示南海表层海水盐度在1993—2014年有淡化趋势,最显著区域位于吕宋岛以西和南海南部。盐度收支分析表明淡水强迫在吕宋岛以西海域起主要贡献,而水平平流输运主导南海西部的表层盐度变化。吕宋岛以西表层盐度的降低与近年来沃克环流加强引起的夏季强降雨增加有关。展开更多
短毛五加总甙(AGVPS)是中药短毛五加(Acanthopanax gracilistylus var. pubescens)的有效成份。本文发现短毛五加总甙能抑制正常家兔由多种诱导因素所致的血小板聚集。同时,它还抑制花生四稀酸所致血小板聚集时TXA_2的产生,增加离体家...短毛五加总甙(AGVPS)是中药短毛五加(Acanthopanax gracilistylus var. pubescens)的有效成份。本文发现短毛五加总甙能抑制正常家兔由多种诱导因素所致的血小板聚集。同时,它还抑制花生四稀酸所致血小板聚集时TXA_2的产生,增加离体家兔胸主动脉PGI_2产生。在高脂喂养的动脉粥样硬化的家兔模型上,能提高血浆PGI_2水平。展开更多
基于2004—2018年Argo(Array for Real-Time Geostrophic Oceanography)浮标观测的温度、盐度数据,利用经验正交函数(EOF)分析和小波分析等方法对北印度洋(40°—105°E,5°S—25°N)障碍层时空分布特征进行分析。结果...基于2004—2018年Argo(Array for Real-Time Geostrophic Oceanography)浮标观测的温度、盐度数据,利用经验正交函数(EOF)分析和小波分析等方法对北印度洋(40°—105°E,5°S—25°N)障碍层时空分布特征进行分析。结果显示:北印度洋的东部常年存在障碍层,而西部障碍层出现的概率相对较低;较厚的障碍层出现在阿拉伯海东南部(67°—75°E,3°—12°N)、孟加拉湾(82°—93°E,11°—20°N)和赤道东印度洋(81°—102°E,4°S—3°N)。阿拉伯海东南部和孟加拉湾障碍层厚度以年变化为主,且呈同位相变化,均为冬季最大,夏季最小。赤道东印度洋区域则主要呈现半年周期变化,在夏季和冬季各出现一次峰值。进一步分析表明,孟加拉湾和赤道东印度洋障碍层厚度主要受等温层深度变化影响,混合层深度变化对障碍层厚度变化的影响相对较小;阿拉伯海障碍层厚度同时受等温层深度变化和混合层深度变化影响,其中等温层深度变化对其影响更大。展开更多
In this study, the upper ocean heat content （OHC） variations in the South China Sea （SCS） during 1993- 2006 were investigated by examining ocean temperatures in seven datasets, including World Ocean Atlas 2009 （W...In this study, the upper ocean heat content （OHC） variations in the South China Sea （SCS） during 1993- 2006 were investigated by examining ocean temperatures in seven datasets, including World Ocean Atlas 2009 （WOA09） （climatology）, Ishii datasets, Ocean General Circulation ModeI for the Earth Simulator （OFES）, Simple Ocean Data Assimilation system （SODA）, Global Ocean Data Assimilation System （GODAS）, China Oceanic ReAnalysis system （CORA） , and an ocean reanalysis dataset for the joining area of Asia and Indian-Pacific Ocean （AIPO1.0）. Among these datasets, two were independent of any numerical model, four relied on data assimilation, and one was generated without any data assimilation. The annual cycles revealed by the seven datasets were similar, but the interannual variations were different. Vertical structures of temperatures along the 18~N, 12.75~N, and 120~E sections were compared with data collected during open cruises in 1998 and 2005-08. The results indicated that Ishii, OFES, CORA, and AIPO1.0 were more consistent with the observations. Through systematic shortcomings and advantages in presenting the upper comparisons, we found that each dataset had its own OHC in the SCS.展开更多
文摘南海北部航次观测资料显示南海北部表层盐度在2004—2012年期间缓慢降低,2012年盐度达到最低。客观分析数据EN4(the UK Met Office EN.4.0.2 objective analyses)以及OFES(ocean general circulation model for the Earth Simulator)模式结果都显示南海表层海水盐度在1993—2014年有淡化趋势,最显著区域位于吕宋岛以西和南海南部。盐度收支分析表明淡水强迫在吕宋岛以西海域起主要贡献,而水平平流输运主导南海西部的表层盐度变化。吕宋岛以西表层盐度的降低与近年来沃克环流加强引起的夏季强降雨增加有关。
文摘短毛五加总甙(AGVPS)是中药短毛五加(Acanthopanax gracilistylus var. pubescens)的有效成份。本文发现短毛五加总甙能抑制正常家兔由多种诱导因素所致的血小板聚集。同时,它还抑制花生四稀酸所致血小板聚集时TXA_2的产生,增加离体家兔胸主动脉PGI_2产生。在高脂喂养的动脉粥样硬化的家兔模型上,能提高血浆PGI_2水平。
文摘基于2004—2018年Argo(Array for Real-Time Geostrophic Oceanography)浮标观测的温度、盐度数据,利用经验正交函数(EOF)分析和小波分析等方法对北印度洋(40°—105°E,5°S—25°N)障碍层时空分布特征进行分析。结果显示:北印度洋的东部常年存在障碍层,而西部障碍层出现的概率相对较低;较厚的障碍层出现在阿拉伯海东南部(67°—75°E,3°—12°N)、孟加拉湾(82°—93°E,11°—20°N)和赤道东印度洋(81°—102°E,4°S—3°N)。阿拉伯海东南部和孟加拉湾障碍层厚度以年变化为主,且呈同位相变化,均为冬季最大,夏季最小。赤道东印度洋区域则主要呈现半年周期变化,在夏季和冬季各出现一次峰值。进一步分析表明,孟加拉湾和赤道东印度洋障碍层厚度主要受等温层深度变化影响,混合层深度变化对障碍层厚度变化的影响相对较小;阿拉伯海障碍层厚度同时受等温层深度变化和混合层深度变化影响,其中等温层深度变化对其影响更大。
基金supported by the National Basic Research Program of China (Grant Nos. 2010CB950400 and 2013CB430301)the National Natural Science Foundation of China (Grant Nos. 41276025 and 41176023)+2 种基金the R&D Special Fund for Public Welfare Industry (Meteorology) (Grant No. GYHY201106036)The OFES simulation was conducted on the Earth Simulator under the support of JAMSTECsupported by the Data Sharing Infrastructure of Earth System Science-Data Sharing Service Center of the South China Sea and adjacent regions
文摘In this study, the upper ocean heat content （OHC） variations in the South China Sea （SCS） during 1993- 2006 were investigated by examining ocean temperatures in seven datasets, including World Ocean Atlas 2009 （WOA09） （climatology）, Ishii datasets, Ocean General Circulation ModeI for the Earth Simulator （OFES）, Simple Ocean Data Assimilation system （SODA）, Global Ocean Data Assimilation System （GODAS）, China Oceanic ReAnalysis system （CORA） , and an ocean reanalysis dataset for the joining area of Asia and Indian-Pacific Ocean （AIPO1.0）. Among these datasets, two were independent of any numerical model, four relied on data assimilation, and one was generated without any data assimilation. The annual cycles revealed by the seven datasets were similar, but the interannual variations were different. Vertical structures of temperatures along the 18~N, 12.75~N, and 120~E sections were compared with data collected during open cruises in 1998 and 2005-08. The results indicated that Ishii, OFES, CORA, and AIPO1.0 were more consistent with the observations. Through systematic shortcomings and advantages in presenting the upper comparisons, we found that each dataset had its own OHC in the SCS.
