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991.
992.
993.
利用1993年ENSO事件爆发(4月)前酝酿时期“热带大洋与全球大气-海洋耦合响应试验”强化观测阶段“向阳红五号”科学考察船155°E,2°S定点海洋气象和高空大气探测资料,分析了赤道西太平洋大气边界层特征。结果表明:赤道西太平洋上空辐合对流区边界层内也有等温或逆温层存在,大气边界层物理参数变化与大尺度海-气变异有密切关系,赤道太平洋沃克环流加强、东移,边界层上部逆温层出现概率明显增大,边界层内高湿层湿度减小。另外,边界层内实测风速、风向廓线随高度的变化基本上不服从Ekman规律,但由其平均,分量合成得到的平均风随高度的变化却基本符合Ekman规律。 相似文献
994.
995.
996.
中国对虾血细胞及其免疫研究 总被引:54,自引:0,他引:54
于1991年3月-1992年4月青岛近海及一养虾场捕集中国对虾亲虾和越冬亲虾,以扫描电镜和透射电镜观察中国虾的血细胞形态及其亚显微结构;研究定量测定细胞吞噬活性的方法。结果表明,中国对虾血细胞分3种:无颗粒细胞,呈球形或梭形,胞质不含颗粒粒;小颗粒细胞及颗粒细胞,卵球形或椭球球形,胞质含有电子致密颗粒,颗粒可分均匀、非均匀的;小颗粒细胞质富含线粒体,可能与它对异物敏感易发生胞吐作用有关,该细胞是识 相似文献
997.
C. K. Paull W. Ussler H. G. Greene R. Keaten P. Mitts J. Barry 《Geo-Marine Letters》2003,22(4):227-232
A sediment gravity flow descended through the axis of Monterey Canyon on 20 December 2001 at 13:35 Pacific standard time.
The timing of this event is documented by a current-meter package which recorded an 11.9-dbar pressure increase in less than
10 min and was found 550 m down-canyon from its deployment site, buried completely within a >70-cm-thick gravity flow deposit.
This event is believed to have started in less than 290 m of water because an instrument at this location was also lost at
the same time. A 178-cm core collected after the event from the axis of the canyon at 1,297-m water depth contained fresh,
greenish, chlorophyll-rich organic material at 32-cm sub-bottom depth, suggesting the event extended to this water depth.
The only trigger identified for this mass movement event appears to be moderate sea and surf conditions. Thus, gravity flow
events of this magnitude do not require an exceptional triggering event. 相似文献
998.
Using benthic macrofauna to assess environmental quality of four intertidal mudflats in Hong Kong and Shenzhen Coast 总被引:4,自引:0,他引:4
Cai Lizhe Nora F. Y. Tam Teresa W. Y. Wong Ma Li Gao Yang Yuk-Shan Wong 《海洋学报(英文版)》2003,22(2):309-319
Abstract-Intertidal zone is a significant wetland between land and ocean. It plays an important rolein maintaining local ecological balance. Both Mai Po and Futian intertidal mudflats are located in Shen-zhen Bay and are important "refueling" point along the East Asian/Australian flyway of migratory birds.The environmental quality of Mai Po and Futian mudflats have aroused great concern due to rapid eco-nomic developments in Hong Kong and Shenzhen in recent decades. Microinfauna of Mai Po and Futianmudflats was investigated in December 2000 and the faunal data were used to assess their environmentalquality. Two other mudflats, namely Ma Wan Typhoon Shelter (a more disturbed area) and Luk Kengintertidal mudflat (a place with relatively less human disturbance), were also sampled for macroinfaunaand used as reference mudflats. Shannon-Weaver species diversity index (I_(sd)), biotic coefficient (C_b)and macrofaunal pollution index (I_(mp)) of the macrofauna community on four intertidal mudflats wereused to 相似文献
999.
1000.
C. K. Paull W. Ussler H. G. Greene R. Keaten P. Mitts J. Barry 《Geo-Marine Letters》2002,22(4):227-232
A sediment gravity flow descended through the axis of Monterey Canyon on 20 December 2001 at 13:35 Pacific standard time. The timing of this event is documented by a current-meter package which recorded an 11.9-dbar pressure increase in less than 10 min and was found 550 m down-canyon from its deployment site, buried completely within a >70-cm-thick gravity flow deposit. This event is believed to have started in less than 290 m of water because an instrument at this location was also lost at the same time. A 178-cm core collected after the event from the axis of the canyon at 1,297-m water depth contained fresh, greenish, chlorophyll-rich organic material at 32-cm sub-bottom depth, suggesting the event extended to this water depth. The only trigger identified for this mass movement event appears to be moderate sea and surf conditions. Thus, gravity flow events of this magnitude do not require an exceptional triggering event. 相似文献