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121.
介绍DSP芯片TMS320VC5402和24位A/D转换器ADS1251的性能、特点,设计由它们构成的海洋重力仪数据采集处理系统,给出DSP进行数据采集与处理以及与上位机通信的软硬件设计方法。同时,用Delphi实现视窗界面的处理结果的存储和曲线图形的显示、打印。 相似文献
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从敞口集装箱船的险情-安全措施分析出发,介绍了核定此类船舶载重线的要素,以及根据有限航区的特点,在国际海事组织《敞口集装箱暂行指南》对无限航区敞口集装箱船载重线核定要求的基础上,导出对有限航区敞口集装箱船的相应要求,提出了关于有限航区敞口集装箱船设计应考虑的若干问题。 相似文献
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西北太平洋,尤其是中国及其附近海域是船舶航行比较密集的区域,也是台风活动非常频繁的海域。成功避让台风不仅意味着保证船舶安全,还需要避免不合理绕航、滞航等带来的时间和经济损失。台风的活动是有一定的规律的,不断积累和交流在该区域内的避台经验对于驾驶员来说十分重要。介绍了几条具体航线上的避台措施,供船舶驾驶员参考。 相似文献
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Igor P. Semiletov Irina I. Pipko Irina Repina Natalia E. Shakhova 《Journal of Marine Systems》2007,66(1-4):204
Climatic changes in the Northern Hemisphere have led to remarkable environmental changes in the Arctic Ocean, which is surrounded by permafrost. These changes include significant shrinking of sea-ice cover in summer, increased time between sea-ice break-up and freeze-up, and Arctic surface water freshening and warming associated with melting sea-ice, thawing permafrost, and increased runoff. These changes are commonly attributed to the greenhouse effect resulting from increased atmospheric carbon dioxide (CO2) concentration and other non-CO2 radiatively active gases (methane, nitrous oxide). The greenhouse effect should be most pronounced in the Arctic where the largest air CO2 concentrations and winter–summer variations in the world for a clean background environment were detected. However, the air–land–shelf interaction in the Arctic has a substantial impact on the composition of the overlying atmosphere; as the permafrost thaws, a significant amount of old terrestrial carbon becomes available for biogeochemical cycling and oxidation to CO2. The Arctic Ocean's role in determining regional CO2 balance has been ignored, because of its small size (only 4% of the world ocean area) and because its continuous sea-ice cover is considered to impede gaseous exchange with the atmosphere so efficiently that no global climate models include CO2 exchange over sea-ice. In this paper we show that: (1) the Arctic shelf seas (the Laptev and East-Siberian seas) may become a strong source of atmospheric CO2 because of oxidation of bio-available eroded terrestrial carbon and river transport; (2) the Chukchi Sea shelf exhibits the strong uptake of atmospheric CO2; (3) the sea-ice melt ponds and open brine channels form an important spring/summer air CO2 sink that also must be included in any Arctic regional CO2 budget. Both the direction and amount of CO2 transfer between air and sea during open water season may be different from transfer during freezing and thawing, or during winter when CO2 accumulates beneath Arctic sea-ice; (4) direct measurements beneath the sea ice gave two initial results. First, a drastic pCO2 decrease from 410 μatm to 288 μatm, which was recorded in February–March beneath the fast ice near Barrow using the SAMI-CO2 sensor, may reflect increased photosynthetic activity beneath sea-ice just after polar sunrise. Second, new measurements made in summer 2005 beneath the sea ice in the Central Basin show relatively high values of pCO2 ranging between 425 μatm and 475 μatm, values, which are larger than the mean atmospheric value in the Arctic in summertime. The sources of those high values are supposed to be: high rates of bacterial respiration, import of the Upper Halocline Water (UHW) from the Chukchi Sea (CS) where values of pCO2 range between 400 and 600 μatm, a contribution from the Lena river plume, or any combination of these sources. 相似文献
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