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中华绒螯蟹不同发育阶段腹肢粘液腺同工酶的比较 总被引:5,自引:0,他引:5
采用聚丙烯酰胺凝胶电泳方法对中华绒螯蟹不同发育阶段(幼蟹、未成熟蟹、成熟蟹及抱卵蟹)腹肢粘液腺的乳酸脱氢酶(LDH)、醇脱氢酶(ADH)、苹果酸脱氢酶(MDH)、过氧化物酶(POD)、酯酶(EST)及淀粉酶(AMY)等同工酶进行研究。结果表明不同发育阶段中华绒螯蟹腹肢粘液腺中,LDH同工酶的表达较稳定,均只有一条酶带,酶活性呈逐步减弱趋势,至抱卵蟹时活性又增强;ADH同工酶在不同发育阶段酶带数及酶活性也呈减少趋势,至抱卵蟹时又重新增加;MDH同工酶有m-MDH和s-MDH两种类型,其比值随发育阶段不同有一定变化;不同发育阶段POD同工酶活性均较弱;EST同工酶至抱卵蟹时酶带数最多,活性相对最强;AMY同工酶随不同发育阶段,酶带数及酶活性呈逐步复杂趋势。 相似文献
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Nudging资料同化对北极海冰密集度预报的改进 总被引:2,自引:2,他引:0
北极夏季海冰的快速减少使得北极航道提前开通成为可能。为了给北极冰区船运活动提供及时可靠有效的海冰预报保障,急需提高海冰预报水平。本文基于麻省理工大学通用环流模式(MITgcm),使用牛顿松弛逼近(Nudging)资料同化方法将德国不莱梅大学的第二代先进微波辐射成像仪(AMSR2)海冰密集度资料同化到模式中,建立了北极海冰数值预报系统。设计试验对比3种不同Nudging系数计算方案的改进效果,结果表明选择合适参数后,不同方案均能显著改进海冰密集度初始场。通过设计有无Nudging同化的两组预报试验,结合卫星遥感海冰密集度及中国第五次北极科学考察期间"雪龙"船的走航海冰密集度观测数据,定量分析了Nudging同化方案对北极海冰密集度的24~120 h预报结果的改进效果。结果表明,Nudging同化对120 h内全北极海冰密集度的空间分布和移动单点目标的海冰密集度预报结果均有显著改善;但在海冰变化很小的情况下,Nudging同化试验的24~120 h预报结果均劣于惯性预报结果,说明基于Nudging同化的数值预报系统还需进一步提高预报技巧。 相似文献
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引入拖曳系数参数化的海冰自由漂流模拟研究 总被引:2,自引:0,他引:2
Many interesting characteristics of sea ice drift depend on the atmospheric drag coefficient(C_a) and oceanic drag coefficient(C_w).Parameterizations of drag coefficients rather than constant values provide us a way to look insight into the dependence of these characteristics on sea ice conditions.In the present study,the parameterized ice drag coefficients are included into a free-drift sea ice dynamic model,and the wind factor α and the deflection angle θ between sea ice drift and wind velocity as well as the ratio of C_a to C_w are studied to investigate their dependence on the impact factors such as local drag coefficients,floe and ridge geometry.The results reveal that in an idealized steady ocean,C_a/C_w increases obviously with the increasing ice concentration for small ice floes in the marginal ice zone,while it remains at a steady level(0.2-0.25) for large floes in the central ice zone.The wind factor α increases rapidly at first and approaches a steady level of 0.018 when A is greater than 20%.And the deflection angle θ drops rapidly from an initial value of approximate 80° and decreases slowly as A is greater than20%without a steady level like α.The values of these parameters agree well with the previously reported observations in Arctic.The ridging intensity is an important parameter to determine the dominant contribution of the ratio of skin friction drag coefficient(C_s' /C_s) and the ratio of ridge form drag coefficient(C_r'/C_r) to the value of C_a/C_w,α,and θ,because of the dominance of ridge form drag for large ridging intensity and skin friction for small ridging intensity among the total drag forces.Parameterization of sea ice drag coefficients has the potential to be embedded into ice dynamic models to better account for the variability of sea ice in the transient Arctic Ocean. 相似文献
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