根据1998-2004年8～10月中国大陆西北太平洋柔鱼生产数据,结合对柔鱼渔场与各水层水温的分析,以作业次数为基础建立各水层水温的适应性指数(Suitability Index,SI)模型,采用算术平均法(Arithmetic Mean Model,AMM)和几何平均法(Geometri...根据1998-2004年8～10月中国大陆西北太平洋柔鱼生产数据,结合对柔鱼渔场与各水层水温的分析,以作业次数为基础建立各水层水温的适应性指数(Suitability Index,SI)模型,采用算术平均法(Arithmetic Mean Model,AMM)和几何平均法(Geometric Mean Model,GMM)建立综合栖息地指数(Habitat Suitability Index,HSI)模型;并对1998—2004年8～10月的HSI值与实际作业次数、产量和单船日产量(CPUE)作比较。结果表明,8～10月,HSI>0.6时,AMM的产量和作业次数比重分别占83.4%和80.9%,CPUE均2.1t/d以上;GMM的产量和作业次数比重分别占73.5%和69.6%,CPUE均2.3t/d以上。2种模型比较认为,AMM模型稍优于GMM模型。同时,利用2005年8～10月生产数据及水温资料对HSI模型进行验证。结果表明,基于水温垂直结构的栖息地指数模型能较好地预测西北太平洋中心渔场和潜在渔场。展开更多
Dissolved and particulate 234 Th, particulate organic carbon(PON), nitrogen, and chlorophyll-a concentrations in the upper 200 m of water columns from seven stations in the northwestern North Pacific Ocean were determ...Dissolved and particulate 234 Th, particulate organic carbon(PON), nitrogen, and chlorophyll-a concentrations in the upper 200 m of water columns from seven stations in the northwestern North Pacific Ocean were determined in the winter of 1997.The dissolved, particulate, and total 234 Th activities (dissolved plus particulate)show a pronounced deficiency with respect to its parent 238 U in the euphotic zone whereas the total 234 Th shows a near-equilibrium at the depth greater than 100 m.The 234 Th data are used to derive the mean residence time, export fluxes of 234 Th, and fluxes of particulate organic carbon and nitrogen out of the euphotic zone. In the Subarctic Current area, the residence time of dissolved 234 Th with respect to its removal onto particles is 40 ~50 d while the residence time of dissolved 234Th in the subtropical area is about 20 d due to the Kuroshio's influence.The particulate organic carbon(POC)and particulate organic nitroge(PON)fluxes in winter range over 3.8～8.2 and 0.50～0.98 mmol/(m2 ·d), respectively, and are higher in the west region than in the east, and higher in the south than in the north. The co-influence of Kuroshio-Oyashio Currents with supply of nutrient substances from the coastal area and the light condition are two factors determining the horizontal distribution of POC fluxes in winter.The depth distribution of the chlorophyll-a as well as the consistence of the ratio of POC to PON with the Redfield ratio suggest that phytoplankton is the main contributor to the export of POC in this area in winter.The POC fluxes in the northwestern North Pacific Ocean in winter are comparable to some areas in the world oceans in spring and summer seasons.展开更多
文摘根据1998-2004年8～10月中国大陆西北太平洋柔鱼生产数据,结合对柔鱼渔场与各水层水温的分析,以作业次数为基础建立各水层水温的适应性指数(Suitability Index,SI)模型,采用算术平均法(Arithmetic Mean Model,AMM)和几何平均法(Geometric Mean Model,GMM)建立综合栖息地指数(Habitat Suitability Index,HSI)模型;并对1998—2004年8～10月的HSI值与实际作业次数、产量和单船日产量(CPUE)作比较。结果表明,8～10月,HSI>0.6时,AMM的产量和作业次数比重分别占83.4%和80.9%,CPUE均2.1t/d以上;GMM的产量和作业次数比重分别占73.5%和69.6%,CPUE均2.3t/d以上。2种模型比较认为,AMM模型稍优于GMM模型。同时,利用2005年8～10月生产数据及水温资料对HSI模型进行验证。结果表明,基于水温垂直结构的栖息地指数模型能较好地预测西北太平洋中心渔场和潜在渔场。
基金the National Natural Science Foundation ofChina under contract No.40173027.
文摘Dissolved and particulate 234 Th, particulate organic carbon(PON), nitrogen, and chlorophyll-a concentrations in the upper 200 m of water columns from seven stations in the northwestern North Pacific Ocean were determined in the winter of 1997.The dissolved, particulate, and total 234 Th activities (dissolved plus particulate)show a pronounced deficiency with respect to its parent 238 U in the euphotic zone whereas the total 234 Th shows a near-equilibrium at the depth greater than 100 m.The 234 Th data are used to derive the mean residence time, export fluxes of 234 Th, and fluxes of particulate organic carbon and nitrogen out of the euphotic zone. In the Subarctic Current area, the residence time of dissolved 234 Th with respect to its removal onto particles is 40 ~50 d while the residence time of dissolved 234Th in the subtropical area is about 20 d due to the Kuroshio's influence.The particulate organic carbon(POC)and particulate organic nitroge(PON)fluxes in winter range over 3.8～8.2 and 0.50～0.98 mmol/(m2 ·d), respectively, and are higher in the west region than in the east, and higher in the south than in the north. The co-influence of Kuroshio-Oyashio Currents with supply of nutrient substances from the coastal area and the light condition are two factors determining the horizontal distribution of POC fluxes in winter.The depth distribution of the chlorophyll-a as well as the consistence of the ratio of POC to PON with the Redfield ratio suggest that phytoplankton is the main contributor to the export of POC in this area in winter.The POC fluxes in the northwestern North Pacific Ocean in winter are comparable to some areas in the world oceans in spring and summer seasons.
