kuroshio

kuroshio

1. 7 He Dehua, Yang Guanming, Wang Chunsheng, 1994.Distribution of indicative copepods in the Kuroshio area of the East China Sea[J].

10王春生、何德华、刘镇盛,2003.象山港浮游动物生物量和丰度的季节变动[J].水产学报(待刊)[C]。

2. THE KUROSHIO IN LUZON STRAIT AND ITS TRANSPORT DURING SEPTEMBER 1985

1985年9月的吕宋海峡黑潮及其输送

3. The Kuroshio East of Taiwan Island and in the East China Sea in the Winter of 1997

1997年冬季台湾岛以东与东海黑潮

4. Kuroshio in the East China Sea in 2000

2000年东海黑潮

5. 3) There is an offshore branch of the Taiwan Warm Current in the west side of the Kuroshio, and it makes a cyclonic meander, then flows northeastward.

3)黑潮西侧有一台湾暖流外侧分支 ,先作气旋式弯曲 ,尔后向东北方向流动 .

6. Observations of Argos satellite-tracked drifters in the Kuroshio area

Argos表面漂流浮标在黑潮区的若干观测结果

7. CI-30 Doppler Current Meter and Its Application in The Kuroshio Survey

CI-30型多普勒声纳海流计及其在黑潮调查中的应用

8. Relationship between Evolution of Wind Stress Anomalies in the Kuroshio Region and ENSO

ENSO对黑潮海区风应力异常影响的初步探讨

9. RUAN Xue-qin,MA Fu-hui.Solar activity,sea temperature in the Kuroshio region and the flood and drought in the middle reach of the Yangtze River[J].Chinese J of Space Science,1995,15(4):326-332.

[6]阮雪琴,马福慧.太阳活动、黑潮海温年季变化与长江中游旱涝灾害[J].空间科学学报,1995,15(4):326-332.

10. A PRELIMINARY ANALYSIS OF THE VARIATION OF SURFACE VELOCITY OF THE KUROSHIO ON SECTION J IN THE EAST CHINA SEA

东海J断面上黑潮表层流速变化的初步分析

11. East China Sea Kuroshio

东海黑潮

12. kuroshio upper circulation in the ECS

东海黑潮上层环流

13. EDDY ENERGY TRANSPORT OF WAVE CYCLONES OVER KUROSHIO AREA

东海黑潮上空气旋波的扰动能量传输

14. main part of the Kuroshio

东海黑潮主段

15. Study on Circulation Substructure in the Main Part of the Kuroshio in the East China Sea

东海黑潮主段环流子结构研究

16. LOW FREQUENCY VARIATION OF THE SEA LEVEL IN THE KUROSHIO REGION OF THE EAST CHINA SEA

东海黑潮区域水位的低频变化

17. SOME RESULTS FROM THE STUDY OF THE VARIATION OF THE KUROSHIO IN THE EAST CHINA SEA

东海黑潮变异研究的若干结果

18. Kuroshio Frontal Eddy,Warm Filament and Warm Ring in the East China Sea

东海黑潮锋面涡、暖丝和暖环

19. DISTRIBUTION OF ZOOPLANKTON IN THE FRONTAL EDDY REGION OF THE KUROSHIO IN THE EAST CHINA SEA

东海黑潮锋面涡旋区浮游动物的分布

20. Numerical study on the Kuroshio path states in the northern Okinawa Trough of the East China Sea

中国东海冲绳北部槽中黑潮路径状况的数值研究

21. The water masses in the Taiwan Strait (TS) contain the Kuroshio Branch Water (KBW), the South China Sea Surface Water (SCSSW), and the China Coastal Water (CCW).

中文摘要台湾海峡受黑潮分支水、南海北部表层水和大陆沿岸水的影响，加上东亚季风的变化以及地形所控制，使得水团呈现复杂的季节变化。

22. There is a high salinity signal in the seas outside of Hsin-Chu, suggesting sea water coming from the Kuroshio, which has circumvented the northeast tip of Taiwan.

中文摘要圣婴现象对全球气候变迁所造成的影响是当今重要的议题，但是其对台湾气候的影响尚不明显，更难以厘清其与海洋或大气之间的关系，因此值得我们进一步研究。

23. The results show that this model can reasonable reproduce the equatorial currents, the Kuroshio Current, the Gulf Stream and the other main currents in global ocean.

从模拟结果看该模式具有较好的模拟能力，可以合理地模拟南极绕极流、赤道流系、黑潮和湾流等世界各主要大洋流系。

24. Part of the electricity board to maintain the Kuroshio family-style, high-quality solid capacitors inductors with 4 + closed loop design to the 45nm processor to play a broader space.

供电部分主板保持了黑潮家族的风格，高品质固态电容+封闭电感配以4相回路设计给了45nm处理器广阔的发挥空间。

25. South China Sea;Kuroshio;picophytoplankton;Trichodesmium;diazotrophs;nitrogen fixation,;new production;primary production

关键词:南海;黑潮;超微浮游植物;束毛藻;固氮生物;固氮作用;新生产力;基础生产力

26. Key words: Quaternary, paleoceanography, Okinawa Trough, Kuroshio, sedimentation

关键词:第四纪,古海洋,冲绳海槽,黑潮,积

27. Colloid;Kuroshio;South China Sea;Okinawa Trough;Carbohydrate;Amino Acid;Trace Element

关键词:胶体;黑潮;南海;冲绳海槽;碳水化合物;氨基酸;腐植酸;微量元素

28. Kuroshio;Intrusion;South China Sea;Counter current;cyclonic circulation

关键词:黑潮;入侵;南海;反流;低压环流

29. Kuroshio;Intrusion;Luzon Strait;South China Sea;Counter currents;cyclonic flow pattern

关键词:黑潮;入侵;吕宋海峡;南海;反流;低压环流

30. Keywords Cu;ACuCC;the East China Sea;Kuroshio;

关键词铜;表观络合容量;海水;东海黑潮;

31. Kuroshio intrusion engenders an eddy at the west of Kyushu Island of Japan.

冬季日本九州西侧海域存在一个半封闭的涡旋。

32. During the winter, the Kuroshio oceanic current brings warm water of high salinity from the Pacific through the Luzon Strait.

冬季期间，黑潮海流把高咸度的温暖海水由太平洋经吕宋海峡带入本港。

33. Numerical Simulation of the Influence of Successively Anomalous Winter Wind Field on Ocean Currents around the Kuroshio Area

冬季风风场持续异常对黑潮流域影响的数值模拟

34. Numerical Simulations on the Influence of the Previous Winter Kuroshio SSTA on East Asian Summer Monsoon

冬季黑潮SSTA影响东亚夏季风的数值试验

35. IMPACTS OF KUROSHIO SSTA ON STORM TRACK OVER NORTH PACIFIC IN WINTER

冬季黑潮区域海温异常对北太平洋风暴轴的影响

36. Keywords Okinawa Trough;Paleoclimate event;Kuroshio Current;Terrestrial organic material;Paleo-productivity;

冲绳海槽;气候事件;黑潮;陆源有机质;古生产力;

37. SEDIMENTARY DIATOM RECORDS ON EXCURSION OF KUROSHIO CURRENT IN OKINAWA TROUGH SINCE LAST GLACIATION

冲绳海槽末次冰期以来黑潮流游移在沉积硅藻中的记录

38. The wind variation, wavelike meander of Kuroshio and Taiwan Warm Current and instantaneous eddy, atmospheric pressure vibration are mainly factors for the low frequency current variation.

初步得出:风的变化、强流弯曲和瞬时涡旋是低频流变化的机制,而在半封闭海区低频流的变化同海面气压振荡有关。

39. Based on the CTD data collected on PN section in the East China Sea during March of 2001, the numerical simulation method is used to study the effect of sea-bottom undulation on sound propagation on PN section in the Kuroshio area.

利用2001年3月东海PN断面"973"调查获得的CTD数据,用数值模拟方法研究了PN断面黑潮区域海底起伏对声传播的影响。

40. THE INTERPRETATION ON THE SURFACE TEMPERATURE FRONTS OF KUROSHIO IN THE EAST CHINA SEA USING NOAA IR DATA

利用诺阿卫星红外信息对东海黑潮表层温度锋的解译

41. The Intraseasonal Long Rossby Wave in the Subtropical Ocean and Its Effect to the Kuroshio in the East China Sea

副热带海区季节内Rossby长波及其对东海黑潮的影响

42. While the main material sources of the central and western parts of the southern Yellow Sea are of matter from the Yellow River some are of deep-Sea materials transported by the Kuroshio system.

南黄海中、西部主要物质来源为黄河输送的物质,但该区域也不排除来自于黑潮系统所带来的远洋物质。

43. A SIMPLE MODEL FOR THE THERMAL STRUCTURE OF KUROSHIO EAST OF TAIWAN

台湾以东海域黑潮热结构的一个简单模型

44. Kuroshio transport

台湾以东黑潮流量

45. The northeast of the Taiwan Island is due to the Kuroshio and its topography.

台湾岛东北海域内潮响应强烈主要是受黑潮锋和地形的影响。

46. Tsushima Warm Current derives from several sources, includes a branch of Kuroshio, part of Taiwan Warm Current and Yellow Sea mixed water coming from the west of Cheju Island.

台湾暖流来自台湾海峡水与黑潮入侵的混合。对马暖流具有多源性，主要源自黑潮分支和台湾暖流以及黄海陆架水。

47. The numerical experiment reconstructed fairly successfully the circulation patterns of the Kuroshio, the Taiwan Warm Current, the Tsushima Warm Current and coast currents.

各因素共同作用下的黄海东海总流场数值模拟中，模式较好的再现了黑潮、台湾暖流、对马暖流、黄海暖流和沿岸流等各环流流系。

48. In the northeastern shelf or in the East China Sea, the Kuroshio intrudes northward in the form of branches in winter, and enters into the shelf from the north as a continental margin current.

在东海东北部陆架海域，冬季黑潮以其分支形式向北入侵，夏季则主要以大陆边缘流的形式向北进入陆架。

49. In the southeast of the South China Sea, there maybe existed the water from the Sulu Sea, and its temperature and salinity characteristics were similar to that of the Kuroshio water near the Luzon Strait.

在南海东南部可能有来自苏禄海的海水 ,其温、盐度特征类似于吕宋海峡中的黑潮水

50. Effects of Topography on Kuroshio Frontal Meanders in the East China Sea

地形对东海黑潮锋面弯曲影响研究

51. The water in the west side of Tsushima Warm Current is a mixed water of East China Sea and the water in its east side is a branch water coming from the Kuroshio.

对马暖流西侧的水体是东海混合水,而其东侧为黑潮分支。

52. BRANCHINGS OF KUROSHIO INTO BASHI CHANNEL AND THE SOUTH CHINA SEA

巴士海峡和南海东北部黑潮分支

53. VARIATIONS OF VELOCITY AND TRANSPORT OF THE KUROSHIO IN THE BASHI CHANNEL

巴士海峡黑潮流速和流量的变化

54. 5 grid, the three-dimensional current system in the Kuroshio south of Japan and Kuroshio Extension is determined and analyzed by using the P-vector method.

应用P矢量方法对日本以南黑潮和黑潮延续体三维流场进行了诊断计算和分析研究。

55. This study compares the taxa distribution and biochemical composition of zooplankton from stations in coastal upwelling caused by the intrusion of the Kuroshio Current into the East China Sea shelf.

摘要本研究探讨台湾东北海域由黑潮入侵大陆棚所引发的涌升流及其附近区域浮游动物之大类分布与其生化组成。

56. Japan is the island and affected by the Kuroshio Ocean significantly.

日本是岛国，又深受黑潮影响，海洋性显著。

57. Spring Kuroshio SST

春季黑潮区域海温

58. It is not clear whether Kuroshio plays a role and further investigation is needed.

是否与黑潮有关，目前仍不清楚， 尚待研究。

59. Annual Variation of the Kuroshio Transport in a Two-Layer Numerical Model with a Ridge

有脊的两层数值模式黑潮输送的年度变化

60. The mean abundance, but not for species number, of siphonophores was significantly higher in Kuroshio waters than in coastal waters.

本海域黑潮水团之平均丰度显著高于沿岸水团；

61. Sound speed and current velocity of the Kuroshio at the PN section hi East ChinaSea are inverted by using the least square method and singular value decompositiontechnique.

本论文在东海PN断面黑潮区域用最小二乘法结合奇异值分解技术反演了声速和海流，由于声速与温度的近似线性关系，可以很容易的得到温度分布，结合流速，计算黑潮的热输运。

62. The intrusion of Kuroshio water from the Luzon Strait into the northern South China Sea is the possible source of water mass for this phenomenon.

此一南向流应是与黑潮入侵水在台湾西南海域形成顺时针旋转的反气旋式涡流有关。

63. Observation of frontal waves and associated salinity minimum formation along the Kuroshio Extension

沿黑潮流锋面波和相伴的盐最小形成的观测

64. THE EFFECTS OF VARIATION FOR FLOW CORE POSITION AND FLUX ON KUROSHIO FRONTAL MEANDERS IN THE EAST CHINA SEA

流核位置和流量变化对东海黑潮锋面弯曲影响的研究

65. Taiwan is located at the crossing point between the cold water continental current and the warm water Kuroshio current.

海鲜的种类分布主要受沿岸底质与洋流温度影响。

66. Kuroshio source area

源地黑潮

67. The distributions of tropic oceanic lower-temperature and high-saline species in the shelf area can indicate the scope of invading and upwelling of the Kuroshio subsurface water.

热带大洋高盐偏低温类群种类在陆架区的分布状况可反映黑潮次表层水的入侵涌升范围;

68. This may be attributed to the seasonal intrusion of the Kuroshio Current to the study water.Nitrogen was a better tracer than carbon in investigating trophic relationships of marine organisms.

生物体内同位素含量的季节性差异表现在体 型较小的浮游生物内，春、夏差异不明显而分别与秋季有显著差异，可能与黑潮的季节 性消长有关。

69. The results show that:(1) on the scale of seasonal variation,the transports of Mindanao Current and Kuroshio have inverse trends;

由此得出以下结论 :( 1 )棉兰老海流对北赤道逆流的初始流量贡献较大 ,是北赤道逆流的主要水源提供者之一 ,棉兰老海流与黑潮在季节变化中存在反相关系 ;

70. Characteristics of the Kuroshio Frontal Eddy in the East China Sea in Autumn

秋季东海黑潮锋面涡旋的特点

71. Tensyu, Blank Olympia, Beniizu, Shina bailey, Kuroshio, Zi Zhenxiang, Campbell Early, Maciji, Honey Red, Ikawa 1014, Ikawa 1025, Benizuiho, Jingya and so on (13 varieties) formed eighth group;

第八类:天秀、黑奥林、京亚、露都蓓蕾、黑潮、紫珍香、康拜尔早生、?莉、红蜜、井川1014、红瑞宝等13 个品种,它们是巨峰系的欧美杂交种。

72. [2]GUAN B X.Effects of bottom topography in the Taiwan and adjacent area on the path of the Kuroshio[J].Studia Marina Sinica,1978,14:1-23.

管秉贤.我国台湾及其附近海底地形对黑潮途径的影响[J].海洋科学集刊,1978,14:1-23.

73. The Kuroshio Current brings a huge variety of fish to Okinawa.

而黑潮洋流则给冲绳带来了品种繁多的鱼类。

74. Ye, L. (1994) On the mechanism of South China Sea Warm Current and Kuroshio Branch in winter - Preliminary results of 3-D baroclinic experiments.

苏纪兰、刘先炳（1992）南海环流的数值模拟。见：海洋环流研讨会论文选集，曾庆存，袁重光，赵剑平，余宙文等主编，海洋出版社，北京。

75. Though the Kuroshio Water was found to enter into the South China Sea passed through the Bashi Channel, its influence was weak.

虽发现有黑潮水穿越巴上海峡进入南海，但其势力甚弱。

76. The 10 Be concentrations in surface water increase gradually towards the kuroshi o and increase sharply at the edge of t he Kuroshio Current.

表层水10Be的浓度从长江口到黑潮逐渐增大,在黑潮的边缘则剧烈增大。

77. Keywords MOM2.O simulation Kuroshio Seasonal changes, Wind,,,, stress curl Warm eddy Yellow Sea Cold Water Mass Bottom,,,, boundary mixing Circulation of two layer structure

西北太平洋环流;季节变化;风应力涡度;琉球以东;海流;黄海冷水团;底边界混合;两层环流结构;

78. RELATIONSHIP BETWEEN KUROSHIO MEANDER PATTERN AND OMMASTREPHES BARTRAMI CPUE IN NORTHWEST PACIFIC OCEAN

西北太平洋黑潮路径变化与柔鱼CPUE的关系研究

79. The western sector, Kuroshio, mainly involves the subtropical gyre (STG) and the subtropical cell (STC), and the eastern sector mainly involves the anticyclonic gyre to the southeast of Japan which quickly recirculates.

西段(即黑潮)主要参与副热带环流(STG)和经向环流(STC); 东段主要参与日本东南的反气旋式涡旋再回流。

80. The cold water body results from the upwelling of subsurface Kuroshio water, which shows the influence of the Kuroshio on the Chinese marine environment.

该冷水块是黑潮次表层水涌升的结果,是黑潮对我国近海海洋环境影响的典型实例之一。