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The results showed that there were 19 species in the catches, the main species included skipjack tuna, yellowfin tuna and bigeye tuna, in which skipjack tuna, yellowfin tuna and other fishes accounted for 70.51%, 26.92% and 2.56% in the catc...

中西太平洋太平洋金枪鱼的主要产区之一,世界主要金枪鱼的产量有 60~ 70 %来自太平洋水域[1 ] ,而这其中有 76%来自中西太平洋[2 ] 。中西太平洋金枪鱼渔业是一个多样性的渔业,作业方式包括围网、竿

Stationary and nonstationsary coupled oscillation regions are located over the western and eastern Pacific, respectively Thus, the interdacadal variations for intensity and period of these coupled interannual oscillations are closely related to PDO

西太平洋地区海温的耦合振荡作用区域是时间稳定的,而东太平洋地区海温的耦合振荡作用区域存在时变性因此PDO对夏季江淮地区降水和太平洋海温年际藕合振荡的强度和周期的年代际变化有重要影响。

During the PDO warm phase, however, there is a significant tropospheric biennial oscillation for the coupled interannual oscillations over these regions In addition , it seems to have a stronger correlation with the SST of the tropical eastern Pacific summer.

结果表明PDO冷暖位相中夏季江淮地区降水量与太平洋海温年际耦合振荡周期和强度均存在显著差异PDO冷位相中,夏季江淮地区降水与前期冬季西南太平洋和同期夏季黑潮区海温在7~8a时间尺度上的耦合最显著,而在PDO暖位相中,与这些地区海温呈现极显著的准2a耦合振荡,并且与同期夏季赤道东太平洋地区海温的准2a耦合振荡也迅速加强。

The lag correlation indicates that the eastern Pacific SST in winter correlates with the WPSH anomaly two or three months later to the highest degree; the SST in the tropical Indian Ocean and the WPSH anomaly in the corresponding period significantly correlates with each other in winter; and the SST in the western Pacific in winter and spring negatively correlates to the WPSH anomaly in the corresponding period.

选取各关键海区分析海温与西太副高在不同时段上的超前滞后相关,结果表明,冬季东太平洋海温与滞后其2—3个月的副高异常达最大正相关,热带印度洋海温异常与冬季同期副高异常的正相关最显著;西太平洋海温在冬春季与同期的副高负相关最显著;北太平洋海温在冬春季滞后副高1—2个月时存在负相关,大西洋暖池区6月与西太副高的同期正相关最大;对南太平洋来说,冬季的西太副高与从前秋到春季的SST都存在最大负相关。

On the other hand, when the tropical western Pacific is in a cooling state in spring, convective activities are weakened around the Philippines. In this case, there is an anticyclonic anomaly circulation in the lower troposphere over the South China Sea, and the western Pacific subtropical high shifts westward, thus, the late onset of the SCSM can be caused. Moreover, when the tropical western Pacific is also in a cooling state, convective activities around the Philippines are also weak in summer, since the abrupt northward-shift of the western Pacific subtropical high is not obvious in mid-June and early July and it gradually shifts northward during its northward advance in this case, the East Asian summer monsoon rainband can be maintained in the Yangtze River and the Huaihe River valleys.

相反,当春季热带西太平洋处于冷状态,菲律宾周围对流活动弱,在这种情况下,南海上空对流层下层有反气旋性距平环流,西太平洋副热带高压偏西,从而使得南海夏季风爆发晚;并且,当夏季热带西太平洋也处于冷状态,菲律宾周围对流活动也很弱,在这种情况下,西太平洋副热带高压北进时,在6月中旬或7月初向北突跳并不明显,而是以渐进式向北移动,从而使得东亚季风雨带一直维持在长江流域和淮河流域。

The results show that when the tropical western Pacific is in a warming state in spring, convective activities are intensified around the Philippines. In this case, there is a cyclonic anomaly circulation in the lower troposphere over the South China Sea, and the western Pacific subtropical high shifts eastward, thus, the early onset of the South China Sea summer monsoon can be caused. Moreover, when the tropical western Pacific is also in a warming state, convective activities around the Philippines are also strong in summer, since the western Pacific subtropical high abruptly shifts northward in mid-June and early July during its northward advance in this case, the abrupt northward-shift of the East Asian summer monsoon rainband from South China to the Yangtze River and the Huaihe River valleys is obvious in mid-June and this monsoon rainband again jumps northward from the Yangtze River and the Huaihe River valleys to the Yellow River valley, North China and Northeast China in early July.

分析结果表明:当春季热带西太平洋处于暖状态,菲律宾周围对流活动强,在这种情况下,南海上空对流层下层有气旋性距平环流,西太平洋副热带高压偏东,从而使得南海夏季风爆发早;并且,当夏季热带西太平洋也处于暖状态,菲律宾周围对流活动也很强,在这种情况下,西太平洋副热带高压北进时,在6月中旬和7月初存在明显的突跳,从而使得东亚季风雨带在6月中旬明显由华南北跳到江淮流域,并于7月初由江淮流域北跳到黄河流域、华北和东北地区。

Evidence suggests that when northern snow forced teleconnection is generated in this season, anomalous zonal/meridional circulations are revealed in east Asia-western Pacific band; with east Asia-Pacific teleconnection formed, anomalous zonal circulation is dominant over that band; the anomalous vortex of north Pacific origin moves southwestward and, r...

研究发现当北半球夏季出现积雪强迫型遥相关时,东亚-西太平洋地区既存在异常纬向环流,也存在异常经向环流;而当出现东亚太平洋型遥相关时,东亚-西太平洋地区以异常纬向环流为主。分析还发现源于北太平洋的异常涡旋在向南传播的过程中,先取西南路径,在到达菲律宾东部以后折向东南。

Land-sea heating, monsoon circulation, eastern Pacific trade wind and the slow seasonal shift of NE Pacific SST form winter to summer bihemispherically- all in joint action give rise to the enhancement of the Walker circulation that will travel east-and northward (west-and southward); the intensification of the maintained eastern Pacific Hadley circulation and north America-Alatantic Walker circulation zonally is responsible dominantly for the zonal/meridional movement of the WPSH in the winter-to-summer (or summer-to-winter) shift and its combination with the north American subtropical high.

海陆加热、季风环流、东太平洋信风以及东北太平洋海表温度由冬向夏关于赤道南北季节转换的迟缓性等综合作用导致的纬向Walker环流的加强东移和北抬、持续的东太平洋Hadley环流和北美—大西洋纬向Walker环流的加强是西太平洋副高由冬向夏产生东西、南北移动及其与北美副高合并的主要原因。

China Pacific Insurance Company was incorporated in Shanghai on April 26, 1991 as the first nationwide joint stock commercial insurance company in China.Approved by the State Administration for Industry and Commerce, the company was renamed "China Pacific Insurance Co., Ltd" on October 24, 2001 and divided into two controlled divisions, China Pacific Property Insurance Co., Ltd and China Pacific Life Insurance Co., Ltd. With more than 1100 branches and offices in major cities across China, the two divisions have formed well-established insurance service networks. Besides, the new company invested in setting up China Pacific Services Inc in the US, China Pacific Insurance H.K.

中国太平洋保险公司1991年4月26日在上海正式开业,是中国第一家全国性的股份制商业保险公司。2001年10月24日经国家工商行政管理总局批准,公司正式更名为&中国太平洋保险股份有限公司&,公司在国内控股投资设立中国太平洋财产保险股份有限公司和中国太平洋人寿保险股份有限公司,产、寿险公司在国内主要城市设有1100多个分支机构,拥有较为完善的保险服务网络。

Corresponding to the long-lasting El Nio event, cyclonic anomalous circulation over the eastern North Pacific weakens slowly and anticyclonic anomalous circulation over the western North Pacific strengthens slowly at 850 hPa. Therefore the tropical Pacific westerly anomaly keeps long. The anomalous positive velocity potential over the western South Pacific at 200 hPa, which is related to the strong Australian winter monsoon, helps a long duration of El Nio. Corresponding to the short-lasting El Nio, the anomalous positive velocity potential over the western Pacific at 200 hPa moves eastward quickly and results in the vanishing of El Nio event.

还发现对于持续时间较长的El Nio事件,东北太平洋上850hPa异常气旋性环流减弱和西北太平洋上异常反气旋性环流增强较慢,因此赤道太平洋异常西风维持的时间也较长,而与澳大利亚冬季风加强相关联的南半球西太平洋的速度势正距平的维持,对El Nio的持续也起一定作用;对应持续时间较短的El Nio事件,西太平洋上200hPa速度势正距平的迅速东移,对El Nio的迅速消亡起重要作用。

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