Members of the cfb ( cytophaga - flexibacter - bacteroides ) were found to be rich in upper sediment of " warm pool " while they were not detected in sediment from " manganese nodule " area , which indicated that there were more organic substances in the " warm pool " area 除了紫细菌之外， cfb类群在“暖池”区沉积物中也是一类较重要的细菌，主要集中在表层沉积物；而在“结核”区没有检测到属于cfb类群的细菌，表明“暖池”区表层存在较多的有机物。
But only for the closure of indonesia passage , warm pool can be formed under 150m with the center between 300m and 600m or so while in upper layer the modern sea temperature is still colder , so seen from the simulation , only the open of indonesia passage can not form the warm pool like the present P )模拟的海温要暖，形成浅层暖池。但单是上述通道关闭，暖池只形成在150米以下，中心在300 ? 600米深海洋层，而海洋上层( 150米以上)仍为现代冷。依数值模拟来看，只有上述通道的开启，并不能形成如现代浅层海洋暖池。
1 ) the centers of the strong olr mjo as found in the tropical indian ocean and the western pacific warm pool are observed in any one of the four seasons ; the mjo are stronger in the boreal winter and spring than in the boreal summer and autumn and move southward and northward with season ; high climatic sst is the conditions for strong olr mjo 得到如下主要结论： 1 )热带印度洋和热带西太平洋暖池区域是olr季内振荡高强度区；它们终年存在，北半球冬春季强、夏秋季弱，且随季节更替作南北向移动；气候高sst区是其存在条件。
Genetic analysis shows that it may be caused by the difference of the response of each area to winter monsoon ' s abnormal , the kuroshio and our offshore is influenced mostly by heat flux between the sea and atmosphere , but in the other areas , the abnormal current incited by abnormal wind has decisive effect on the change of the sea temperature , at the same time , air pressure also has some impact on the sea temperature 其区域性形成的原因主要可能是因为各海区对冬季风异常的响应方式不同，强冬季风使得黑潮与我国近海海洋过多散热，海温降低；在西北太平洋暖池北部，强冬季风引起西风异常，从而引发异常气旋性环流，海水辐合下沉加热其表层以下海水，同时异常环流使得更多东侧异常暖水向西加热其表层水；在黑潮与亲潮交汇处的升温也主要是由于强冬季风导致的流场异常，海水辐合下沉升温。
In this study , we investigate the microbial diversity of deep sea sediments and analyze the characteristic of substance and energy conversion driven by microorganism in " warm pool " area for the first time . samples including deep sea sediments of the pacific ocean and other environmental samples from polar region were collected and analyzed 本论文首次对“暖池”区海底沉积物中的微生物进行了分子生态学研究，分析了微生物多样性，对由微生物参与的物质能量循环特征进行了探讨，为研究深海生物圈在地球圈层相互作用中的地位提供了参考资料。
When the spatial pattern is of the north - south asymmetry , in the warm north - cold south years , there is a anticyclone circulation existing over the warm pool at 850hpa , easterly at 15 n and westerly in the tropical region have been greatly strengthened , while the center of anticyclone circulation moves to the east asia at 200hpa , and the hadley circulation has been affected evidently , so the summer rainfall may be above normal in the middle and lower reaches of the yangtze river , vice versa . there are different relations to east asia atmospheric circulation and summer rainfall in china 当ssta为南北半球反对称分布时，与ssta北暖南冷分布相对应， 850hpa暖池区上空为一反气旋偏差环流， 15 n附近东风气流和赤道附近西风气流增强，长江中下游地区盛行偏南风气流； 200hpa反气旋偏差环流中心移到东亚大陆上空；副热带高压强度、西伸脊点都明显变强、西伸； hadley环流得到发展，长江中下游(华北)地区为上升(下沉)气流，降水明显增多(减少) ，北冷南暖年则相反。
When the spatial pattern is uniform in the whole area , there is a better relations between the wp ssta and walker circulation , hadley circulation , enso and the summer rainfall of the upper and middle reaches of the yangtze river , while the spatial pattern is of the north - south asymmetry , there is a better relation between the wp ssta and hadley circulation and the summer rainfall of the middle and lower reaches of the yangtze river 暖池区ssta不同分布型与东亚大气环流和中国夏季降水关系不同， ssta的一致性分布与hadley 、 walker环流、 enso循环及长江中上游地区降水关系较好，而ssta南北反对称分布与hadley环流和长江中下游地区降水关系较好。
Results show that there are two main spatial patterns of the wp ssta : one is uniform in the whole area , the other is of the north - south asymmetry . when the spatial pattern is uniform in the whole area , in the warm years , there is a anticyclone circulation existing over the warm pool and westerly in the subtropical region and easterly in the tropical region have been greatly strengthened at 850hpa , while a anticyclone circulation over the india region at 200hpa , the walker circulation has been strengthened , the summer rainfall may be above normal in the upper and middle reaches of the yangtze river , vice versa 当ssta为一致性分布时，暖异常年， 850hpa暖池区上空为一反气旋偏差环流，副热带地区西风和低纬度地区东风得到加强，长江中上游地区盛行偏南风气流； 200hpa南亚上空为一反气旋偏差环流，长江中上游地区为北风； walker环流加强，副热带高压偏强，经向垂直环流在25 35 n附近为上升气流，长江中上游地区降水偏多，是lanina事件的多发年，对应的soi指数偏高，冷异常年则相反。
The topography and the physiognomy of the south china sea are very complex such as continental slop , continental shelves , seamounts , sea basin , etc . the south china sea lies between qingzang plateau , which is as the main driver of the variety of climate , and the western part of the pacific , which is called warm pool , and is influenced by some current systems , such as coastal current , kuroshi , etc . the south sea has considerable species 南海具有陆坡、陆架、海沟、海盆等复杂的地形、地貌；南海位于作为地球气候变化的主要驱动力的青藏高原和西太平洋暖池之间；南海受到沿岸流、南海暖流水、黑潮入侵水等流系的影响；南海具有丰富的物种分布；上述因素共同影响南海生源要素的分布、输送和迁移。
The difference of microbial group between different sea areas was the 8 - and e - subdivision of proteobacteria , which was abundant at upper sediment of " warm pool " area while they were not detected at the sediments of " manganese nodule " area . at the core sediment of " warm pool " area , members of - proteobacteria reduced from upper to lower sediments 在“结核”区沉积物中没有检测到属于这两个亚群的细菌，而在“暖池”区沉积物中属于这两个亚群的细菌数量较多(最高可达29 ) ，并且-亚群的细菌呈现随沉积物深度增加而减少的趋势。
