台湾海峡西部毛颚类的生态研究

本文根据1984年5月-1985年2月在台湾海峡西部综合调查所获的浮游毛颚类样品,经分析共出现26种毛颚类,其中,尤以肥胖箭虫、百陶箭虫和拿卡箭虫最优势,本海区毛颚类虽周年可见,但以春、夏两季较多,尤其是夏季,其种类数和个体数皆居年的最高值,根据其分布特点,可分为近岸暖水性、近岸暖温性、广盐暖水和外海暖水等4个生态类群,其季节变化分布规律与沿岸水系、外海水系的消长和推移密切相关.     

极地低压对费拉姆海峡大西洋入流水天气尺度变化的影响

The Atlantic inflow in the Fram Strait(78°50′N) has synoptic scale variability based on an array of moorings over the period of 1998–2010. The synoptic scale variability of Atlantic inflow, whose significant cycle is 3–16 d, occurs mainly in winter and spring(from January to April) and is related with polar lows in the Barents Sea. On the synoptic scale, the enhancement(weakening) of Atlantic inflow in the Fram Strait is accompanied by less(more)polar lows in the Barents Sea. Wind stress curl induced by polar lows in the Barents Sea causes Ekman-transport,leads to decrease of sea surface height in the Barents Sea, due to geostrophic adjustment, further induces a cyclonic circulation anomaly around the Barents Sea, and causes the weakening of the Atlantic inflow in the Fram Strait. Our results highlight the importance of polar lows in forcing the Atlantic inflow in the Fram Strait and can help us to further understand the effect of Atlantic warm water on the change of the Arctic Ocean.     

台湾海峡西部海域水螅水母类和栉水母类的生态研究

本文根据采自台湾海峡西部海域4个季度月的169份浮游动物定量样品,分析了水螅水母类和栉水母类的种类组成、个体数的季节变化和平面分布,并着重就其与环境的关系做了探讨。结果表明,水螅水母和栉水母的个体数高峰出现在春季,分别为330个/100m³和157个/100m³所记录的67种水螅水母和栉水母根据其生态习性,大致可分为近岸暖温性、近岸暖水性、近岸狭暖水性、大洋广暖水性和大洋狭布性等5个生态类群。它们在调查海区的分布状况在一定程度上可反映出闽浙沿岸流,粤东沿岸流和外海暖流(南海暖流和黑潮支流)的动态。     

行星尺度阻塞波和天气尺度波相互作用的数值模拟

用数值方法研究了行星尺度阻塞波和天气尺度波之间的相互作用,得到在涡源强迫下,当不存在地形时,大尺度流场可发展成偶极型阻塞,瞬时流场分裂成南北对称的2支,总流场可以看到明显的多涡结构;加上双波地形后,大尺度流场发展成Ω型阻塞,瞬时流场同样分裂成2支,但北支要明显强于南支.而且通过一系列对比试验发现,适当的弱的基本西风气流是阻塞发生的有利条件.此外,讨论了初始阻塞和造波器（扰动源）位置的配置,以及造波器关闭时间的不同对阻塞强度和生命周期的可能影响.     

台湾海峡地区雾形成的天气类型分析

利用 1 980— 1 997年东亚逐日 0 8时地面天气图资料 ,归纳并分析了台湾海峡地区(2 0°— 2 7°N ,1 1 5°— 1 2 5°E)形成雾的 4种天气类型 ,它们分别是冷平流主导型、暖平流主导型、均压场型和台风外围型 ,为台湾海峡地区雾的预报提供天气学参考。     

温带爆发性气旋的天气尺度诊断分析

本文根据ＭＭ４模式输出资料，利用平衡模式的ω－方程对１９８３年４月２５－２６日的模式气旋作了诊断分析，结果显示，气旋爆发性剧烈发展，与大尺度加热，积云对流加热，温度平流，涡度平流等物理因子密切相关，其中以温度平流和非绝热热尤为重要。     

一次冷涡背景下次天气尺度系统对强对流环境场的影响

在同一东北冷涡背景下,2016年6月12—13日山西境内连续2 d出现强对流天气,12日为分散性对流而13日为大范围强对流。基于多源资料通过对比探讨次天气尺度系统及其演变对风暴环境进而对风暴结构的影响,得出以下结论：（1）两日风暴强度和风暴结构差异显著。6月12日对流孤立分散且回波强度小于55 dBZ,而13日准线性风暴发展成尺度较大的弓形回波引发大范围强对流天气,回波强度达60 dBZ。（2）此次过程的关键影响系统为冷涡背景下的次天气尺度低涡。12日次天气尺度低压扰动开始出现,距离远而未影响山西;13日低压扰动东移发展为次天气尺度切断低涡,低涡相关的地面冷锋及850 hPa切变线触发山西上游对流。（3）12日低层水汽含量低,0~3 km垂直风切变弱,13日低涡前偏南水汽输送使低层显著增湿,叠加中层干冷空气形成不稳定层结,受低涡影响0~3 km风垂直切变增强至5.0×10^-3 s^-1,冷锋触发的对流风暴在上述环境下强烈发展并产生阵风锋,阵风锋组织风暴形成飑线,冷池与0~3 km风切变相互作用使飑线维持。（4）13日有利于飑线发展的环境要素与东北冷涡西侧的次天气尺度切断低涡系统密切相关,次天气尺度低涡是飑线形成发展的关键系统。     

闽南—台湾浅滩渔场微型硅藻的分类研究

利用透射电镜（ＴＥＭ）研究闽南－台湾浅滩渔场的微型硅藻时,鉴定出１４个在我国首次的种类,它们是：极小曲壳藻（Ａｃｈｎａｎｔｈｅｓ ｍｉｎｕｔｉｓｓｉｍａ）,分岐双壁藻（Ｄｉｐｌｏｎｅｉｓ ｄｉｖｅｒｇｅｎｓ）、槌棒脆杆藻（Ｆｒａｇｉｌａｔｉａ ｏｐｅｐｈｏｒｏｉｄｅｓ）、微细脆杆藻（Ｆｒａｇｉｌａｒｉａ ａｔｏｍｕｓ）、折断舟形藻（Ｎａｖｉｃｕｌａ ｆｒａｃｔａ）、虫瘿舟形藻（Ｎａｖｉｃｕｌａｇａ     

背景西风对由局地天气尺度波所形成阻塞的影响

本文从理论上研究了在不同的背景西风条件下阻塞胚胎与局地天气尺度波之间的相互作用。结果发现合适的弱西风对阻塞的形成是至关重要的 ,较强的背景西风不利于阻塞的形成。同时局地天气尺度波的位置也起着重要作用。     

台湾海峡南部的海洋锋

通过近期水文观测,结合卫星遥感和历史水文资料,对台湾海峡南部海域的海洋锋现象进行了整体分析。结果表明,由于多种水系在此交汇,台湾海峡南部冬、夏季匀有明显锋面发育。受季风气候影响,锋面发育有显著的季节差异。夏季影响本海区的水系主要有韩江冲淡水、上升流、南海水、和黑潮水等。它们的交汇形成了韩江冲淡水羽状锋、台湾浅滩上升流锋、黑潮锋、以及陆架／陆坡锋等的三维锋结构。韩江冲淡水和上升汉对夏季海崃南部浅海峰     

福建沿海暨台湾海峡地质灾害初探

本文系统全面地论述了福建沿海及台湾海峡主要地质灾害类型的分在特征，发育规律及危害情况，对地质灾害的控制因素和相互的成因联系与其对于综合防治的意义进行了初步的分析，提出以成因与域因素相结合的地质灾害类型的划分原则。     

Phytoneuston in the southern Taiwan Strait

In June and November 1988 samples were collected by the improved Manta neuston net at 18 stations in the southern Taiwan Strait.One hundred and two species and variations of phytoneuston are identified.Total individuals of phytoneuston in June are more than those in November.The horiwntal distribution of phytoneuston is that the dense area occurs in the southern Taiwan Bank in June, while it appears in the western Taiwan Bank in November.The diet variations of phytoneuston are very obvious.The.abundance of phytoneuston occurs in the afternoon (16:00),and the minimum at midnight which is opposite to zooneuston.The relationships between phytoneuston and environment, and between phytoneuston and zooneuston are also discussed.     

台湾海峡南部漂浮植物

1988年6和11月,在台湾海峡南部用改进的Manta型漂浮生物网采集漂浮植物,共鉴定漂浮植物102种及变种.漂浮植物具有明显的季节变化,6月总数量高于11月.在平面分布上,6月漂浮植物密集区出现在台湾浅滩南部.11月密集区出现在台湾浅滩西部.漂浮植物数量具有一定的昼夜变化,最高值出现午后4时,最低值在午夜前后,与漂浮动物相反.讨论了漂浮植物与环境的关系,以及漂浮植物与漂浮动物的关系.     

闽台海岸带气候的异同

本文对闽，台海岸带的风况与风能资源，日照与太阳能资源，热量资源，水资源，台风等几种气候要素进行对比分析，并揭示闽，台海岸带气候的共同特征和差异。     

Abundance pattern of heterotrophic nanoflagellates in the southern Taiwan Strait

The analysis of 103 samples collected quantitatively from the southern Taiwan Strait (22°4'-24°3'N, 117°5'-119°9'E), China, in August 1997 indicates that the abundance of heterotrophic nanoflagellates (HNF) ranges from 391 to 1 846 ×103 cell/dm3, with an average of 949 × 103 cell/dm3, and 96.2% of cells are in size of 2-22 μm in all HNF met in the samples. The HNF cells are 9.83-45.79 μg/dm3 after conversion from cell number to carbon content, with an average of 22.82 μg/dm3 . The HNF abundance is relatively low in comparison with other areas. The nitrogen and phosphorus nutrients of the water are lower than previous investigations, which may be caused by the El Nino. The biomass of HNF is higher in southern waters, where cell concentration is 3-5 folds higher than that in other waters, and nearly 2-fold as high as the average of the investigated areas. The HNF is mainly habitat in 0-30 m water layer. Both horizontal and vertical HNF distribution must be influenced by hy-drographical dynamic pro     

台湾海峡南部夏季的颗粒有机碳

根据2004年夏季、2005年夏季和2006年夏季3个航次观测的颗粒有机碳(POC)数据,表层POC含量的分布表现出近岸高、远岸低的特点,表层和次表层POC含量的高值区出现在东山以东以及南澳附近上升流区。沿岸流较强的2005年和2006年航次具有相对丰富的总悬浮颗粒物(TSM)含量。浮游植物是该区POC的主要来源。各航次的POC含量与叶绿素a(Chl a)含量正相关,所有航次统计的Chl a/POC与Chl a呈正相关,上升流区Chl a/POC偏小,上升流较强的航次高Chl a区的Chl a/POC也偏小,反映了上升流与高营养转换效率浮游生物生态在空间和时间上的联系。根据Chl a/POC~Chl a关系图判断,台湾海峡南部海域1988年、1998年和2004年夏季航次的浮游生物营养转换效率受到相对抑制,而在上升流信号较强的2005年和2006年夏季航次,上升流区的浮游生物高营养转换效率状态得以强化。各航次的POC含量和Chl a/POC比值与TSM含量正相关,POC/TSM比值与TSM负相关,沿岸流带来的陆源悬浮颗粒物通量波动,并没明显干扰台湾海峡南部以海洋浮游生物生态主导的颗粒有机碳生物地球化学循环格局。     

Bridges, Tunnels and Their Relationship to the Economic Development on Both Sides of Taiwan Strait

The construction of bridges and tunnels plays an important role in the social and economic development of cities and local regions. The planning of the bridge and tunnel across Taiwan Straits will have a positive effect on the economic development at each stage: preplanning, engineering construction, and the completion of the project. The two sides of Taiwan Straits have the advantage of a suitable location, consanguineous relationship, and appropriate geographic conditions. Currently, there are many economic and cultural communications between both sides of the Straits. The bridge and tunnel from Xiamen to Jinmen can be regarded as the beginning of the “golden link belt.” The total capability for sustainable development of Fujian Province ranks the sixth among 31 provinces in China, which will provide powerful support for the construction of the bridge and tunnel.     

Bridges,Tunnels and Their Relationship to the Economic Development on Both Sides of Taiwan Strait

The construction of bridges and tunnels plays an important role in the social and economic development of cities and local regions. The planning of the bridge and tunnel across Taiwan Straits will have a positive effect on the economic development at each stage: preplanning, engineering construction, and the completion of the project. The two sides of Taiwan Straits have the advantage of a suitable location, consanguineous relationship, and appropriate geographic conditions. Currently, there are many economic and cultural communications between both sides of the Straits. The bridge and tunnel from Xiamen to Jinmen can be regarded as the beginning of the “golden link belt.” The total capability for sustainable development of Fujian Province ranks the sixth among 31 provinces in China, which will provide powerful support for the construction of the bridge and tunnel.     

台湾海峡两岸地质特征和演化

文中参照各家关于台湾海峡及邻区的地质构造和演化的观点,依据作者的野外考察和室内研究成果,列举了一些鲜为人知的事实和困难,以澄清海峡两岸的构造联系和差异,肯定了浙闽结晶基底属于古亚洲大陆并发育为加里东地槽,而台湾结晶基底与板块俯冲密切相关。上覆岩系反映了地壳运动所导致的海侵、海退旋回,中生代的火山活动和板块碰撞。该区的北东向断裂愈临近太平洋板块活动强度愈大,时代较新的北西向断裂在海峡两岸均有走滑压性特征。文中详述了在基底构造、上覆岩系、断裂系统方面需要深化的认识。