1) SST
表层海温
1.
Numerical Experiment of SST Response to Typhoon Process in Yellow Sea and Bohai Sea;
黄、渤海表层海温对台风过程响应数值试验
2.
By comparative analysis on the SST variations in Pearl River estuary,the reasons that caused the difference of SST variations during two strongest El Nino events of 20th century in 1982/1983 and 1997/1998 are investigated.
比较分析20世纪2次最强El Nino事件(1982/1983年与1997/1998年)珠江口表层海温(SST)的变化差异,发现造成其差异的原因:一是到达地面的太阳总辐射1982/1983年高于1997/1998年;二是南海高压势力1982/1983年弱于1997/1998年;三是1982/1983年冬季风速比1997/1998年大1~2 m/s。
2) subsurface temperature
次表层海温
1.
Annual variation characteristics of subsurface temperature, HST and MLD overthe Tropical Pacific-Indian Ocean and the relationship between the characteristics and ENSO,Indian Ocean dipole and ITCZ are studied by applying the subsurface temperature, HSTand MLD data from 1955 to 2003, using the method of EOF.
根据1955~2003年次表层海温、海洋上层400m热含量和混合层深度资料,采用EOF分析方法,研究热带太平洋-印度洋上层海温、热含量和混合层深度的年变化特征及其与厄尔尼诺、印度洋偶极子、热带辐合带分布和活动的关系。
3) sea surface temperature
海面温度海水表层水温
4) SST
海水表层温度
1.
Preliminary Analysis on the Relationship between the Distribution of Fishing Ground of Pacific Saury(Cololabis saira) and SST in Northwest Pacific;
西北太平洋秋刀鱼渔场分布及与海水表层温度的关系分析
2.
Evidences show that high sea surface temperature (SST) have close relationship with coral reef bleaching.
卫星遥感能够提供大范围、同步与连续的海洋数据,如海水表层温度和海色数据,从而能够及时监测和预测珊瑚礁的白化。
5) sea surface temperature
海水表层温度
1.
The sea surface temperature was estimated using the \%U\%\+k\-\{37\} value (the unsaturated ratio of alkenone) in sediment from the Okinawa Trough during the last 20000 years, which ranges from 15 9℃ to 26 2℃ with an average of 22 9℃.
应用生物标志化合物长链烯酮不饱和比值 Uk37估算冲绳海槽 2万年以来古海水表层温度 ,其波动范围在 1 5。
2.
Glacial-interglacial fluctuations and long-term changes in carbonate dissolution and preservation, sea surface temperature (SST), depth of thermocline (DOT), paleoproductivity and predominant PF species as responding to the East Asian paleo.
11′E,水深2,772米)997个样品中浮游有孔虫群的研究,揭示了210万年来南海南部高分辨率(约2千年)的古海洋学变化历史,展示了碳酸盐溶解与保存、海水表层温度、温跃层深度、古生产力以及浮游有孔虫主要属种在冰期-间冰期和长时间尺度上的变化,以及对东亚季风和热带气候演化的响应。
3.
Based on the catch amount data of Chinese squid jigger vessels from January to July 2006 and the sea current, sea surface temperature (SST) and chlorophyll-a (chl-a) data derived from satellites, the characteristics of Illex argentinus fishing grounds, their productivity, and environment factors in southwest Atlantic were analyzed.
基于2006年1—7月中国鱿钓船在西南大西洋捕获阿根廷滑柔鱼的生产数据及卫星反演的海流、海水表层温度和叶绿素a浓度等海洋环境资料,综合分析了阿根廷滑柔鱼的作业渔场、产量及环境特点。
6) sea surface temperature
表层海水温度
1.
Cores DOC024,retrieved from the northern Okinawa Trough in the East China Sea,are used to reconstruct the upwelling evolution over the last 7 300 years based on a multi-proxy approach including the combination of planktonic foraminifer fauna,Neogloboquadrina dutertrei δ18O,sea surface temperature(SST)and depth of thermocline.
对取自冲绳海槽北部的DOC024岩心进行了浮游有孔虫氧同位素和统计分析,依据浮游有孔虫群落组合和Neogloboquadrina dutertreiδ18O的记录以及表层海水温度、温跃层深度的变化揭示了近7300aBP以来日本九州西南海区上升流的演化过程。
2.
ruber shells,in order to reconstruct the sea surface temperature(SST)changes at a general time resolution of average ca.
ruber壳体的Mg/Ca比值测定,再造了距今约140ka以来时间分辨率约800年的表层海水温度(SST)变化,揭示末次冰期南海南部的SST曾降温达约5℃,且存在类似Dansgaard-Oeschger(D/O)事件的千年尺度波动。
3.
The quantitative census of planktonic foraminifera from the upper 25 m of ODP 130 Site 807A,combined with the paleotemperature data estimated by using faunal transfer function and the oxygen isotopic record,reveal the periodical changes of sea surface temperature(SST) and thermocline in the Western Pacific Warm Pool(WPWP) during the last 1.
6 Ma以来冰期旋回中赤道西太平洋的表层海水温度和温跃层深度的变化,为研究西太平洋暖池的变动提供了重要依据。
补充资料:春暮过石龟谷题温处士林园(一作送温逸人)
【诗文】:
隐几无名老,何年此陆沈。丘园自得性,婚嫁不婴心。
岁计因山薄,霞栖在谷深。设罝连草色,晒药背松阴。
触兴云生岫,随耕鸟下林。支颐笑来客,头上有朝簪。
【注释】:
【出处】:
全唐诗:卷238_41
隐几无名老,何年此陆沈。丘园自得性,婚嫁不婴心。
岁计因山薄,霞栖在谷深。设罝连草色,晒药背松阴。
触兴云生岫,随耕鸟下林。支颐笑来客,头上有朝簪。
【注释】:
【出处】:
全唐诗:卷238_41
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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