Ocean-Atmosphere Interaction in the Lifecycle of ENSO： The Coupled Wave Oscillator

To explain the oscillatory nature of E1 Nino/Southern Oscillation （ENSO）, many ENSO theories emphasize the free oceanic equatorial waves propagating/reflecting within the Pacific Ocean, or the discharge/recharge of Pacific-basin-averaged ocean heat content. ENSO signals in the Indian and Atlantic oceans are often considered as remote response to the Pacific SST anomaly through atmospheric teleconnections. This study investigates the ENSO life cycle near the equator using long-term observational datasets. Space-time spectral analysis is used to identify and isolate the dominant interannual oceanic and atmospheric wave modes associated with ENSO. Nino3 SST anomaly is utilized as the ENSO index, and lag-correlation/regression are used to construct the composite ENSO life cycle. The propagation, structure and feedback mechanisms of the dominant wave modes are studied in detail. The results show that the dominant oceanic equatorial wave modes associated with ENSO are not free waves, but are two ocean-atmosphere coupled waves including a coupled Kelvin wave and waves are not confined only to the Pacific a coupled equatorial Rossby （ER） wave. These Ocean, but are of planetary scale with zonal wavenumbers 1-2, and propagate all the way around the equator in more than three years, leading to the longer than 3-year period of ENSO. When passing the continents, they become uncoupled atmospheric waves. The coupled Kelvin wave has larger variance than the coupled ER wave, making the total signals dominated by eastward propagation. Surface zonal wind stress （x） acts to slow down the waves. The two coupled waves interact with each other through boundary reflection and superposition, and they also interact with an off-equatorial Rossby wave in north Pacific along 15N through boundary reflection and wind stress forcing. The precipitation anomalies of the two coupled waves meet in the eastern Pacific shortly after the SST maximum of ENSO and excite a dry atmospheric Kelvin wave which quickly circles the whole equator and leads to a zonally symmetric signal of troposphere temperature. ENSO signals in the Indian and Atlantic oceans are associated with the two coupled waves as well as the fast atmospheric Kelvin wave. The discharge/recharge of Pacific-basin-averaged ocean heat content is also contributed by the two coupled waves. The above results suggest the presence of an alternative coupled wave oscillator mechanism for the oscillatory nature of ENSO.     

微波消解-电感耦合等离子体原子发射光谱法测定催干剂中金属元素含量

应用电感耦合等离子体原子发射光谱法(ICP-AES)测定了不同种类催干剂中9种金属元素,即钴、锰、铅、钙、锌、钒、锆、镧和铈。样品置于聚四氟乙烯溶样罐中加入浓硝酸及高氯酸,盖紧罐盖后按预设程序分两步进行微波加热,加压消解,所得溶液稀释至一定体积供ICP-AES分析。对上述元素的谱线中选择合适的谱线作分析线,达到了9元素的同时测定。同混合标准溶液制备各元素的工作曲线,其线性范围均在100.0 mg·L~(-1)以内。以一催干剂样品为基体,用标准加入法作回收试验,测得回收率在93.8%～109.9%之间,测定值的相对标准偏差(n=6)在0.11%～1.56%之间。不同来源的5个催干剂样品的分析结果表明所测得的金属元素的类别和含量显著差异。试验还证实所提出的方法具有操作快速、简单、方便,适合应用于日常分析工作。     

浅析环境空气样品采集的影响因素

环境空气质量中的气态污染物的监测监测结果的准确可靠,除了实验测试条件的掌控、测试人员的技术水平外,还与样品的采集过程有关.作为常规例行监测的项目,空气中二氧化硫、二氧化氮的监测已进行多年.作者在实际工作中发现,样品采集的影响因素对监测结果产生直接的影响,但这些因素往往被忽视.本文将从最常见、常常被人忽视而对监测结果直接产生影响的环境温度、采样瓶阻力和动力系统等方面进行分析.     

微波辅助萃取/样品前处理联用技术的研究进展

微波辅助萃取是近年来新发展的一种样品前处理技术,随着微波辅助萃取的发展和成熟,它与其它样品前处理技术的联用得到了迅速发展。与传统前处理方法相比,这些联用方法具有快速、高效、操作简便、节省溶剂、选择性好、应用范围广的特点。该文综述了微波辅助萃取及其与其它样品前处理技术联用的特点及适用性,并对近年来微波辅助萃取与其它前处理方法联用的发展概况及在分析领域中的应用情况进行了详细总结。     

凝固点降低测定物质摩尔质量实验装置的改进

介绍一种改进的凝固点降低法测定物质摩尔质量的实验装置,通过调节合适的阻凝温度与散热补偿电流,对样品凝固点的测定精度可以达到±0.003℃,对样品摩尔质量的测定误差可控制在0.5%左右。     

氢化物发生-原子荧光光谱法测定海洋沉积物中砷、锑、铋、汞、硒

提出了用盐酸-硝酸-水(3+1+4)混合酸消解样品,氢化物发生-原子荧光光谱法测定海洋沉积物样品中砷、锑、铋、汞、硒的方法。考察了原子荧光光谱仪的最佳工作条件。在最佳条件下砷、锑、铋、硒的检出限(3s/k)分别为0.018,0.004,0.001,0.003μg.g-1,汞的检出限(3s/k)为0.604ng.g-1。应用于3种海洋沉积物标准物质的测定,测定值与标准值吻合。     

Synthesis and Characterization of Magnetic TiO2/SiO2/NiFe2O4 Composite Photocatalysts

Magnetic TiO2/SiO2/NiFe2O4 composite photocatalytic particles with high crystalline TiO2 shell were synthesized via a mild solution route.The prepared composite particles were characterized with X-ray diffraction(XRD),transmission electron microscopy(TEM),high resolution transmission electron microscopy(HRTEM),scanning electron microscopy(SEM),ultraviolet-visible(UV-Vis) spectroscopy and vibrating sample magnetometer(VSM).The results show that the obtained TiO2/SiO2/NiFe2O4 composite particles were composed...     

铀矿样FPXRF分析中Th、Sr的影响与校正

探讨了Th、Sr元素与U伴生的地质学依据以及伴生元素的存在对U含量的FPXRF分析的干扰机理:铀样品中Th、Sr元素的影响主要表现为FPXRF仪器谱上ThLα和SrKα特征X射线对ULα特征X射线的干扰。结果表明,采用U、Th、Sr多元回归模型能有效地校正谱线重叠干扰,应用FPXRF分析铀矿样品中铀含量与推荐值相对误差控制在一定范围内,基本满足野外生产要求。     

镜面物体往复通过弱湍流大气系统的成像

分别利用部分相干理论、以广义随球波函数为基础的Ｋａｒｈｕｎｅｎ－Ｌｏｅ′ｖｅ展开和相干成像理论研究了弱湍流像差大气照明系统互强度函数传输特征和位地湍流介质中镜面物体成像规律。结果表明：仅当反射光束相干尺度（成像光束等效直径）小于成像孔径的尺度时才能改善湍流大气中两次成像的质量。     

化学分析测量的质量保证

介绍了化学分析测量过程中取样、样品处理和测量中的质量保证。