我国及邻区板内地震与板缘地震的关系

我国及邻区可划分为两个地震域。其内带及外带的地震活动有相互消长的关系。相邻板块施加的外力,使板内水平压应力增强,是板内地震的主要原因。热羽活动、地幔上隆、固体潮、地球旋转轴摆动、地球自转速率变化可能是次要原因     

热层大气潮汐微分算子与微分积分方程

本文进一步讨论了热层大气潮汐微分算子的问题,求得了有平均风场及风切变时的微分算子;从有限汉克尔（Hankel）变换的反演,求得了热层大气结构的微分积分方程,并讨论了这一方程的求解问题。     

长江中下游地区内生铁铜矿床与膏盐的关系

A middle-Trlassic sequence of strata composed .of gypsumstlt beds has been reeognized in the middle-lower Yangtze Valley. The mineralization in the gypsum-salt beds is closely related to Yenshanian magmatism, During the Yenshanian, magmatic intrusion activities were very active across evaporite beds, occupying great space in gypsum-salt beds. The magmatie rocks and the alterated country rocks are characterized by alkali-eurichment and halogen-enrichment. Copper and iron ores mainly occur in the evaporite beds or overlying levels. The genesis of endogenic copper and iron ores is commonly considered to be the consequence of interaction of magma with the gypsumsalt beds, i.e. there exists a close genetic connection between evaporites, magmatism and copper-iron ores. These observed features are of great significance both in practice and theory.     

北海海陆风环流特征分析

利用北海气象观测站测风资料,分析北海海陆风环流的日变化及其季节变化特征,分析结果表明：陆风出现时间为半夜前后开始,５￣７ｈ达最强盛期,中午前后结束：海风出现时间为中午前后开始,１６￣１８ｈ达最强盛期,半夜前后结束 。     

热带西太平洋暖池和副热带高压之间的关系

文中研究了热带西太平洋暖池和西太平洋副热带高压的季节性变化和年际变化关系。结果表明,西太平洋暖池面积和副热带高压面积指数季节变化趋势基本一致,暖池中心的纬向移动与副热带高压西伸脊点相反,而经向移动和５００ｈＰａ副热带高压脊平均位置的南北季节性变化非常一致。西太平洋副热带高压的年际变化落后暖池大约３个月左右,用暖池２８℃或２９℃面积指数可以很好地预测出当年６,７,８三个月西太平洋副热带高压的面积指数。     

中国地区大气气溶胶辐射强迫及区域气候效应的数值模拟

利用太阳直接辐射日总量和日照时数等多年观测资料,反演了中国地区大气气溶胶0.75 μm光学厚度的年、月平均值,分析了我国大气气溶胶状况的时空分布特征。据此,在中国区域气候模式中考虑气溶胶的辐射影响,模拟中国地区气溶胶直接辐射强迫的大小及气候响应的季节变化特征。计算结果表明: 我国大气气溶胶光学厚度多年平均分布状况是以四川盆地为大值中心向四周减少;长江中下游武汉附近和南疆盆地为另两个大值中心;青藏高原为气溶胶低值区;我国绝大部分地区春季气溶胶光学厚度值最大,各地气溶胶光学厚度最小值出现的季节则有所不同。气溶胶辐射强迫介于-5.3～-13 W/m2之间;辐射强迫具有春、夏季大,秋、冬季小,冬季南方偏大,夏季北方偏大的特征。气溶胶辐射强迫的分布与其光学厚度的分布基本一致。由于气溶胶的影响,中国大陆地区地面气温均有所下降,四川盆地到长江中下游地区以及青藏高原北侧到河套地区降温最为明显,分别可达-0.4℃和-0.5℃。气候响应具有明显的季节特征。地面气温的变化除与辐射强迫的大小有关外,还受大气环流的影响。     

FPGA在时间测量中的应用

利用现场可编程门阵列(FPGA)的内部资源，在FPGA中实现了高精度时间间隔测量系统的设计。     

Substrate selection and seasonal variation in abundance and size composition of isopod Lirceus fontinalis in Ontario streams, Canada

The abundance and size composition of stream isopods Lirceus fontinalis were investigated from April 2001 to August 2002 in 3 streams in southern Ontario, Canada. Effects of current speed was released from the analysis by choosing slow flowing water. The effects of substrate, season and water depth on the abundance, distribution and size composition of the isopods were analyzed. It was found that substrate and season influence isopods the most. The rocky substrate with attached filamentous macro-algae contains an isopod abundance 7.05 times that of bare rock substrate and 14.6 times that of fine-sand and mud substrate. There was a large variation with respect to seasonality in both abundance and size composition of the isopods, with the highest abundance occurring in summer and the lowest in winter and spring; individual isopods also tend to be larger in the winter and spring. In all substrates, shallow areas tend to support higher densities of isopods than deeper areas.