APPLICATION OF MAP AND FILE INFORMATIONVISUALIZATION SYSTEM TO COMPREHENSIVEDIVISION OF NATURAL DISASTERS- Takingthe ChangjiangValleg as an Example

In recent years，scholars at home and abroad have method，and that vanous disasters would be analyzed assynthetically studied natural dlsaste‘theoretically and an Integral．SHI Peilun（1991）putforwad a scientificmethodologlcally，as well as its cases analys。s（CND，term—regional disaster system，which Indicates that1987； MA et al，1990； MARBLE，1990； NE et al，the situation of a disaster（calamity loss）results from1999； PATAK et al，1982； SHI，1991；VAN et al，h…     

FARMLAND AND URBAN AREA DYNAMICS MONITORING INCHINA USING REMOTE SENSING AND SPATIALSTATISTICS METHODOLOGY

1 INTRODUCTIONGlobal change research involves much geo-objectsand geo-process, such as climate and environmentalchange, substance and energy cycling, land-use/land-cover change (LUCC), interactivity between human and nature, etc.. So it need cooperation frommany research communities including international research programs groups such as IGBP (InternationalGeosphere-Biosphere Programme IPCC (Intergovemmental Panel on Climate Change), IHDP (InternationalHuman Dimension Program o…     

大城市气象要素日变程数值模拟

众所周知,在大工业中心,人们的生产活动,导致了大气污染及气象状况的改变。近年来,在小气候研究中,物理——数值模拟方法得到了广泛的应用。采用这一方法可以在一定程度上阐明地球边界层污染的形成过程,深入研究各种气象特征的发展动力。     

Effect of Ploughing Depth on the Growth and Yield of Heracleum candicans： a Threatened Medicinal Herb and a Less-explored Potential Crop of the Himalayan Region

This paper examines the effect of ploughing depths （A -- 60 cm, B -- 45 cm and C -- 30 cm） on the growth and yield of Heracleum candicans Wall （Apiaceae）, a threatened medicinal herb of the Himalayan region. This less-explored plant is being suggested as a potential crop for the mountain agriculture. The study was carried out in an orchard in Himachal Pradesh, India at 2500 m altitude, for two successive growth years. During the first year, all plants remained in juvenile state; in the second year, nearly 65 % plants produced flowers only under 60cm ploughing depth. Among its morphological traits, plant height, collar diameter and aboveground flesh weight were found to be strongly correlated （P 〈 0.01） with the belowground biomass during the first year （r =0.968, 0.925 and 0.973, respectively） and during the second year （r=0.945, 0.928 and 0.775, respectively）. Increase in the ploughing depth was significantly correlated （P〈0.01） with all growth parameters, including the belowground dry weight, marketable portion of the produce. The belowground biomass （commercial yield; 16.28 Qt/hec） at depth A was about 2.6 and 4.7 times higher than those recorded at depths B and C, respectively. The results clearly justify the importance of deep ploughing and this paper strongly recommends it for economically sustainable cropping.     

八十年代英国中学地理教学

八十年代,地理教学在英国学校中占有众所承认的地位,英国学校把地理教学纳入教程的方式因地方教育机构所管理的学校学制不同而异。最普遍的学制是5～11岁的儿童上小学,9—13岁的儿童上中学,这些学校均将地理纳入综合的教学课程中,或做为环境教育的部分内容。     

地生态学的理论及一些实践问题

在确定地理学在环境科学中的地位以前,首先须简要概述这方面的矛盾现象。在60—70年代生态问题范围已明显地大大扩充了,已不能容纳在传统的生物生态学范围内。开始寻求新的定义,在探索过程中产生或重建了人的生态学,社会生态学(Э.С.马尔卡扬),人类生态学(Н.Н.玛依塞耶夫),全球生态学(М.И.布迪科)。我们认为,后两种名称只说明了生态学的规模,它的新“范围”,而不是新观点,新方法。第一种名称人的生态学这一术语已广为流传,它的情况较复杂,在西方也提出了人的生态学。     

NGC4051短时标光变的多波段同时性观测

探索活动星系的快速光变,是研究星系中心致密核结构及辐射机制的强有力手段。NGC4051是在X射线波段具有短时标(分—小时)光变的极少数活动星系之一。为进一验证X射线波段短时标光变的观测结果,也为了探索光学波段是否具有短时标光变及它们的相关性,我们于1985年5月13—15日分别在美国和中国对NGC4051进行了X射线波段及可见光波段的同时性联测。Martin博士和程福臻在美国利用EXOSAT卫星观测了NGC4051的X射线辐射;谢光中等人在云南天文台利用一米RCC望远镜及积分光度计进行了U波段的观测。结果如下:(1)软X射线的流量降低了13倍,而硬X射线的流量已小到探测不到(至少降低了203倍);(2)U波段在13日晚的观测表明NGC4051有一个时标～1200秒、振幅ΔU 0.11(±0.03)的短时标光变。这种光变共有四个事例,且光变曲线十分完整,由于标准误差σ=0.03,可信度已大于3σ。此外,这一结果还与P.E.Marshall等人在X—射线波段所得到的光变时标～1000秒相吻合,这似乎表明两个波段的光变可能具有相关性。     

Sequences in the Hardness Ratio-Peak Energy Plane of Gamma-Ray Bursts

The narrowness of the distribution of the peak energy of the vFv spectrum of gamma-ray bursts (GRBs) and the unification of GRB populations are great puzzles yet to be solved. We investigate the two puzzles based on the global spectral behaviors of different GRB populations, the long GRBs, the short GRBs, and the X-ray flashes (XRFs), in the HR - Ep plane (HR the spectral hardness ratio) with BATSE and HETE-2 observations. It is found that the long GRBs and the XRFs observed by HETE-2 seem to follow the same sequence in the HR-Ep plane, with the XRFs at the low end of this sequence. We fit the sequence by a universal Band function, and find that this sequence is mainly defined by the low energy index α, and is insensitive to the high energy index,β. With fixed β=-5, a best fit is given by α=-1.00 with X^2min/dof=2.2. The long and short GRBs observed by BATSE follow significantly different sequences in the HR-Ep plane, with most of the short GRBs having a larger hardness ratio than the long GRBs at a given Ep. For the long GRBs a best-fit yields α=-0.30 and β=-2.05. For the short GRBs, a best fit gives α=-0.60 with x^2min=1.1 (withβfixed at-2.0 because it is numerically unstable). The α value for the short GRBs is significantly greater than that for the long GRBs. These results indicate that the global spectral behaviors of the long GRB sample and the XRF sample are similar, while that of the short GRBs is different. The short GRBs seem to be a unique subclass of GRBs, and they are not the higher energy extension of the long GRBs.     

Effect of Counter-Gradient in the Computation of Turbulent Fluxes of Heat and Moisture in a Regional Model

The counter-gradient terms in the computations of turbulent fluxes of heat and moisture have been included in the PBL parameterization of a regional model for monsoon prediction. Results show that inclusion of counter-gradient terms has a marginal impact in the prediction of large scale monsoon circulation and rainfall rates.     

Wintertime Stratospheric Anomalies-Part I: Warm Pools

The stratospheric worm pools, called the 4-day wave also, are mainly the temperature anomalies in the polar regions of winter hemisphere. It will be shown that their occurrence, propagation speed and specific structure can be explained by the lower frequency coherent heating resulting from the wave interaction in the breaking layers of the stratosphere. Although their vertical phase slope is negligibly small, the warm pools cannot be considered as a barotropic anomaly.