三爪仑国家森林公园旅游气候分析

从气候特点、旅游气候适宜度、气象气候风景资源及旅游气象障碍等方面进行分析,发现三爪仑国家森林公园是理想的观光、度假、避暑和疗养的胜地。     

An investigation of the environmental loads of Shei-Pa National Park in Taiwan

 Recreation is one of the functions of national parks. Nevertheless, heavy tourism has started to impose serious problems on the maintenance of some national parks in Taiwan. This study has tried to survey as well as calculate the impact problems resulting from park tourism in terms of environmental loads. A simple method is proposed to calculate the quantity of environmental loads. Only visitor information from questionnaires and per capita data are needed in the calculation process. Shei-Pa National Park was taken as an example. The water demand, the electricity used and the various forms of the environmental loads, including wastewater and solid waste discharge, were all surveyed and calculated on a per capita basis. Received: 21 July 1999 · Accepted: 8 November 1999     

Rural poverty in Peninsular Malaysia and the Malaysian national agricultural policy

The National Agricultural Policy was implemented to arrest the decline that agriculture experienced in the 1970s and early 1980s. It aims to modernise and revitalise Malaysian agriculture and alleviate rural poverty while retaining labour in agriculture. This paper evaluates its likely effects on poverty among small‐scale padi farmers. The analysis is based on an evaluation of the strategies and programs that are being implemented as part of the policy. It is argued that the National Agricultural Policy will not alleviate poverty in the padi sub‐sector for three main reasons. Firstly, the strategies and programs currently being employed are essentially unchanged from those that were unsuccessfully employed in the past. Secondly, it is premised on a theoretical base which will not lead to the development of effective anti‐poverty strategies. And, finally, it is flawed by policy contradictions.     

中国国家气象中心中期数值天气预报业务系统

中期天气预报的研究要形成日常的业务，不仅仅是气象问题，也包括相当多的工程技术上的问题。本文概括地描述中国国家气象中心建立中期数值天气预报业务系统过程中的研究与工程建设成果以及运行状况、效果检验等。     

Contour scaling of a sandstone by salt weathering under simulated hot desert conditions

A laboratory study has been used to investigate relationships between salts and contour scaling—a weathering feature commonly observed on rock surfaces in salt-rich environments. Surface disaggregation and essentially surface-parallel cracks were produced in sandstone blocks using 10 per cent solutions of sodium sulphate and magnesium sulphate applied daily to single exposed surfaces for sixty days. A control block soaked once in saturated magnesium sulphate and subsequently wetted daily with distilled water showed extensive surface disaggregation, but no cracking. Both surface disaggregation and subsurface cracking were associated with relative concentrations of microcrystalline salt. A tentative model of contour scaling is proposed, which involves linking together potential cracks by salt-induced fracturing of intervening, crack-stopping grains. Further control blocks treated respectively with 10 per cent and saturated sodium chloride showed no evidence of subsurface cracking and only limited surface disaggregation of the ‘saturated’ block.     

The formation of offshore ripples in the zone under irregular waves

In this article, results obtained from an experimental investigation conducted to determine the wave-induced geometric characteristics of offshore ripples and bars are presented. The experiments were performed using irregular waves. Natural beach sand was used in the study, where the mean diameter was 0.35 mm and the specific gravity was 2.63. The initial slope of the beach was 1:5. Different wave groups were generated over the initially flat beach, and a number of characteristics were determined. These include the ripple number, individual and average ripple heights, individual and average ripple lengths and the length of the offshore bar. The results of the experimental study were evaluated and empirical expressions based on the results were formulated.     

Laboratory Experiment of Plasma Flow Around Magnetic Sail

To propel a spacecraft in the direction leaving the Sun, a magnetic sail (MagSail) blocks the hypersonic solar wind plasma flow by an artificial magnetic field. In order to simulate the interaction between the solar wind and the artificially deployed magnetic field produced around a magnetic sail spacecraft, a laboratory simulator was designed and constructed inside a space chamber. As a solar wind simulator, a high-power magnetoplasmadynamic arcjet is operated in a quasisteady mode of 0.8 ms duration. It can generate a simulated solar wind that is a high-speed (above 20 km/s), high-density (10¹⁸ m⁻³) hydrogen plasma plume of ∼0.7 m in diameter. A small coil (2 cm in diameter), which is to simulate a magnetic sail spacecraft and can obtain 1.9-T magnetic field strength at its center, was immersed inside the simulated solar wind. Using these devices, the formation of a magnetic cavity (∼8 cm in radius) was observed around the coil, which indicates successful simulation of the plasma flow of a MagSail in the laboratory.     

Scaling Laws for Collisionless Laser–Plasma Interactions of Relevance to Laboratory Astrophysics

Scaling laws for interaction of ultra-intense laser beams with a collisionless plasmas are discussed. Special attention is paid to the problem of the collective ion acceleration. Symmetry arguments in application to the generation of the poloidal magnetic field are presented. A heuristic model for evaluating the magnetic field strength is proposed. PACS Numbers: 52.38Kd, 52.38.Fz, 41.75.Jv     

Holocene beaver damming, fluvial geomorphology, and climate in Yellowstone National Park, Wyoming

We use beaver-pond deposits and geomorphic characteristics of small streams to assess long-term effects of beavers and climate change on Holocene fluvial activity in northern Yellowstone National Park. Although beaver damming has been considered a viable mechanism for major aggradation of mountain stream valleys, this has not been previously tested with stratigraphic and geochronologic data. Thirty-nine radiocarbon ages on beaver-pond deposits fall primarily within the last 4000 yr, but gaps in dated beaver occupation from ~ 2200–1800 and 950–750 cal yr BP correspond with severe droughts that likely caused low to ephemeral discharges in smaller streams, as in modern severe drought. Maximum channel gradient for reaches with Holocene beaver-pond deposits decreases with increasing basin area, implying that stream power limits beaver damming and pond sediment preservation. In northern Yellowstone, the patchy distribution and cumulative thickness of mostly < 2 m of beaver-pond deposits indicate that net aggradation forced by beaver damming is small, but beaver-enhanced aggradation in some glacial scour depressions is greater. Although 20th-century beaver loss and dam abandonment caused significant local channel incision, most downcutting along alluvial reaches of the study streams is unrelated to beaver dam abandonment or predates historic beaver extirpation.