教師の資質能力に関する調査 : 小学校予備調査の結果分析

本研究の目的は,小学校教師の資質能力を調査し,教員養成および現職教育のプログラムを開発することにある。そのために学校教育に関与する人々-ステークホルダー-に質問紙調査を行った。本論文では,その予備調査の結果を分析した。ステークホルダーはいずれも今日の子どもを取り巻く諸問題に敏感に反応して回答している。しかしながら保護者と教師では,子どもへの焦点の当て方が異なっている。教師はある種の能力を大学で身につけ,他の能力を勤務校で身につけると考えられている。この研究は教師のライフステップを見極めた研究へとつながることが望まれる。The purpose of this research is to investigate necessary abilities to be a good elementary school teacher and to develop programs for teacher training and an incumbent education. For this purpose we sent out questionnaires to the people who take part the academic training. We call them \u27stake-holder\u27. In this thesis, the result of this preliminary research was analyzed. Every \u27stake-holder\u27 made answers sensitively reacting to today\u27s child\u27s problems. However the focus point in the process of watching children is different between the guardian and the teacher. It is thought that teachers acquire certain kind of skills at the university, and acquire other skills in work school. It is hoped this research leads to further research that ascertains the life step of teachers

Studies of japanese climate based on macro-scale airflow patterns

Cluster analysis is adopted to the airflow system of Japanese Islands and macro-scale airflow patterns are set up. In each macro-scale airflow pattern, pressure system and distribution of climatic element are characteristic. Adopting principal component analysis to distribution of climatic element, fundamental climatic conditions are expressed. By these conditions, land surface features and pressure system in major synoptic cimatological field are discussed. Further, influences of macro-scale airflow patterns to the yearly variation of air temperature and pecipitation are clarified

Some characteristics of shrine distribution in central japan

For the fear of strong winds which bring calamity to a rice crop, there are shrines that deify the god of wind in various places in Japan. In order to clarify various wind god shrines, the distribution of prominent shrines, which has influenced them, was investigated. Consequently, it became clear that the distribution of prominent shrines can be roughly classified into six types. They are whole country type, central part type, inland type. Kanto type, Chugoku type, and Kyushu type. It was presumed that their formation age and the difference in divine favor reflect these distributional types

Macro-scale airflow patterns in the japanese islands

Daily surface wind distributions in the Japanese Islands in 1973 are classified by cluster analysis. As a result, twelve macro-scale airflow patterns are clarified. Their resultant wind patterns are characterized as follows: southwesterly wind or sea breeze (a1-a4 type), northeasterly wind (b1-b3 type), and northwesterly wind (c1-c5 type). Applying discriminant analysis to the other years, the daily patterns are clarified from 1968 to 1977. According to their frequency in the calender pentad, the periods in which each type prevails are as follows: summer (a1-a4 type), spring or autumn (b1-b3 type) and winter (c1-c5 type). Furthermore, the macro-scale airflow patterns are considered good indicators of the climate in the Japanese Islands

Climatic change during historical times in japan : reconstruction from climatic hazard records

A synoptic analysis of climatic hazard records in historical times of Japan is presented. The cool age (7-9c.), the warm age (10-14c.) and the cold age (15-19c.) are indicated. The relationship between summer and winter conditions in the climatic change is also shown. Thus, the knowledge of the climatic change in Japan from the 7th to the 19th century was systematically summarized

Climate of little ice age in japan

The climate during the period from 16th to 19th century in Japan was reconstructed by the historical weather records of the Feudal Clan Tsugaru. Fluctuations of monthly precipitation frequency, snowfall ratio and so on were examined, and deviations of temperature and precipitation were estimated. Further, "Little Ice Age" in Japan was divided into three cold phases and two interglacials. The cold phases are as follows: 1611-1650, 1691-1720 and 1821-1850