STUDY ON PERIGLACIAL PHENOMENA AND ENVIRONMENTS IN THE ALPINE ZONE OF JAPAN
STUDY ON PERIGLACIAL PHENOMENA AND ENVIRONMENTS IN THE ALPINE ZONE OF JAPAN
批准号:
07458023
负责人:
TAKAHASHI Nobuyuki
金额:
$4.54万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (B)
财政年份:
1995
资助国家:
日本
项目状态:
已结题
起止时间:
1995 至 1997
中文摘要
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英文摘要
Observations of air and ground temperature and wind speed and direction were carried out in the alpine zone of Japanese high mountains, the Daisetsuzan Mountains, Mt.Yoteizan and Mt.Rishirizan in Hokkaido, northern Japan, and Mt.Sugorokudake and Mt.Minamidake in central Japan. The results are summarized as follows.1. the Daisetsuzan MountainsThe air temperatures at the wind-blown bare sites and at the forest line of 1,700m a.s.l. showed that the upper part of the Daisetsuzan Mountains belongs to a discontinuous permafrost zone and moreover to the alpine zone. The mean wind speed at the wind-blown site from October to April exceeds 10 m/s, and the prevailing wind direction is WNW.In autumn the lowest ground temperature is recorded in the Pinus pumila community, characterizing the upper part of Japanese high mountains, among all the plant communities. This indicates that the Pinus pumila community creates a peculiar environment for the ground temperature regime in summer.2. Mt.Yoteizan a … More nd Mt.RishirizanThe air temperatures at the wind-blown sites near the summits of Mt.Yoteizan (1,898m a.s.l.) and Mt.Rishirizan (1,719m a.s.l.) indicated that the climatic conditions of both sites corresponds to that of discontinuous permafrost zone. But a permafrost has not been confirmed through a ground temperature observation or a boring research.3. Mt.Sugorokudake and Mt.MinamidakeThe air and ground temperatures were observed at the wind-blown sites near the summits of Mt.Sugorokudake (2,860m a.s.l.) and Mt.Minamidake (3,033m a.s.l.). There is a difference in the altitude between the both mountains, but the conspicuous difference in the air temperature condition is not recognized between the two. The air temperatures indicated that there is a permafrost in the wind-blown bare ground near the summits. Permafrost, however, did not recognized through the ground temperature observation on Mt.Sugorokudake. On Mt.Minamidake, more observation and research are required to confirm that there is a permafrost or not. Less
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高橋伸幸: "北海道南西部,羊蹄山高山帯における1994年秋季〜1996年春季の気温観測" 北海学園大学学園論集. 92号. 1-18 (1997)
高桥伸之:“北海道西南部羊蹄山高山地带1994年秋季至1996年春季的温度观测”北海学园大学学报第92. 1-18号(1997年)。
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高橋伸幸: "飛騨山脈双六岳高山帯における1994年秋季〜1996年春季の気温・地温観測" 北海学園大学学園論集. 90号. 115-127 (1996)
高桥伸之:“飞驒山脉双六岳高山地带1994年秋季至1996年春季气温和土壤温度的观测”北海学园大学学报第90期。115-127(1996年)。
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高橋伸幸: "北海道南西部、羊蹄山高山帯における1994年秋季〜1996年春季の気温観測" 北海学園大学学園論集. 第92号. ((発表予定)1997)
高桥伸之:“北海道西南部羊蹄山高山地带1994年秋季至1996年春季的温度观测”北海学园大学学报第92期。((待出版)1997年)
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TAKAHASHI,N.AND SATO,K.: "SUMMER GROUND TEMPERATURE CONDITIONS IN THE PINUS PUMILA COMMUNITY IN THE ALPINE ZONE OF THE DAISETSUZAN MOUNTAINS" GEOGRAPHICAL REVIEW OF JAPAN. 69A. 693-705 (1996)
高桥,N. 和佐藤,K.:“大雪山高山地区普米拉松群落的夏季地面温度条件”日本地理评论。
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TAKAHASHI,N.: "AIR TEMPERATURE CONDITIONS AT THE FOREST LINE LEVEL ON THE EASTERN SIDE OF THE NORTHERN DAISETSUZAN MOUNTAINS, CENTRAL HOKKAIDO, NORTHERN JAPAN" GEOGRAPHICAL REVIEW OF JAPAN. 71A. 588-599 (1998)
高桥,N.:“日本北部北海道中部大雪山北部森林线水平的空气温度”日本地理评论。
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