Seasonal Variations in Soil Temperature on the Alpine Tundra Community in Mt. Changbai in Northeast China : Comparison with Mt. Tateyama in Central Japan
We examined the synchronization of soil temperatures on an alpine tundra community between Mt. Changbai in northeastern China, and Mt. Tateyama in central Japan. The soil temperatures were measured at one-hour intervals for a total of 7526 recordings at both study sites, where a glacial relict plant...
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Center for Far Eastern Studies University of Toyama
2006
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ftunivtoyama:oai:toyama.repo.nii.ac.jp:00006598 2023-05-15T14:54:43+02:00 Seasonal Variations in Soil Temperature on the Alpine Tundra Community in Mt. Changbai in Northeast China : Comparison with Mt. Tateyama in Central Japan Wada Naoya Qi-Jing LIU Kawada Kunio 2006-05 application/pdf http://hdl.handle.net/10110/1168 https://toyama.repo.nii.ac.jp/?action=repository_uri&item_id=6598 https://toyama.repo.nii.ac.jp/?action=repository_action_common_download&item_id=6598&item_no=1&attribute_id=18&file_no=1 en eng Center for Far Eastern Studies University of Toyama https://toyama.repo.nii.ac.jp/?action=repository_uri&item_id=6598 http://hdl.handle.net/10110/1168 FES Far Eastern Studies, 5, 35-43(2006-05) 1347-7250 AA11693979 https://toyama.repo.nii.ac.jp/?action=repository_action_common_download&item_id=6598&item_no=1&attribute_id=18&file_no=1 Alpine tundra Arctic Oscillation Circumpolar plants Glacial relict Temperature Journal Article Article 2006 ftunivtoyama 2022-11-20T21:37:46Z We examined the synchronization of soil temperatures on an alpine tundra community between Mt. Changbai in northeastern China, and Mt. Tateyama in central Japan. The soil temperatures were measured at one-hour intervals for a total of 7526 recordings at both study sites, where a glacial relict plant Dryas octopetala var. asiatica was predominant. The hourly mean soil temperatures had high synchronization between the two mountains (r2= 0.87). After comparing soil temperatures by dividing the climate into two seasons, we found that synchronization of temperatures between the two mountains was higher in winter (r2= 0.75) than in summer (r2= 0.44). The Arctic Oscillation index, which is related to atmospheric circulation in the Northern Hemisphere, was significantly correlated with air temperature near each study site in the coldest month. Despite the difference in geographical location, a high similarity of seasonal variations in soil temperature in winter suggests that the thermal condition on the two mountains is controlled by the same air masses from higher latitudes. Keywords: Alpine tundra, Arctic Oscillation, Circumpolar plants, Glacial relict, Temperature innovation activities have a high potential to maintainable growth, this strategy alone is inadequate; entrepreneurship that involves a riskier style of management is required. Third, innovation alone carried out by venture enterprises in Japan can not contribute directly to employment creation. Rather, by combining innovation activities with market-in characteristics, enterprises are more likely to realize a surplus quickly, then achieve maintainable growth, thus indirectly contributing to employment creation. Article in Journal/Newspaper Arctic Dryas octopetala Tundra ToRepo (University of Toyama Repository) Arctic |
institution |
Open Polar |
collection |
ToRepo (University of Toyama Repository) |
op_collection_id |
ftunivtoyama |
language |
English |
topic |
Alpine tundra Arctic Oscillation Circumpolar plants Glacial relict Temperature |
spellingShingle |
Alpine tundra Arctic Oscillation Circumpolar plants Glacial relict Temperature Wada Naoya Qi-Jing LIU Kawada Kunio Seasonal Variations in Soil Temperature on the Alpine Tundra Community in Mt. Changbai in Northeast China : Comparison with Mt. Tateyama in Central Japan |
topic_facet |
Alpine tundra Arctic Oscillation Circumpolar plants Glacial relict Temperature |
description |
We examined the synchronization of soil temperatures on an alpine tundra community between Mt. Changbai in northeastern China, and Mt. Tateyama in central Japan. The soil temperatures were measured at one-hour intervals for a total of 7526 recordings at both study sites, where a glacial relict plant Dryas octopetala var. asiatica was predominant. The hourly mean soil temperatures had high synchronization between the two mountains (r2= 0.87). After comparing soil temperatures by dividing the climate into two seasons, we found that synchronization of temperatures between the two mountains was higher in winter (r2= 0.75) than in summer (r2= 0.44). The Arctic Oscillation index, which is related to atmospheric circulation in the Northern Hemisphere, was significantly correlated with air temperature near each study site in the coldest month. Despite the difference in geographical location, a high similarity of seasonal variations in soil temperature in winter suggests that the thermal condition on the two mountains is controlled by the same air masses from higher latitudes. Keywords: Alpine tundra, Arctic Oscillation, Circumpolar plants, Glacial relict, Temperature innovation activities have a high potential to maintainable growth, this strategy alone is inadequate; entrepreneurship that involves a riskier style of management is required. Third, innovation alone carried out by venture enterprises in Japan can not contribute directly to employment creation. Rather, by combining innovation activities with market-in characteristics, enterprises are more likely to realize a surplus quickly, then achieve maintainable growth, thus indirectly contributing to employment creation. |
format |
Article in Journal/Newspaper |
author |
Wada Naoya Qi-Jing LIU Kawada Kunio |
author_facet |
Wada Naoya Qi-Jing LIU Kawada Kunio |
author_sort |
Wada Naoya |
title |
Seasonal Variations in Soil Temperature on the Alpine Tundra Community in Mt. Changbai in Northeast China : Comparison with Mt. Tateyama in Central Japan |
title_short |
Seasonal Variations in Soil Temperature on the Alpine Tundra Community in Mt. Changbai in Northeast China : Comparison with Mt. Tateyama in Central Japan |
title_full |
Seasonal Variations in Soil Temperature on the Alpine Tundra Community in Mt. Changbai in Northeast China : Comparison with Mt. Tateyama in Central Japan |
title_fullStr |
Seasonal Variations in Soil Temperature on the Alpine Tundra Community in Mt. Changbai in Northeast China : Comparison with Mt. Tateyama in Central Japan |
title_full_unstemmed |
Seasonal Variations in Soil Temperature on the Alpine Tundra Community in Mt. Changbai in Northeast China : Comparison with Mt. Tateyama in Central Japan |
title_sort |
seasonal variations in soil temperature on the alpine tundra community in mt. changbai in northeast china : comparison with mt. tateyama in central japan |
publisher |
Center for Far Eastern Studies University of Toyama |
publishDate |
2006 |
url |
http://hdl.handle.net/10110/1168 https://toyama.repo.nii.ac.jp/?action=repository_uri&item_id=6598 https://toyama.repo.nii.ac.jp/?action=repository_action_common_download&item_id=6598&item_no=1&attribute_id=18&file_no=1 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Dryas octopetala Tundra |
genre_facet |
Arctic Dryas octopetala Tundra |
op_relation |
https://toyama.repo.nii.ac.jp/?action=repository_uri&item_id=6598 http://hdl.handle.net/10110/1168 FES Far Eastern Studies, 5, 35-43(2006-05) 1347-7250 AA11693979 https://toyama.repo.nii.ac.jp/?action=repository_action_common_download&item_id=6598&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766326481346101248 |