首页> 外文期刊>日本草地学会誌 >Ecological consideration for the distribution of natural grassland vegetation zones in relation to the climate and climate change in Japan. 4. The effects of global warming on the natural grassland vegetation in Japan
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Ecological consideration for the distribution of natural grassland vegetation zones in relation to the climate and climate change in Japan. 4. The effects of global warming on the natural grassland vegetation in Japan

机译:日本气候和气候变化对天然草地植被带分布的生态影响。 4.全球变暖对日本天然草原植被的影响

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摘要

We predicted how natural grassland vegetation in Japan will change in response to the global warming. We divided the Japanese grassland vegetations into four vegetation zones ; the subarctic, the cool-temperate, the warm-temperate and the subtropical grassland vegetation zones according to Zoysia japonica-type grassland and Z. tenuifolia-type grassland, Sasa-type grassland and Pleioblastus chino-type grassland. According to our results, the distribution in natural grassland vegetation will not change within the next 50 to 60 years. After that, however, the temperature will rise so rapidly and the maximum snow depth will decrease rapidly. One hundred years from now later, the temperature will rise around 3.3 to 3.8 degrees Celsius and the natural vegetation zones in Japan will greatly change. In Hokkaido, the subarctic natural grassland vegetation zone in lowland area will disappear. And the warm-temperate natural grassland vegetation zone in the lowland will spread to Shimokita and Tsugaru peninsula, the northernmost of the mainland, and will also appear even in the plains around Abashiri and Tokachi district in Hokkaido. The cool-temperate natural grassland vegetation zone in Shikoku, Kyusyu and Kii peninsula were predicted to have mostly disappear. On the other hand, the subtropical natural grassland vegetation zones in lowlands of Kyusyu and Shikoku were predicted to spread over Boso peninsula, the south part of Kanto, and the southern Izu peninsula.
机译:我们预测了日本的天然草原植被将随着全球变暖而变化。我们将日本草地植被分为四个植被带;根据结缕草型草原和Z. tenuifolia型草原,Sasa型草原和Pleioblastus chino型草原划分为亚北极,冷温带,温带和亚热带草原植被带。根据我们的结果,在未来50至60年内,天然草地植被的分布不会改变。但是,此后温度将迅速上升,最大积雪深度将迅速下降。从现在开始的一百年后,温度将升高约3.3到3.8摄氏度,日本的自然植被区将发生巨大变化。在北海道,低地地区的北极北极天然草地植被带将消失。低地的温带天然草地植被带将蔓延到大陆最北端的下北田和津轻半岛,甚至出现在北海道网走地区和十胜地区附近的平原上。据预测,四国,九州和纪伊半岛的温带天然草地植被带大部分消失了。另一方面,九州和四国低地的亚热带天然草地植被带预计会扩散到Boso半岛,关东南部和伊豆半岛南部。

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