气候变化条件下四川盆地草耕资源大区高覆盖度草地适宜区演替及机制

    Study on succession and mechanism of suitable area of high coverage grassland in Sichuan Basin under climate change

    • 摘要: 四川盆地是国家青藏高原生态屏障区的重要组成部分,其高覆盖度草地是人类生存和发展的重要自然资源,研究气候变化条件下的演替及机制,有助于合理开发利用草地资源,开展保护与修复工作,提高草地生态系统功能和稳定性。本研究基于中国多时期土地利用遥感监测数据,获得四川盆地草耕资源大区高覆盖度草地的分布数据,选用33个与气候、地形、土壤相关的环境变量,采用最大熵模型(MaxEnt)进行四川盆地高覆盖度草地现代与未来气候条件下的生态适宜性评价。结果表明:(1)四川盆地草耕资源大区高覆盖度草地适宜区面积约为52.06×104 km2,中、高适宜区主要分布在汉中盆地北部地区。(2)昼夜温差月均值、最暖季度降水量、最冷月份最低温度、降水量季节性变化是主要的影响生态因子,贡献率分别为34.0%,21.8%、14.1%和13.5%;(3)适宜区在未来时期不同气候情景下都有所增加,分布格局与历史时期总体表现较为一致。新增适宜区在汉中盆地南、北部均有分布,而保留适宜区和丧失适宜区主要集中在汉中盆地北部地区。2050s-SSP2-4.5情景下潜在适宜区面积最大,表明中等减排路径对于高覆盖度草地的发展比较有利。

       

      Abstract: The Sichuan Basin is an important part of the national ecological barrier zone of the Qinghai-Tibet Plateau, and its high-cover grassland is an important natural resource for the survival and development of human beings. The study of succession and mechanisms under climate change conditions can help to rationally develop and utilise grassland resources, carry out conservation and restoration work, and improve the function and stability of grassland ecosystems.In this study, we obtained the distribution data of high-cover grassland in the Sichuan Basin based on the remote sensing monitoring data of land use in China over a period of time, selected 33 environmental variables related to climate, topography and soil, and used the Maximum Entropy Model (MaxEnt) to evaluate the ecological suitability of high-cover grassland in the Sichuan Basin under the modern and future climatic conditions. The results showed that: (1) the area of high-cover grassland suitability in the Sichuan Basin grass ploughing resource area is about 52.06×104 km2, and the middle and high suitability areas are mainly distributed in the northern part of Hanzhong Basin. (2) Monthly mean diurnal temperature difference, precipitation in the warmest season, minimum temperature in the coldest month, and seasonal variation of precipitation are the main ecological factors, with contribution rates of 34.0%, 21.8%, 14.1%, and 13.5%, respectively. (3) Suitable zones will increase in the future under different climatic scenarios, and the distribution pattern is more in line with the overall performance in the historical period. The new suitable areas were distributed in the south and north of Hanzhong Basin, while the retained and lost suitable areas were mainly concentrated in the north of Hanzhong Basin. 2050s-SSP2-4.5 scenario had the largest area of potential suitable areas, which indicated that the medium emission reduction pathway was more favourable for the development of high-cover grassland.

       

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