| 中国耕地变化区的气候背景对比分析 |
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| 引用本文： | 石瑞香,杨小唤.中国耕地变化区的气候背景对比分析[J].地球信息科学,2010,12(3):309-314. |
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| 作者姓名： | 石瑞香 杨小唤 |
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| 作者单位： | 中国科学院地理科学与资源研究所资源与环境信息系统国家重点实验室, 北京 100101 |
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| 基金项目： | 中国科学院知识创新工程重大项目（KSCX1-YW-09-01） |
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| 摘 要： | 研究我国耕地变化区的气候背景,对于了解耕地资源的生产能力,评价耕地占补平衡政策的实施效果,实现耕地资源保护和粮食安全等具有重要意义。本文在分析全国耕地空间变化的基础上,从年平均气温、年降水量和日照时数三个方面,研究耕地增加区和减少区的气候背景,并将其进行比较和分析,以期为国家保护耕地资源和发展农业生产等提供建议。研究结果表明,20世纪80年代末至2008年4个时段,耕地减少区比耕地增加区的年平均气温高0.45~1.05℃,年降水量高56.77~79.59mm,年日照时数少45.80~98.83h。耕地显著减少区比耕地显著增加区的年平均气温高0.81~1.85℃,年降水量高85.69~305.26mm,年日照时数少86.96~207.85h。在四个时段中,我国耕地重心逐渐北移且海拔升高。若海拔高度不变,耕地增加区比耕地减少区北移0.5-1个纬度,耕地显著增加区比耕地显著减少区北移1-2个纬度;若纬度不变,耕地增加区比耕地减少区,海拔升高100~200m,耕地显著增加区比耕地显著减少区,海拔升高150~350m。随年份增加,耕地增加区和显著增加区与耕地减少区和显著减少区在水分条件上的差别越来越大。这些结论对于研究我国粮食生产能力、评价耕地占补平衡、调整产业布局等具有重要意义。
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| 关 键 词： | 中国 耕地 变化 气候背景 |
| 收稿时间： | 2010-01-28; |
Research on the Climate Background in Arable Land Changed Areas of China |
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| SHI Ruixiang,YANG Xiaohuan.Research on the Climate Background in Arable Land Changed Areas of China[J].Geo-information Science,2010,12(3):309-314. |
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| Authors: | SHI Ruixiang YANG Xiaohuan |
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| Institution: | State Key Laboratory of Resources and Environment Information System,Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing 100101,China |
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| Abstract: | It was very important to learn the climate background in arable land changed areas of China then to estimate food production,to evaluate the balance of arable land quantity and quality,and to put in practice arable land protection and food security.In this paper,the arable land changed areas were firstly analyzed.Next,annual mean temperature,precipitation and sunshine hours were chosen to analyze the climate conditions in arable land changed areas so as to provide suggestions on land protection and economic development.The results showed that annual mean temperature,precipitation and sunshine hours in arable land decreased areas were 0.45-1.05℃ higher,56.77-79.59mm more and 45.80-98.83h less than arable land increased areas during the four periods from the end of 1980s to 2008.While annual mean temperature,precipitation and sunshine hours in areas with significant arable land reduction were 0.81-1.85℃ higher,85.69-305.26mm more and 86.96-207.85h less than those with significant arable land increase.The core part of China＇s arable land was gradually moving upward/northward from the end of 1980s to 2008.According to altitude,the arable land increased areas seemed to be about 0.5-1° more northward than the decreased areas,while the significantly increased areas seemed to be about 1-2° more northward than the significantly decreased areas.Otherwise,according to latitude,the arable land increased areas seemed to be about 100-200 meters higher than the decreased areas,while the significantly increased areas seemed to be about 150-350 meters higher than the significantly decreased areas.The difference in precipitation became more and more significant between the arable land decreased area and the increased area as time went on from the end of 1980s to 2008.These conclusions are important help for us to learn grain production,to evaluate the balance of arable land quantity and quality,and to readjust industrial layout in China. |
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| Keywords: | China arable land change climate background |
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