Spatiotemporal characteristics and patterns of the global cultivated land since the 1980s

被引:0
作者
Zhang L. [1 ]
Yao Z. [1 ]
Tang S. [2 ]
Li X. [1 ]
Hao T. [1 ]
机构
[1] Key Laboratory of Remote Sensing Monitoring of Geographic Environment, College of Heilongjiang, Harbin Normal University, Harbin
[2] Key Laboratory of Radiometric Calibration and Validation for Environmental Satellites, National Satellite Meteorological Center, CMA, Beijing
来源
Dili Xuebao/Acta Geographica Sinica | 2017年 / 72卷 / 07期
基金
中国国家自然科学基金;
关键词
Cultivated land; Global land; Spatiotemporal characteristics; Spatiotemporal patterns; use change;
D O I
10.11821/dlxb201707009
中图分类号
学科分类号
摘要
Based on the global land use/cover data from 1982 to 2011(CG-LTDR), this paper analyzes the characteristics and spatial patterns of cultivated land change since the 1980s. The results are summarized as follows: (1) Since the 1980s, the world's arable land has increased by 528.768 × 104 km2 with a rate of 7.920 × 104 km2/a, although the trend is not statistically significant. The world's arable land grew fastest in the 1980s. Areas of cultivated land in North America, South America and Oceania increased by 170. 854×104 km2, 107. 890×104 km2 and 186.492×104 km2, respectively since the 1980s, showing significant trends with rates of 7.236× 104 km2/a, 2.780×104 km2/a and 3.758×104 km2/a, respectively. Areas in Asia, Europe and Africa decreased by 23.769×104, 4.035×104, 86.76×104 km2, with rates of-5.641×104 km2/a, -0.813× 104 km2/a and -0.595×104 km2/a, respectively. Only Asia revealed a significant reduction trend. (2) Since the 1980s, the increased cultivated land in the world has been mainly converted from grasslands and forests, accounting for 53.536% and 26.148%, respectively. Newly cultivated land was mostly distributed in southern and central Africa, eastern and northern Australia, southeastern South America, central US, Alaska, central Canada, western Russia, northern Finland and northern Mongolia. Among these regions, Botswana in southern Africa has the highest proportion of increased arable land, an increase of 80%-90%. (3) Since the 1980s, a total of 1071.946 × 104 km2 of arable land has been converted to other types of land, mostly grasslands and forests that account for 57.482% and 36.000%, respectively. Global reduction of arable land was mainly found in southern and central Africa, central South America, southern Russia and southern Europe (Bulgaria, Romania, Serbia and Hungary). Among these regions, southern Africa experienced the highest reduction of 60%. (4) Cultivated lands in all continents had a trend of expanding to high latitudes, and most countries in the world are characterized by expansion of newly cultivated land and reduction of cultivated land in the earlier period. © 2017, Science Press. All right reserved.
引用
收藏
页码:1235 / 1247
页数:12
相关论文
共 31 条
  • [1] Ramankutty N., Delire C., Snyder P., Feedbacks between agriculture and climate: An illustration of the potential unintended consequences of human land use activities, Global and Planetary Change, 54, 1-2, pp. 79-93, (2006)
  • [2] Tian H.Q., Chen G.S., Zhang C.H.I., Et al., Century-scale responses of ecosystem carbon storage and flux to multiple environmental changes in the southern United States, Ecosystems, 15, 4, pp. 674-694, (2012)
  • [3] Terrestrial carbon balance in tropical Asia: Contribution from cropland expansion and land management, Global & Planetary Change, 100, 1, pp. 85-98, (2013)
  • [4] He F., Li M., Liu H., Reconstruction of cropland area at Lu scale and its spatialtemporal characteristics in the Northern Song Dynasty, Acta Geographica Sinica, 71, 11, pp. 1967-1978, (2016)
  • [5] Chhabra A., Geist H., Houghton R.A., Et al., Multiple Impacts of Land-Use/Cover ChangeLand-Use and Land-Cover Change, pp. 71-116, (2006)
  • [6] Liu J., Kuang W., Zhang Z., Et al., Spatiotemporal characteristics, patterns and causes of land use changes in China since the late 1980s, Acta Geographica Sinica, 69, 1, pp. 3-14, (2014)
  • [7] Shi P., Wang J., Chen J., Et al., The future of human-environment interaction research in geography: Lessons from the 6th Open Meeting of IHDP, Acta Geographica Sinica, 61, 2, pp. 115-126, (2006)
  • [8] Findell K.L., Pitman A.J., England M.H., Et al., Regional and global impacts of land cover change and sea surface temperature anomalies, Journal of Climate, 22, 12, pp. 3248-3269, (2009)
  • [9] Forster P., Ramaswamy V., Artaxo P., Et al., Changes in atmospheric constituents and in radiative forcing, Climate Change 2007: The Physical Science Basis: Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, (2007)
  • [10] Ramankutty N., Achard F., Alves D., Et al., Global changes in land cover, IHDP Newsletter, 3, pp. 4-5, (2005)