[1]. Ma Jianyong, Shugart H., Yan X., Cao C., Wu S. Fang J. Evaluating carbon fluxes of global forest ecosystems by using an individual tree-based model FORCCHN. Science of the Total Environment , 2017, 586: 939-951 [2]. Ma Jianyong, Yan X., Hu S., Guo Y. Can monthly precipitation interpolation error be reduced by adding periphery climate stations? A case study in China’s land border areas. Journal of Water and Climate Change, 2017, 8(1): 102-113 [3]. Ma Jianyong, Yan X., Dong W., Chou J. Gross primary production of global forest ecosystem has been overestimated. Scientific Reports, 2015, 5: 10820 [4]. Ma Jianyong, Dong W., Wei Z., Yan X. Evaluating daily surface maximum temperature interpolation error by adding climate stations near border areas over China. International Journal of Climatology, 2015, 35: 2798-2808. [5]. 马建勇, 谷晓平, 廖留峰. 21世纪贵州省10oC热量资源对气候变化的响应. 中国农业气象, 2014, 35 (2)：128-134 [6] 马建勇, 谷晓平, 黄玫, 于飞. 近50年贵州净生态系统生产力时空分布特征. 生态环境学报, 2013, 22 (9)：1462-1470 [7] 马建勇, 潘婕, 许吟隆*, 姜江. SRES A1B情景下东北地区未来干旱趋势预估. 干旱区研究，2013, 30 (2)：329-335 [8] 马建勇, 许吟隆*. 东北地区作物生长季干旱时空分布特征及其环流背景. 中国农业气象, 2013, 34 (1)：81-87 [9] 马建勇, 许吟隆*, 潘婕. 东北地区农业气象灾害的趋势变化及其对粮食产量的影响. 中国农业气象, 2012, 33 (2)：283-288 |
