贺俊[1] Smith S D, Travis E H, Ziter S F, et al. Elevated CO2 increases productivity and invasive species success in an aridecosystem[J]. Nature,2000,408:79-81.
[2] 张新时,周广胜,高琼,等.全球变化研究中的中国东北森林-草原陆地样带(NECT)[J].地学前缘,1997,4(1/2):145-151.
[3] Law B E, Falge E, Gu L, et al. Environmental controls over carbondioxide and water vapor exchange of terrestrial vegetation[J]. Agricuhuraland Forest Meteorology,2002,l13(1/4):97-120.
[4] Parton W J, Ojima D S, Schimel D S. Environmental change in grasslands: Assessment using models[J].Climatic Change,1994,28 (1):111-141.
[5] 李英年,赵新全,汪诗平,等.黄河源区气候温暖化及其对植被生产力影响评价[J].中国农业气象,2007,4(28):374-377.
[6] 胡隐樵.黑河实验(HEIFE)能量平衡和水汽输送研究进展[J].地球科学进展,1994,9(4):32-34.
[7] 张强,曹晓彦.敦煌地区荒漠戈壁地表热量和辐射平衡特征的研究[J].大气科学,2003,27(2):245-254.
[8] Brutsaert W. Evaporation into the atmosphere: theory, history, and applications[M].USA: Kluwer Academic Publishers,1982:299.
[9] 王宗明,张柏.区域尺度作物生产力对全球变化响应的研究进展及展望[J].中国农业气象,2005,26(2):112-115.
[10] Yatagai A, Yasunari T. Trends and decadal- scale fluctuations of surface air temperature and precipitation over China and Mongolia during the recent 40 year period (1951- 1990) [J].Journal of the Meteorological Society of Japan,1994,72(6):937-957.
[11] Yatagai A, Yasunari T. interranual variations of summer precipitation in the arid/semi· arid regions in China and Mongolia: their regionality and relation to the Asian summer monsoon: Special edition on HEIFEI[J].Journal of the Meteorological Society of Japan,1995,73(5):909-923.
[12] Sugita M, Asanuma J, Tsujimura M, et al. An overview of the rangelands atmosphere- hydrosphere- biosphere interaction study experiment in northeastern Asia (RAISE) [J].Journal of Hydrology, 2007,333(1):3-20.
[13] 季国良,邹基玲,吕兰芝.藏北高原地面加热场的季节变化[J].高原气象,1997,16(1):1-9.
[14] 季国良,姚兰昌,袁福茂,等.1982年西藏高原高寒草甸能量平衡闭合研究气加热场特征[J].中国科学(B辑),1986,5(2):214-224.
[15] 张宇,吕世华,陈世强,等.绿洲边缘夏季小气候特征及地表辐射与能量平衡特征分析[J].高原气象,2005,24(4):527-533.
[16] Massman W J, Lee X. Eddy covariance flux corrections and uncertainties in long-term studies of carbon and energy exchanges [J].Agricultural and Forest Meteorology,2002,113(1/4):121-144.
[17] 王修信,刘馨,陈声海,等.半干旱地区草地水热通量与环境因素及相关性研究[J].应用基础与工程科学学报,2008,16(8):770-777.
[18] 李正泉,于贵瑞,温学发,等.中国通量观测网络(China FLUX)能量平衡闭合状况的评价[J].中国科学(D辑),2004,34(增刊 II):46-56.
[19] Wilson K A, Goldstein A, Falge E, et al. Energy balance closure at FLUXNET sites[J].Agricultural and Forest Meteorology,2002,113 (14):223-243.
[20] 倪攀,金昌杰,王安志,等.半干旱风沙草原区草地潜热通量的特征[J].中国农业气象,2008,29(4):427-431.
[21] 关德新,吴家兵,于贵瑞,等.气象条件对长白山阔叶红松林 CO2通量的影响[J].中国科学 D辑:地球科学,2004,34(增Ⅱ):103-108. 杰 .典型草原区草地潜热通量特征.中国农学通报 ,2014,30(第26期9月): 195-199
|