Bian Lingen, Gao Zhiqiu, Lu Longhua, et al. Measurements of CO2 fluxes over two different underlying surfaces in an agricultural ecosystemover lower basins of the Yangtze. J Appl Meteor Sci, 2005, 16(6): 828-834.
Citation: Bian Lingen, Gao Zhiqiu, Lu Longhua, et al. Measurements of CO2 fluxes over two different underlying surfaces in an agricultural ecosystemover lower basins of the Yangtze. J Appl Meteor Sci, 2005, 16(6): 828-834.

MEASUREMENTS OF CO2 FLUXES OVER TWO DIFFERENT UNDERLYING SURFACES IN AN AGRICULTURAL ECOSYSTEMOVER LOWER BASINS OF THE YANGTZE

  • Received Date: 2005-04-07
  • Rev Recd Date: 2005-06-15
  • Publish Date: 2005-12-31
  • In order to better understand the regional climate change, it is necessary to quantify the CO2 flux over agricultural ecosystem. CO2 fluxes are collected directly by using eddy covariance over a rice paddy in the summer of 2001 and over an inhomogeneous crop surface in the summer of 2002 respectively. On average, daytime absorption and nighttime release of CO2 flux by the rice paddy are 55.16 g· m-2·d-1and 14.19 g·m-2·d-1, and by the inhomogeneous crop surface are 22.67 g·m-2·d-1and 12.40 g·m-2·d-1. Rice paddy and the inhomogeneous crop surface are sinks of atmospheric CO2. China is a great agricultural country, increasing the area of rice paddy will help CO2 deposition, and will slow down increase of atmospheric CO2 and greenhouse effect. In addition, the relationship between daytime absorption of CO2 flux and Photosynthetically-active radiation is investigated for the rice paddy, and resulting a negative correlation. Hopefully the results obtained in present work will provide an important basis for numerical modeling of CO2 flux between atmosphere and land。
  • [1]
    周秀骥,吴国雄.中国气象事业发展战略研究.重大科学技术问题卷.北京:气象出版社,2004.101。
    [2]
    宋长春.湿地生态系统碳循环研究进展.地理科学,2003,23(5):622-628。 http://www.cnki.com.cn/Article/CJFDTOTAL-DLKX200305017.htm
    [3]
    Miyata A,Leuning R,Thomas O,et al.Carbon dioxide and methane fluxes from an intermittently flooded paddy field.Agricultural and Forest Meteorology,2000,102:287-303。 doi:  10.1016/S0168-1923(00)00092-7
    [4]
    Katul G G,Leuning R,Kim J.Estimating CO2 source/sink distributions within a rice canopy using higher-order closure models.Boundary-Layer Meteorology,2001,98:103-125。 doi:  10.1023/A:1018730118183
    [5]
    Campbell C S,Heilman J L,McInnes K J,et al.Diel and seasonal variation in CO2 flux of irrigated rice.Agricultural and Forest Meteorology,2001,108:15-27。 doi:  10.1016/S0168-1923(01)00225-8
    [6]
    Gao Z,Chae N,Kim J,et al.Modeling of surface energy partitioning,surface temperature and soil wetness in the Tibetan prairie using the Simple Biosphere Model 2 (SiB2).J Geophys Res,2004,109:D06102,dio:10.1029/2003JD004089。 http://www.oalib.com/references/19068698
    [7]
    高志球,卞林根,陆龙骅,等.利用SiB2模拟水稻不同生长期稻田表面的能量和CO2通量.应用气象学报,2004,15(2):129-140。 http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20040218&flag=1
    [8]
    Lu Longhua,Cheng Yanjie,Bian Lingen,et al.A study the turbulence fluxes transfer of C02,sensible heat and latent heat for the surface layer over the typical rice field,Yangtdz Delta.Chinese Journal of Geophysics,2003,46(6):978-987。 http://cn.bing.com/academic/profile?id=5542dfe3918c7ba5e6ee0802cf6d8cec&encoded=0&v=paper_preview&mkt=zh-cn
    [9]
    周秀骥.长江三角洲低层大气与生态系统相互作用研究.北京:气象出版社,2004.166-169。
    [10]
    Gao Z Q,Bian L G,Zhou X J.Measurements of turbulent transfer in the near-surface layer over a rice paddy in China.J Geophys Res,2003,108(D13):4387,dio:10.1029/2002JD002779。 https://www.researchgate.net/publication/51997454_Measurements_of_turbulent_transfer_in_the_near-surface_layer_over_a_rice_paddy_in_China
    [11]
    Leuning R, King K M.Comparison of eddy-covariance measurements of CO2 fluxes by open-and closed-path CO2 analysers.Boundary-Layer Meteorology , 1992 , 59 :297-11。
  • 加载中
  • -->

Catalog

    Figures(5)  / Tables(1)

    Article views (2987) PDF downloads(1500) Cited by()
    • Received : 2005-04-07
    • Accepted : 2005-06-15
    • Published : 2005-12-31

    /

    DownLoad:  Full-Size Img  PowerPoint