Surface roughness length dynamic over several different surfaces and its effects on modeling fluxes

被引:2
|
作者
Yanlian Zhou
Xiaomin Sun
Zhilin Zhu
Renhua Zhang
Jing Tian
Yunfen Liu
Dexin Guan
Guofu Yuan
机构
[1] Chinese Academy of Sciences,Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research
[2] Graduate University of the Chinese Academy of Sciences,Institute of Applied Ecology
[3] Chinese Academy of Sciences,undefined
关键词
ChinaFLUX; surface roughness length; dynamic; spatial heterogeneity; Yucheng Experimental Station; Qianyanzhou Experimental Station; Changbai Mountains Experimental Station;
D O I
暂无
中图分类号
学科分类号
摘要
Roughness length and zero-plane displacement over three typical surfaces were calculated iteratively by least-square method, which are Yucheng Experimental Station for agriculture surfaces, Qianyanzhou Experimental Station for complex and undulant surfaces, and Changbai Mountains Experimental Station for forest surfaces. On the basis of roughness length dynamic, the effects of roughness length dynamic on fluxes were analyzed with SEBS model. The results indicate that, aerodynamic roughness length changes with vegetation conditions (such as vegetation height, LAI), wind speed, friction velocity and some other factors. In Yucheng and Changbai Mountains Experimental Station, aerodynamic roughness length over the fetch of flux tower changes with vegetation height and LAI obviously, that is, with the increase of LAI, roughness length increases to the peak value firstly, and then decreases. In Qianyanzhou Experimental Station, LAI changes slightly, so the relationship between roughness length and LAI is not obvious. The aerodynamic roughness length of Yucheng and Changbai Mountains Experimental Station changes slightly with wind direction, while aerodynamic roughness length of Qianyanzhou Experimental Station changes obviously with wind direction. The reason for that is the terrain in Yucheng and Changbai Mountains Experimental Station is relatively flat, while in Qianyanzhou Experimental Station the terrain is very undulant and heterogeneous. With the increase of wind speed, aerodynamic roughness length of Yucheng Experimental Station changes slightly, while it decreases obviously in Qianyanzhou Experimental Station and Changbai Mountains Experimental Station. Roughness length dynamic takes great effects on fluxes calculation, and the effects are analyzed by SEBS model. By comparing 1 day averaged roughness length in Yucheng Experimental Station and 5 day averaged roughness length of Qianyanzhou and Changbai Mountains Experimental Station with roughness length parameter chosen by the model, the effects of roughness length dynamic on flux calculation is analyzed. The maximum effect of roughness length dynamic on sensible heat flux is 2.726%, 33.802% and 18.105%, in Yucheng, Qianyanzhou, and Changbai Mountains experimental stations, respectively.
引用
收藏
页码:262 / 272
页数:10
相关论文
共 50 条
  • [1] Surface roughness length dynamic over several different surfaces and its effects on modeling fluxes
    ZHOU Yanlian SUN Xiaomin ZHU Zhilin ZHANG Renhua TIAN Jing LIU Yunfen GUAN Dexin YUAN Guofu Key Laboratory of Ecosystem Network Observation and Modeling Institute of Geographic Sciences and Natural Resources Research Chinese Academy of Sciences Beijing China
    Graduate University of the Chinese Academy of Sciences Beijing China
    Institute of Applied Ecology Chinese Academy of Sciences Shenyang China
    ScienceinChina(SeriesD:EarthSciences), 2006, (SeriesD:EarthSciences) : 262 - 272
  • [2] Surface roughness length dynamic over several different surfaces and its effects on modeling fluxes
    Zhou Yanlian
    Sun Xiaomin
    Zhu Zhilin
    Zhang Renhua
    Tian Jing
    Liu Yunfen
    Guan Dexin
    Yuan Guofu
    SCIENCE IN CHINA SERIES D-EARTH SCIENCES, 2006, 49 (Suppl 2): : 262 - 272
  • [3] Surface roughness length dynamic over several different surfaces and its effects on modeling fluxes
    ZHOU Yanlian
    Graduate University of the Chinese Academy of Sciences
    Institute of Applied Ecology
    Science China Earth Sciences, 2006, (S2) : 262 - 272
  • [4] The behaviour of the roughness length for temperature over heterogeneous surfaces
    Malhi, Y
    QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1996, 122 (533) : 1095 - 1125
  • [5] Roughness analysis for textured surfaces over several orders of magnitudes
    Vepsalainen, Laura
    Stenberg, Petri
    Paakkonen, Pertti
    Kuittinen, Markku
    Suvanto, Mika
    Pakkanen, Tapani A.
    APPLIED SURFACE SCIENCE, 2013, 284 : 222 - 228
  • [6] Effects of uncertainties in universal functions, roughness length, and displacement height on the calculation of surface layer fluxes
    Weidinger, T
    Pinto, J
    Horváth, L
    METEOROLOGISCHE ZEITSCHRIFT, 2000, 9 (03) : 139 - 154
  • [7] Length-Scale Similarity of Turbulent Organized Structures over Surfaces with Different Roughness Types
    Takimoto, Hiroshi
    Inagaki, Atsushi
    Kanda, Manabu
    Sato, Ayumu
    Michioka, Takenobu
    BOUNDARY-LAYER METEOROLOGY, 2013, 147 (02) : 217 - 236
  • [8] Length-Scale Similarity of Turbulent Organized Structures over Surfaces with Different Roughness Types
    Hiroshi Takimoto
    Atsushi Inagaki
    Manabu Kanda
    Ayumu Sato
    Takenobu Michioka
    Boundary-Layer Meteorology, 2013, 147 : 217 - 236
  • [9] Roughness Length of Water Vapor over Land Surfaces and Its Influence on Latent Heat Flux
    Park, Sang-Jong
    Park, Soon-Ung
    Ho, Chang-Hoi
    TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES, 2010, 21 (05): : 855 - 867
  • [10] Roughness of fault surfaces over nine decades of length scales
    Candela, Thibault
    Renard, Francois
    Klinger, Yann
    Mair, Karen
    Schmittbuhl, Jean
    Brodsky, Emily E.
    JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2012, 117