期刊文献+

Estimation of Turbulent Fluxes Using the Flux-Variance Method over an Alpine Meadow Surface in the Eastern Tibetan Plateau 被引量:11

Estimation of Turbulent Fluxes Using the Flux-Variance Method over an Alpine Meadow Surface in the Eastern Tibetan Plateau
下载PDF
导出
摘要 The flux-variance similarity relation and the vertical transfer of scalars exhibit dissimilarity over different types of surfaces, resulting in different parameterization approaches of relative transport efficiency among scalars to estimate turbulent fluxes using the flux-variance method. We investigated these issues using eddycovariance measurements over an open, homogeneous and flat grassland in the eastern Tibetan Plateau in summer under intermediate hydrological conditions during rainy season. In unstable conditions, the temperature, water vapor, and CO2 followed the flux-variance similarity relation, but did not show in precisely the same way due to different roles (active or passive) of these scalars. Similarity constants of temperature, water vapor and CO2 were found to be 1.12, 1.19 and 1.17, respectively. Heat transportation was more eft% cient than water vapor and CO2. Based on the estimated sensible heat flux, five parameterization methods of relative transport efficiency of heat to water vapor and CO2 were examined to estimate latent heat and CO2 fluxes. The strategy of local determination of flux-variance similarity relation is recommended for the estimation of latent heat and CO2 fluxes. This approach is better for representing the averaged relative transport efficiency, and technically easier to apply, compared to other more complex ones. The flux-variance similarity relation and the vertical transfer of scalars exhibit dissimilarity over different types of surfaces, resulting in different parameterization approaches of relative transport efficiency among scalars to estimate turbulent fluxes using the flux-variance method. We investigated these issues using eddycovariance measurements over an open, homogeneous and flat grassland in the eastern Tibetan Plateau in summer under intermediate hydrological conditions during rainy season. In unstable conditions, the temperature, water vapor, and CO2 followed the flux-variance similarity relation, but did not show in precisely the same way due to different roles (active or passive) of these scalars. Similarity constants of temperature, water vapor and CO2 were found to be 1.12, 1.19 and 1.17, respectively. Heat transportation was more eft% cient than water vapor and CO2. Based on the estimated sensible heat flux, five parameterization methods of relative transport efficiency of heat to water vapor and CO2 were examined to estimate latent heat and CO2 fluxes. The strategy of local determination of flux-variance similarity relation is recommended for the estimation of latent heat and CO2 fluxes. This approach is better for representing the averaged relative transport efficiency, and technically easier to apply, compared to other more complex ones.
出处 《Advances in Atmospheric Sciences》 SCIE CAS CSCD 2013年第2期411-424,共14页 大气科学进展(英文版)
基金 funding frown the Chinese National Key Programme for Developing Basic Sciences,the National Natural Science Foundation of China,the Key Program of the Chinese Academy of Sciences,the National Natural Science Foundation of China,the Foundation for Excellent Young Scholars of CAREERI
关键词 flux-variance method relative transfer efficiency eddy-covariance method homogeneous landsurface turbulent flux flux-variance method, relative transfer efficiency, eddy-covariance method, homogeneous landsurface, turbulent flux
  • 相关文献

参考文献1

二级参考文献33

  • 1Adreas,E.L.,R.J.Hill,J.R.Gosz,D.I.Moore,W.D.Otto,and A.D.Sarma,1998:Statistics of surfacelayer turbulence over terrain with metre-scale heterogeneity.Bound.-Layer Meteor.,86,379-408.
  • 2Asanuma,J.,and W.Brutsaert,1999:Turbulence variance characteristics of temperature and humidity in the unstable atmospheric surface layer above a variable pine forest.Water Resour.Res.,35(2),515-521.
  • 3Bian,L.,Z.Gao,X.Xu,L.Lu,and Y.Cheng,2002:Measurements of turbulence transfer in the near surface layer over the southeastern Tibetan Plateau.Bound.-Layer Meteor.,102,281-300.
  • 4Brutsaert,W.,and M.Sugita,1990:The extent of the unstable Monin-Obukhov layer for temperature and humidity above complex hilly grassland.Bound.-Layer Meteor.,51,383-400.
  • 5De Bruin,H.A.R.,1982:The energy balance of the earth's surface:A practical approach.Wettenschappelijk Rapport W.R.82-1.Koninklijk Nederlands Meteoroligisch Instituut de Bilt,307pp.
  • 6De Bruin,H.A.R.,N.Bink,and L.J.M.Kroon,1991:Flux in the surface layer under advective conditions,in Workshop on Land Surface Evaporation,Measurement and Parameterization,T.J.Schmugge,and J.C.Andre,Eds.,Springer-Verlag,New York,157-169.
  • 7De Bruim,H.A.R.,W.Kohsiek,and J.J.M.Van Den Hurk,1993:A verification of some methods to determine the fluxes of momentum,sensible heat and water vapor using standard deviation and structure parameter of scalar meteorological quantities.Bound.-Layer Meteor.,63,231-257.
  • 8Foken,T.,and B.Wichura,1996:Tools for quality assessment of surface-based flux measurements.Agricultural and Forest Meteorology,78,83-105.
  • 9Gao,Z.,L.Bian,and X.Zhou,2003:Measurements of turbulent transfer in the near-surface layer over a rice paddy in China.J.Geophys.Res.,108(D13),4387,doi:10.1029/2002JD002779.
  • 10Gao,Z.,N.Chae,J.Kim,J.Hong,T.Choi,and H.Lee,2004:Modeling of surface energy partitioning,surface temperature and soil wetness in the Tibetan prairie using the Simple Biosphere Model 2 (SiB2).J.Geophys.Res.,109,D06102,dio:10.1029/2003JD004089.

共引文献8

同被引文献148

引证文献11

二级引证文献39

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部