DRY-AIR BOUNDARY-CONDITIONS FOR CORRECTION OF EDDY FLUX MEASUREMENTS

被引:14
作者
SMITH, SD
JONES, EP
机构
[1] Atlantic Oceanographic Laboratory, Bedford Institute of Oceanography, Dartmouth, B2Y 4A2, N.S.
关键词
D O I
10.1007/BF00117925
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
For measurements of eddy fluxes in the atmospheric boundary layer of gases (such as CO2) whose average concentration is very large compared to the fluctuations, corrections for air density fluctuations are required. With the boundary condition of no flux of dry air at the surface, the evaporation correction to eddy fluxes is 2.6 times larger than has been estimated with the boundary condition of no mass flux at all at the surface. The heat flux correction is also increased by a few per cent. © 1979 D. Reidel Publishing Co.
引用
收藏
页码:375 / 379
页数:5
相关论文
共 7 条
[1]  
Bakan S., 1978, Boundary-Layer Meteorology, V14, P597, DOI 10.1007/BF00121898
[2]  
Brook R. R., 1978, Boundary-Layer Meteorology, V15, P481, DOI 10.1007/BF00120609
[4]  
Jones E. P., 1978, Boundary-Layer Meteorology, V15, P357, DOI 10.1007/BF02652607
[5]   1ST MEASUREMENT OF SEA-AIR CO2 FLUX BY EDDY CORRELATION [J].
JONES, EP ;
SMITH, SD .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS AND ATMOSPHERES, 1977, 82 (37) :5990-5992
[6]  
Kondo J., 1975, Boundary-Layer Meteorology, V9, P91, DOI 10.1007/BF00232256
[7]  
Webb E. K., 1977, 2 AUSTR C HEAT MASS, P469