Regional heat flux over the NOPEX area estimated from the evolution of the mixed-layer

被引:30
作者
Gryning, SE [1 ]
Batchvarova, E
机构
[1] Riso Natl Lab, DK-4000 Roskilde, Denmark
[2] Bulgarian Acad Sci, Natl Inst Meteorol & Hydrol, BU-1784 Sofia, Bulgaria
关键词
mixed-layer; turbulent flux; NOPEX; meteorological models; radiosoundings;
D O I
10.1016/S0168-1923(99)00095-7
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
A method to determine the regional integrated heat flux from measurements on the evolution of the mixed-layer is presented. The necessary input for the method can be deduced from successive radiosoundings. The regional heat flux over the NOPEX experimental area, an inhomogeneous region with patches of forest, agricultural fields, mires and lakes within the boreal zone, was determined for 3 days of the campaign in 1994. It was found to be lower than the heat flux over forest and higher than the heat Aux over agricultural fields. The regional heat flux estimated by the mixed-layer evolution method was compared to a land-use-weighted average heat flux. The two independent estimates of the regional heat Bur were found to be in general agreement. (C) 1999 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:159 / 167
页数:9
相关论文
共 40 条
[1]  
AVISSAR R, 1989, MON WEATHER REV, V117, P2113, DOI 10.1175/1520-0493(1989)117<2113:APOHLS>2.0.CO
[2]  
2
[3]   APPLIED-MODEL FOR THE GROWTH OF THE DAYTIME MIXED LAYER [J].
BATCHVAROVA, E ;
GRYNING, SE .
BOUNDARY-LAYER METEOROLOGY, 1991, 56 (03) :261-274
[4]   AN APPLIED-MODEL FOR THE HEIGHT OF THE DAYTIME MIXED-LAYER AND THE ENTRAINMENT ZONE [J].
BATCHVAROVA, E ;
GRYNING, SE .
BOUNDARY-LAYER METEOROLOGY, 1994, 71 (03) :311-323
[5]   EFFECTIVE RESISTANCE TO SENSIBLE-HEAT AND LATENT-HEAT FLUX IN HETEROGENEOUS TERRAIN [J].
BLYTH, EM ;
DOLMAN, AJ ;
WOOD, N .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1993, 119 (511) :423-442
[6]   ESTIMATION OF AREALLY-AVERAGED SURFACE FLUXES [J].
CLAUSSEN, M .
BOUNDARY-LAYER METEOROLOGY, 1991, 54 (04) :387-410
[7]   Boundary layer budgets for regional estimates of scalar fluxes [J].
Denmead, OT ;
Raupach, MR ;
Dunin, FX ;
Cleugh, HA ;
Leuning, R .
GLOBAL CHANGE BIOLOGY, 1996, 2 (03) :255-264
[8]  
DOLMAN AJ, 1992, Q J ROY METEOR SOC, V118, P455, DOI 10.1002/qj.49711850504
[9]   A model for the height of the internal boundary layer over an area with an irregular coastline [J].
Gryning, SE ;
Batchvarova, E .
BOUNDARY-LAYER METEOROLOGY, 1996, 78 (3-4) :405-413
[10]  
GRYNING SE, 1994, Q J ROY METEOR SOC, V120, P47, DOI 10.1002/qj.49712051505