A simplified approach for predicting shortwave radiation transfer through boreal forest canopies

被引:42
作者
Nijssen, B [1 ]
Lettenmaier, DP [1 ]
机构
[1] Univ Washington, Dept Civil & Environm Engn, Seattle, WA 98195 USA
关键词
D O I
10.1029/1999JD900377
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Transmission of shortwave radiation through forest canopies is the primary determinant of the energy inputs to the understory or the ground surface. In the context of land surface change studies and distributed hydrological modeling, there is a need for models that represent the radiative transfer in a simple yet realistic manner, only employing input parameters that are routinely measured. A simple canopy radiation model is presented, which simulates the below-canopy shortwave radiation as a function of measured above-canopy radiation. The model uses a Beer's law approach and accounts separately for the transmission of diffuse and direct shortwave radiation. The model accounts for multiple scattering in the canopy in the near-infrared as well as the effects of multiple reflections between the understory and the overstory. The only required input parameter is the effective leaf area index, although additional information about canopy structural and optical properties can easily be included where available. The model was tested using above- and below-canopy radiation measurements at a mature jack pine site and a black spruce site in the BOREAS southern study area near Prince Albert, Saskatchewan. Without calibration the model performed well at the mature jack pine site. However, at the mature black spruce site, the below-canopy radiation was overpredicted, although some of the apparent overprediction appeared to be due to sampling error.
引用
收藏
页码:27859 / 27868
页数:10
相关论文
共 39 条
[1]   Seasonal variation of energy and water vapor exchange rates above and below a boreal jack pine forest canopy [J].
Baldocchi, DD ;
Vogel, CA ;
Hall, B .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D24) :28939-28951
[2]   Albedo over the boreal forest [J].
Betts, AK ;
Ball, JH .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D24) :28901-28909
[3]   CHANGING IDEAS IN HYDROLOGY - THE CASE OF PHYSICALLY-BASED MODELS [J].
BEVEN, K .
JOURNAL OF HYDROLOGY, 1989, 105 (1-2) :157-172
[4]   EFFECTS OF BOREAL FOREST VEGETATION ON GLOBAL CLIMATE [J].
BONAN, GB ;
POLLARD, D ;
THOMPSON, SL .
NATURE, 1992, 359 (6397) :716-718
[5]   Leaf area index of boreal forests: Theory, techniques, and measurements [J].
Chen, JM ;
Rich, PM ;
Gower, ST ;
Norman, JM ;
Plummer, S .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D24) :29429-29443
[6]   Radiation regime and canopy architecture in a boreal aspen forest [J].
Chen, JM ;
Blanken, PD ;
Blank, TA ;
Guilbeault, M ;
Chen, S .
AGRICULTURAL AND FOREST METEOROLOGY, 1997, 86 (1-2) :107-125
[7]  
DICKINSON RE, 1983, ADV GEOPHYS, V25, P305
[8]   ESTIMATION OF THE DIFFUSE-RADIATION FRACTION FOR HOURLY, DAILY AND MONTHLY-AVERAGE GLOBAL RADIATION [J].
ERBS, DG ;
KLEIN, SA ;
DUFFIE, JA .
SOLAR ENERGY, 1982, 28 (04) :293-302
[9]  
Goudriaan J., 1977, CROP METEOROLOGY SIM
[10]   PHYSICALLY BASED HYDROLOGIC MODELING .2. IS THE CONCEPT REALISTIC [J].
GRAYSON, RB ;
MOORE, ID ;
MCMAHON, TA .
WATER RESOURCES RESEARCH, 1992, 28 (10) :2659-2666