Errors in remote sensing of intercepted photosynthetically active radiation: An example from HAPEX-Sahel

被引:7
作者
Hanan, NP
Begue, A
Prince, SD
机构
[1] UNIV MARYLAND, DEPT GEOG, COLLEGE PK, MD 20742 USA
[2] CIRAD CA, MAISON TELEDETECT, F-34093 MONTPELLIER, FRANCE
基金
美国国家航空航天局;
关键词
D O I
10.1016/S0022-1694(96)03198-8
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Canopy PAR interception (IPAR) is an important variable in many models of canopy photosynthesis and net primary production. IPAR can be estimated remotely using spectral vegetation indices (VI). However, IPAR estimates by this method are subject to errors (E) associated with (i) the estimation of fractional interception (f(PAR)) from a VI measurement (E-F), (ii) the accuracy of estimates of incident PAR (E-T) and (iii) the interaction of these errors (E-X). During the HAPEX-Sahel experiment in Niger in 1991 the temporal evolution of a VI was measured over the study sites with a radiometer mounted in a light aircraft. Ground measurements of f(PAR) and incident PAB on HAPEX West Central shrub fallow, grass fallow, degraded shrub fallow and millet sites were available. The f(PAR) measurements were used to determine the relationship between the VI and fractional interception. The aircraft measurements were then used. together with remote estimates of incident PAR from the TOMS satellite. to estimate IPAR through the season and to quantify the error sources. Both E-F and E-T can result in large absolute and relative errors in IPAR estimates, E-X was generally small. In ten-day summations on the shrub and grass fallow sites, the total errors were mostly less than 20% of the round measurements. On the millet and degraded shrub fallow, the ten-day errors were more substantial. The errors at short time steps (1-10 days) cancel when summed for the whole growing season. In applications where the precise daily errors in IPAR estimates cannot be quantified, the statistical uncertainty of the estimates can be evaluated if the uncertainty in the input variables is known. The standard error of IPAR estimates is then dependent on the residual variance in the regression between vegetation index and f(PAR) and on the mean square error of the remote estimates of incident PAR.
引用
收藏
页码:676 / 696
页数:21
相关论文
共 28 条
[11]   A BIOCHEMICAL-MODEL OF PHOTOSYNTHETIC CO2 ASSIMILATION IN LEAVES OF C-3 SPECIES [J].
FARQUHAR, GD ;
CAEMMERER, SV ;
BERRY, JA .
PLANTA, 1980, 149 (01) :78-90
[12]   Scaling and uncertainty in the relationship between the NDVI and land surface biophysical variables: An analysis using a scene simulation model and data from FIFE [J].
Friedl, MA ;
Davis, FW ;
Michaelsen, J ;
Moritz, MA .
REMOTE SENSING OF ENVIRONMENT, 1995, 54 (03) :233-246
[13]   HAPEX-SAHEL - A LARGE-SCALE STUDY OF LAND-ATMOSPHERE INTERACTIONS IN THE SEMIARID TROPICS [J].
GOUTORBE, JP ;
LEBEL, T ;
TINGA, A ;
BESSEMOULIN, P ;
BROUWER, J ;
DOLMAN, AJ ;
ENGMAN, ET ;
GASH, JHC ;
HOEPFFNER, M ;
KABAT, P ;
KERR, YH ;
MONTENY, B ;
PRINCE, S ;
SAID, F ;
SELLERS, P ;
WALLACE, JS .
ANNALES GEOPHYSICAE-ATMOSPHERES HYDROSPHERES AND SPACE SCIENCES, 1994, 12 (01) :53-64
[14]   VEGETATION CANOPY PAR ABSORPTANCE AND THE NORMALIZED DIFFERENCE VEGETATION INDEX - AN ASSESSMENT USING THE SAIL MODEL [J].
GOWARD, SN ;
HUEMMRICH, KF .
REMOTE SENSING OF ENVIRONMENT, 1992, 39 (02) :119-140
[15]  
HEUVELINK GBM, 1993, THESIS U UTRECHT
[16]  
HUETE A R, 1988, Remote Sensing of Environment, V25, P295
[17]  
Kumar M., 1981, Plants and the daylight spectrum. [Smith, H. (Editor)]., P133
[18]  
LIU HQ, 1995, IEEE T GEOSCI REMOTE, V33, P457, DOI 10.1109/36.377946
[19]  
McMurtrie R. E., 1993, P220
[20]   TERRESTRIAL ECOSYSTEM PRODUCTION - A PROCESS MODEL-BASED ON GLOBAL SATELLITE AND SURFACE DATA [J].
POTTER, CS ;
RANDERSON, JT ;
FIELD, CB ;
MATSON, PA ;
VITOUSEK, PM ;
MOONEY, HA ;
KLOOSTER, SA .
GLOBAL BIOGEOCHEMICAL CYCLES, 1993, 7 (04) :811-841