Effect of the revisit interval and temporal upscaling methods on the accuracy of remotely sensed evapotranspiration estimates

被引:38
作者
Alfieri, Joseph G. [1 ]
Anderson, Martha C. [1 ]
Kustas, William P. [1 ]
Cammalleri, Carmelo [2 ]
机构
[1] ARS, USDA, Hydrol & Remote Sensing Lab, Beltsville, MD 20705 USA
[2] European Commiss, Joint Res Ctr, Ispra, Italy
关键词
WATER-USE EFFICIENCY; EVAPORATIVE FRACTION; SURFACE-TEMPERATURE; ENERGY-BALANCE; SELF-PRESERVATION; HEAT-FLUX; MODEL; VARIABILITY; RESISTANCE; EVOLUTION;
D O I
10.5194/hess-21-83-2017
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Accurate spatially distributed estimates of actual evapotranspiration (ET) derived from remotely sensed data are critical to a broad range of practical and operational applications. However, due to lengthy return intervals and cloud cover, data acquisition is not continuous over time, particularly for satellite sensors operating at medium (similar to 100 m) or finer resolutions. To fill the data gaps between clear-sky data acquisitions, interpolation methods that take advantage of the relationship between ET and other environmental properties that can be continuously monitored are often used. This study sought to evaluate the accuracy of this approach, which is commonly referred to as temporal upscaling, as a function of satellite revisit interval. Using data collected at 20 Ameri-flux sites distributed throughout the contiguous United States and representing four distinct land cover types (cropland, grassland, forest, and open-canopy) as a proxy for perfect retrievals on satellite overpass dates, this study assesses daily ET estimates derived using five different reference quantities (incident solar radiation, net radiation, available energy, reference ET, and equilibrium latent heat flux) and three different interpolation methods (linear, cubic spline, and Hermite spline). Not only did the analyses find that the temporal auto-correlation, i.e., persistence, of all of the reference quantities was short, it also found that those land cover types with the greatest ET exhibited the least persistence. This carries over to the error associated with both the various scaled quantities and flux estimates. In terms of both the root mean square error (RMSE) and mean absolute error (MAE), the errors increased rapidly with increasing return interval following a logarithmic relationship. Again, those land cover types with the greatest ET showed the largest errors. Moreover, using a threshold of 20% relative error, this study indicates that a return interval of no more than 5 days is necessary for accurate daily ET estimates. It also found that the spline interpolation methods performed erratically for long return intervals and should be avoided.
引用
收藏
页码:83 / 98
页数:16
相关论文
共 103 条
[21]  
Brunsell N., 2006, AMERIFLUX US KON KON, DOI 10.17190/AMF/1246068
[22]   APPLICATION OF SELF-PRESERVATION IN THE DIURNAL EVOLUTION OF THE SURFACE-ENERGY BUDGET TO DETERMINE DAILY EVAPORATION [J].
BRUTSAERT, W ;
SUGITA, M .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D17) :18377-18382
[23]   DERIVABLE FORMULA FOR LONG-WAVE RADIATION FROM CLEAR SKIES [J].
BRUTSAERT, W .
WATER RESOURCES RESEARCH, 1975, 11 (05) :742-744
[24]  
Burt JamesE., 1996, ELEMENTARY STAT GEOG
[25]   Upscaling of evapotranspiration fluxes from instantaneous to daytime scales for thermal remote sensing applications [J].
Cammalleri, C. ;
Anderson, M. C. ;
Kustas, Andw. P. .
HYDROLOGY AND EARTH SYSTEM SCIENCES, 2014, 18 (05) :1885-1894
[26]   A data fusion approach for mapping daily evapotranspiration at field scale [J].
Cammalleri, C. ;
Anderson, M. C. ;
Gao, F. ;
Hain, C. R. ;
Kustas, W. P. .
WATER RESOURCES RESEARCH, 2013, 49 (08) :4672-4686
[27]   Daily evapotranspiration estimates from extrapolating instantaneous airborne remote sensing ET values [J].
Chavez, Jose L. ;
Neale, Christopher M. U. ;
Prueger, John H. ;
Kustas, William P. .
IRRIGATION SCIENCE, 2008, 27 (01) :67-81
[28]  
Colaizzi PD, 2006, T ASABE, V49, P1409, DOI 10.13031/2013.22056
[29]   Daytime evaporation and the self-preservation of the evaporative fraction and the Bowen ratio [J].
Crago, R ;
Brutsaert, W .
JOURNAL OF HYDROLOGY, 1996, 178 (1-4) :241-255
[30]   Conservation and variability of the evaporative fraction during the daytime [J].
Crago, RD .
JOURNAL OF HYDROLOGY, 1996, 180 (1-4) :173-194