目的是在形象校正的精确性上探索地面控制点(GCP ) 的空间分发的效果。区域分布式、线性地分布式的 GCP 被用来修正一个沿海的地区的一幅陆地卫星 TM 图象。校正精确性对 99 个独立的点被检查在上内部没有地面控制的潮汐的泥公寓。结果显示在这些区域上的剩余的 root-mean-square 错误比它的测量 GCPs 的对应物若干次大。如果 GCP 空间地在一个区域上被驱散,剩余在东行航程(R~2 =0.827 ) 与距离稳定地波动,但是增加到控制的来源。在 northing,他们在 150 m 附近波动直到 15 km,他们在变化的一个小范围稳定地在以外起床。这些剩余比在东行航程从距离是不太可预言的到控制的来源(R~2 = 0.517 ) 。如果 GCP 沿着一根控制线是分布式的,剩余线性地与距离升起到它并且能干地预言(R~2 = 0。877 ) 在对它垂直的方向。在到它的方向平行,距离几乎没在校正剩余上有很少影响。
The purpose is to explore the effect of the spatial distribution of ground control points (GCPs) on the accuracy of imagery rectification. Both area-distributed and linearly distributed GCPs were used to rectify a Landsat TM image of a coastal zone. Rectification accuracy was checked against 99 independent points over the intertidal mudflats with no ground control. Results indicate that the root-mean-square error of residuals over these areas is several times larger than its GCPs-measured counterpart. If the GCPs are spatially dispersed over an area, residuals fluctuate but increase steadily with distance to the source of control in easting (R^2= 0. 827). in northing they fluctuate around 150 m until 15 km, beyond which they rise steadily at a small range of fluctuation. These residuals are less predictable from distance to the source of control than in easting (R^2= 0.517 ). If the GCPs are distributed along a control line, residuals rise with distance to it linearly and predictably (R^2 = 0. 877) in the direction perpendicular to it. In a direction parallel to it, the distance has little impact on rectification residuals.