Remote-Sensing Technologies and Data Processing Algorithms - New Ecoinformatics Tools in Environmental Science: Applications and Decision-making - page 219

where

n þ k

h
2 mG þ

2
3 Qh

t ¼ l þ ð j QNm j Þ

Let us denote

t þ QMTm 2

T ¼ jk j ð G þ 2Qh = 3 Þ; b ¼ 1 þ jk j Gh = 2 ; r ¼ jkj

Then we get

hTB X

j 1
i¼0 ejjþ rh 3

e j

or, finally, we have

E j ¼ e 0 Z 1 þ rh 3

ð 1 Thb j Þ 1 e 0 þ rh 3 ð 1 Thb j Þ 1 u j u j ;

(Tb) − 1 , Z 1 is the real root of the equation where h ≤

Z j þ 1 TbhZ j 1

= ð Z 1 Þ ¼0

between Z = 1 and Z = hTb.