Geoscience Reference
In-Depth Information
K
y
ð
x
j
;
x
i
Þ
h
i
2
k
2
3
k
l
ji
¼ 1
þ
K
ð
x
i
;
x
i
Þþ
1
þ
h
i
K
ð
x
i
;
x
i
Þ
K
ð
x
j
;
x
i
Þ
K
y
ð
x
j
;
x
i
Þ
1
2
K
ð
x
j
;
2
3
h
i
c
ji
¼
x
i
Þ
1
þ
K
ð
x
j
;
x
i
Þ
X
i
1
h
s
2
u
d
i
¼ f
0
ð
x
i
Þþk
h
s
K
x
ð
x
i
;
0
ð
x
s
Þ
x
s
Þ
uð
x
s
Þþ
s¼0
Thus, starting the calculation by formula (
2.80
) from j = 1. We get the values of
solution
u
1
; u
2
; ...; u
m
with the error
(x
i
). Let us estimate the value of modulus of
the error
ʵ
(x) from above. Let us introduce the following notation:
ʵ
0
ð
x
Þ
00
ð
x
Þ
M ¼ max
½a
;
b
uð
x
Þ
j
j;
N ¼ max
½a
;
b
u
j
j;
L ¼ max
½a
;
b
u
j
j;
;
n
o
K
y
ð
x
K
x
ð
x
Q ¼ max
R
;
y
Þ
;
y
Þ
;
G ¼ max
R
j
K
ð
x
;
y
Þ
j;
n
;
o
K
0
yy
ð
x
K
0
xy
ð
x
B
¼
max
R
;
y
Þ
;
y
Þ
;
h
¼
max
s
h
j ;
m
6
BM
þ
3h
4
N
3
4
Qh
þ
3
10
Bh
2
l ¼
þ
LG
þ
;
h
2
4
L
n ¼
jj
Bm
2
2h
3
N
þ
h
6
BL
M
þ
þ
Then we have
X
j
1
jj
hG
þ
2
3
Qh
h
2
e
i
þ jj
lh
3
e
j
ejjþ
;
i¼0
ejjþ jj
Qh
X
i
1
jj
G
h
2
e
i
s
þ
nh
2
e
ejjþ
;
s¼0
e
i
¼
u
0
ð
x
i
Þu
0
ð
x
i
Þ
. From these formulas we get roughly
where
e
j
¼
uð
x
j
Þuð
x
j
Þ
,
!
ejjþ
hQ
X
jj
G
i
1
s¼0
ejj
i
Þ
h
2
e
þ
n
þ jj
QNm
ð
;
"
#
X
X
jj
hG
þ
j
1
i
1
s¼0
ejj
2
3
Qh
1
þ
jj
Gh
2
ejjþ
jj
Gh
2
þ jj
th
3
e
j
;
i¼0
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