514.18 . . :&@) 9 #$ $
7 12),
= ) , / + .
%&'()' * +,-/. ' ! $& !& $ !
!!: , $, (! ( #.
! [1] ! [3] !!
%! ($, ), ( , ! ). " ’ ,
!, & ( ( ! $ ( ) . ) $& (&.
- ! (!
$ , ! $ !&
0) . / , ! &, # ! ! ! , !,
& $& &. A %, ! ! &.
',0 %&'1 %,2-3 *6+,)'Z. [2]
!& (& ! $ ( ! ! . A
$ $ & (!&
$ % ! . "! !&
$ .
%&'()' 0''5. D 12- !, ! !% . / (!
!, # !$ !:
1. ! . "
$ $ ! ! !&;
2. D ;
3. "# ! % ! % !%
# ! .
) $ !, &, #
% 1.
141
%(' 5'%&'. * ’ $ n !,
! && $.
! !!-!
’! . ' , # ! ! i- ! $
!& , 2-
i i i
i t at bt c
P() 2 . ' – !& ,
3- Pi(t) ait3bit2citdi. *
# ! , $ ! :
1. / si -- i- ! . )
# i- ! si, i
i
i
i tdt s
³
P
) (
1
;
2. D !$ !, $, , !& &, ! i- i+1-
!! , Pi(i) Pi1(i),i 1,n, P'i(i) P'i1(i), P''i(i) P''i1(i),i 2,n1; 3. !& !&, $ $, , !& &, 0- n- . ) P1(0) Pn(n),P'1(0) P'n(n),P''1(0) P''n(n).
D $ ’ 3n & $ % ( !! ! ) 4n $ ( !! ! ). ' & parabolic.sce cubic.sce !’ & ! Scilab 5-& &.
+ $ ! .2 ) ).
$ 0) [1] ` .1.
7 1
* $& `
D$ I II III IV V VI VII VIII IX X XI XII t, ° -5.1 -4.0 0.4 7.9 14.0 17.1 18.5 17.7 13.0 7.4 1.7 -2.8
+. 1.
142
) ) +. 2. + $ : ) parabolic.sce, ) cubic.sce '$ – $, ! $
$& . '$ – , °
P! , $ $
% $, !# $ $ . $ $ ! $ , # ! . 4. 7 ’ , # ! % ! i-
i+1- !! ! . ' ( !& &) ! % ! !. &
$& !&
%$ ,
% $ # ( ’! !- $& (!).
%(). '
& !& (& ! $ $ !& ! (! $ . 0 , # !% % ! (!, ! ), (! ! .
&- '&6 '
1. $ ! : 0)-/ '.1.1 – 27:2011. [ 2011- 11-01] / D !&. .: D !&, 2011. – 123 .
( % !&).
+.3. ' : 1) parabolic.sce, 2) cubic.sce
143
2. $ % .., [' ..: !
!!: " ). %. . . - '. 4. "!.
. %. (!. - ). 43. – D $: )A)A, 2009 – 0.81-87
3. !& [/! ] ; . . #. !, . ).
C%, . #. 2% / !. !.Ä . . -. . : '- +$!, 2003. 343 .
9 # $=
= = =
=. %. `
' % (!
H H H H, !H H !$! ! ! ! ! .
RESUMPTION OF THE ANNUAL VARIATION TEMPERATURE GRAPHIC BASED ON CERTAIN AVERAGE MONTHLY DATE
Victor P. Shytiuk
In this article one of theresumption of annual variation temperature graphic methods is presented,simulated on average monthly temperature date, and based on variation of the algorithm’squadraticand cubic spline tracing issues.
144