FWSE  x _     C?    ?     Verdana   	3    wb            (  THE ISOHYETAL METHOD   (      lC&&π 3̙    5G{_:	Z-F0+%kEŌqbE:kEy|qgj{ް|-&0n7(&ϰ'/3:֨9㢿ƵjO7ʴd#f蠬U~s%*A?m/8'cT>#U@XP'T ZWx9 p){u\   |Z)@	*    g<X            (  Land Area >>   o	&    g6h  @        (  Begin >>   㐿    ls[U%     5%KBURUP+U">,,c*Z$
@!Z$|e~@`Xz#,, KIRЁ$ UTT2
HO9
h@*J jZZE ~YڵrT IU%UBR-SH-" ?R?]H@*djGYiXsIRЁ$ UTT2
HO#,, K>P9*Z$
@!Z$|e~@`[5!ARЁ$ UTT2
HO#,, KۧE ~h@*J jZXhxrT IU%UBR-SH-" ?Ry-9*Z$
@!Z$|e~@`ZRЁ$ UTT2
HO#,, K   G 	!    _C`             (  8cm   G 	#    __`             (  6.5cm    	!   	 _H`             (  7cm  	 _P	#   
 __`             (  8.5cm 	 
 1b}	!    _H`             (  8cm 
  	!    _H`             (  7cm   b
	#    _\`              (  6.5cm   ! 	!    _H`             (  5cm   c 	!    _@`             (  6cm   ȡh 	!    _A`             (  4cm    ـ	#    _a`             (  4.5cm   ԃ 	!    _C`             (  3cm    	!    _F`             (  3cm    I    U R}        WٕL 'Lf͆fpc(l*l' 2I@pٔ  I    U RP     WٕL 'Lf͆fpc(l*l' 2I@pٔ  I    U R}     H%l &g &28{@)) Z' Y͙I͙Tt k -                           `	a    o             (  This method works bestwith a greaterdistribution of pptgages...   :@    ?    	%    g6  h         (  Next >>   , I    U R/       @!0 6'5)錩|ege 6sfVsfQ2   I    U R/    @!0 6'5)錩|ege 6sfVsfQ2   I    U R/    Kʛ' V|Phg6eg6e 	 asY -                            	   o[r              (  Now draw lines delineatinga particular measurement.Use intervals of 1cmbetween each line. Forinstance, if one line represents 3cm, then thenext line should represent4cm, and then 5cm andso on.... Click next to seethe lines drawn...    @   K    U R[$|6       @!2 6'5 		|  ege yfRsfQ0   K     U R[$|6    @!2 6'5 		|  ege yfRsfQ0   K   ! U"+[$|6    H-k g2@{?)) '͙Y͙Dt l "   "           !   !     " 8P  I   # mGCߑ  < fff%։33.㨪6WͨBĨ)!Ҙ(DM  # i @  	!   $ _A`             (  3cm  $ ~i @  @ 	 i @ T	 i @ T@ 	 i @ 	 i @ @ 	 i @ 	 i @ @ 	 i @T	 i @T@ 	 i @	 i @@ 	 i @ 	 i @ @ 	 i @T	 i @T@ 	 i @	 i @@ 	 i @ 	 i @ @ 	 i @T	 i @T@ 	 i @	 i @@ 	 	  D   % mO`  < fff%;
NZ-^R(<U3t{MlK D ~8  % i @  	!   & _D`             (  4cm  & i @  @ 	 i @ h	 i @ h@ 	 i @ ̉	 i @ @ 	 i @4	 i @4@ 	 i @	 i @@ 	 i @ 	 i @ @ 	 i @h	 i @h@ 	 i @̉	 i @@ 	 i @4	 i @4@ 	 i @	 i @@ 	 	  G   ' m9  < fff%Q 6Ω9J*VR蚀h.&rR
$0ͮɋB};  ' Zi @  	!   ( _D_`             (  5cm  ( I i @  @ 	 i @ h	 i @ h@ 	 i @ ̉	 i @ @ 	 i @4	 i @4@ 	 i @	 i @@ 	 i @ 	 i @ @ 	 i @h	 i @h@ 	 i @̉	 i @@ 	 i @4	 i @4@ 	 i @	 i @@ 	 	  I   ) m{@  < fff%Z'.w(dfVx㻉Qs'd  ) f$i @  	!   * _D`             (  6cm  * Vi @  @ 	 i @ h	 i @ h@ 	 i @ ̉	 i @ @ 	 i @4	 i @4@ 	 i @	 i @@ 	 i @ 	 i @ @ 	 i @h	 i @h@ 	 i @̉	 i @@ 	 i @4	 i @4@ 	 i @	 i @@ 	 	  Q   + m&YeȒw  < fff%&pz->hyk֢Nk2pH(ҦhZstӿ33 + f**`i @  	!   , _G?`             (  7cm  , Ui @  @ 	 i @ h	 i @ h@ 	 i @ ̉	 i @ @ 	 i @4	 i @4@ 	 i @	 i @@ 	 i @ 	 i @ @ 	 i @h	 i @h@ 	 i @̉	 i @@ 	 i @4	 i @4@ 	 i @	 i @@ 	 	  L   - m"՟ < fff%L.ދRǯ1;g#
-/!(ƲJѫK>   - \J i @  	!   . _A`             (  8cm ! . i @  @ 	  i @ h	! i @ h@ 	  i @ ̉	! i @ @ 	  i @4	! i @4@ 	  i @	! i @@ 	  i @ 	! i @ @ 	  i @h	! i @h@ 	  i @̉	! i @@ 	  i @4	! i @4@ 	  i @	! i @@   ?    -   /          !   !        A   / 8P@ 	  	! 	   0 o              (  Note how each line goesthrough a gage with thesame amount of rainfall. Forexample: notice how the7cm line goes through twogages that recorded 7cm.The 8cm line goes throughtwo gages that measured8cm, and so on... " 0 b @  " ?     K   1 U R<	%    H%l &g &2@{G)) Z' Y͙I͙Tt k  K   2 U R<	%       @!0 66 		|e'e@sfRsfU0  -   3   1   2   2   2        B   3 8A 	f  4 w             (  In order to properly drawa line when no gages withthe exact amount your looking for is present, youhave to make an educatedguess as to where to put theline. For example: I put the8cm line a little closer tothe gage reading 8.5cmthan I put it from the 7cmline. This is because 8.5cmis closer to being 8cm than7cm is! " 4   D   5 fœ <  %i h mbGX ѩ4zx   杠p .V* }# 5 j
jJp @  " # ?    	t  6 w`             (  Why do the lines appear soawkward? There can bemany reasons, howeverthe most likely would betopographical influences.The figure to the left couldeasily be a mountain slopewith gages reading higherlevels of ppt being higherup the slope. The 8.5cmgage may be at the top ofa mountain while the 3cmgages are down in a smallvalley...    7    6    " 7 B  I   8 U Rr(        WٔL'L ͆fpg(k(l '2IPpו  I   9 U Rr(     WٔL'L ͆fpg(k(l '2IPpו  I   : U Rr(     @!0 6'6		|  ge ysfVs^Q2  -   ;   8   9   :   :        C  $ ; 8PB  q   < n\u d  d  %G-5xF̮Ѷ)F̽(9l ZhUvcqE`_ZA6(k=?P @	VtȅO& < 6 	$   = _k?`              (  Uphill ' = 
j@ " $ & ' ?    	9  > oe              (  Though not always the case,closely-spaced isohyets mayalso be areas of steeperslopes (yellow). Further-spaced isohyets may beareas of little or no slope. Itis possible that closely-spaced isohyets above steepslopes are results ofenhanced orographicinfluence on rainfall... " > 1  ]  ? ll(  <  <   <  %c@  pKF Q1GL  ?Sf PYKJ+g3 (@0@>4*
' (IA_X Ėޟvٔ3$K=&Ρ (@LL31GDTf  0yJ#FRZ =*4 ΍ѳy8FN l-= M y3rd8[lh '^ڥK: P #2*{!1E| c<6İK& v  Kh  3ryttthg(49Ԙ 3S ŝ3=3( O( Y	D	Bf:f N &S$~ ;jj{7V7W Dg DLi̵txtx ʩʪ ;m#z@z 
 ÞPPG = N<aami(6@e?tp3/d:!`z^Q@ hi]Yz^jQڠ@,,ue '}oF
ox 9
 X퐩.	
P .ow # ?  I   @ U Rr(        @!0 66 		|  e' s^RsfU2   I   A U Rr(     @!0 66 		|  e' s^RsfU2   I   B U Rr(     @!0 66 		|  e' s^RsfU2  -   C   @   A   B   B        D  $ C 8C @    	 
                 ! " # $ ?       D mscn$      5.K|/)(@Jr0.nZ0`@!^]&/%Ӥ@_/SPXV҄@/) 1|h. /} A{e Ayt[4hN|LiBT 1|h. /}҄@/)  "I%Ft~PƔ %B yL Ptr0/.K|/)(@Jr7Ɣ %B yL PtI%Ft~PNFR1|h. /}҄@/) PZ]&/%Ӥ@_/SP0`@!\.K|/)(@Jr0.>b	oѢ]:@_%1	P.^S ! D ?   E  Verdana   	!   F _I`  E            (  3cm  F 	!   G _G?`  E            (  4cm  G C- 	!   H _I`  E            (  5cm  H 	#   I _b`  E            (  5.5cm 	 I YP	!   J _J`  E            (  6cm 
 J  	!   K _G?`  E            (  6cm  K 7 	#   L _e`  E            (  6.5cm  L ,w 	!   M _G?`  E            (  7cm  M ! 	#   N _h`  E            (  7.5cm  N :ZB`	!   O _G`  E            (  7cm  O 62	!   P _G?`  E            (  8cm  P q	!   Q _I`  E            (  8cm  Q p D   R ]L4h  < fff%PsJBˤBsRds޷PPbiXAvw\9󾢞$p  R grg@	!   S _O`              (  8cm  S Y@ g   T d < fff%k9:*j(YI(YoQ^J
Y;B
u]hk76?8h6(4{+#{  T cJq	!   U _O`              (  7cm  U z6  F   V nFT  < fff%sQ k"P.^Zb8Z,V@Ap2Y,  V lb	!   W _L`              (  6cm  W Et逿 @   X m}" < fff%ZkMhc6`
cIjWh60g  X QE	!   Y _L`              (  5cm  Y L\ @   Z m| < fff%^`ULahfCf.hP(hYŔb  Z Ӏ	!   [ _L`              (  4cm  [ 'ҿ ;   \ m  < fff%:P%\hi׾6wqe{/x  \ x	!   ] _W`              (  3cm  ] aO 	   ^ o             (  This isohyet chart showsa relatively flat basin. Italso shows the center ofthe storm where ppt fell the most! Here,it is likely that there waslittle or no influencefrom topography.  ^ J  I   _ U Rr,        WהL'L ͆fpc(l(l '2I@pٕ  I   ` U Rr,   @!0 6'6		|  'e sfVs^Q2  -   a   _   `   `   `        E   a 0D @    I   b U R@        @!2 6'5		|  ege ysfVsfQ0   I   c U R@     @!2 6'5		|  ege ysfVsfQ0  "   d    b   c   c   c     d 8@E 	   e o              (  Once you have determinedthe locations of eachisohyet, you then measurethe area in between eachisohyet. For instance, measure the area betweenthe 3cm and 4cm isohyets,then between the 4cm and5cm isohyets, and so on...   e ڹ c   f dK;W 2  2  %OG||I;<SRWA(BYsC_VpA<V\_ATva]Vßc ! f  @ @ @ @  s   g mqTy 2  %#l.Ψ]"_A9
cH&3Nq+Eo ,/ -9kmst29
p業 ! g p @ @ @ @ @     h m/Q 2  2  %ON+ͽ?`\UHοu,TqF*Ym%@e4`oYHM@Z'VpЃ̻_[n~l<AUx,b .+B ! h -@@ @ @ @ @     i mCS 2  2  %O3~]	\хzsFvͤGVi4eQ"g4ׄ\%yT[X,D/q{ƀRp乽H*>4>@T˛HՀ6O˛ 6K緀 ! i @@ @ @ @ @     j m0}_ 2  2  %*O6ta7kamYu},%O8U`R+_'@W;^]cwU[U?uSts
 _sTxUs+qfYPX̴# Xgje̖?X?jҖ )k,qP-Vx4!g7yc#p~STӿr1 YpheXv3.~9uFD ! j ^*@@ @ @ @ @     k d4l` 2  2  %qO7	y	eUdWٗ6dU"`Y8b 8ZֆHil'skU Yhw#g,
,[`.j4ϟTI  Ox ! k cJv@@ @ @ @ @  E   l ]DAX 2  2  %Bs.VGD	eRW} b`Ubf \bj ! l ed @ @ @ @ @ ! f  @ @ @ @ ! g p @ @ @ @ ! h -@@ @ @ @ @ ! i @@ @ @ @ @ ! j ^*@@ @ @ @ @ ! k cJv@@ @ @ @ @ ! l ed @ @ @ @  ! ?    -   m   b   c   c   c           m 8@ @    	 
           ?     I   n U RL        @!2 56 		|  e'@ys^RsfU2   I   o U RL     @!2 56 		|  e'@ys^RsfU2  -   p   n   o   o   o           p 8@ 	   q o(              (  Let's say we figured thesize of each area asshown numerically to theleft... we will take thesenumbers and plug them into a simple graph andcompute the averageppt next!....   q z7`	%   r g%
P            (  54sq km ! r !	&   s g)G
P            (  40 sq km " s eZ	&   t g%
P            (  6 sq. km # t X"P`	'   u g?
P            (  43 sq. km $ u ل	'   v g?
P            (  32 sq. km % v !`	'   w g?
P            (  38 sq. km & w `	'   x g?
P            (  20 sq. km ' x `@     ?     "   y o.1WT     %=Z ( y 	  z w؍            (   Col.1         Col.2          Col.3  Avg.         Area     Col.1 x Col.2Isohyet   between      (cm)      isohyets------------------------------------<3                20         3x20= 60 3.5               38      3.5x38= 1334.5               32      4.5x32= 1445.5               43      5.5x43= 2376.5               54      6.5x54= 3517.5               40      7.5x40= 300>8                 6             8x6= 48 ) z L`	%   { g*           (  Next >> * {  I   | U Ry,       K ' 	V|Pgg6eg6e 	 asa   I   } U Ry,    K ' 	V|Pgg6eg6e 	 asa  -   ~   |   }   }   }          + ~ K @ ( ) * + 	    W{ȍ            (  60 (  ~	     W{ȍ            (  133 )  `	     W{ȍ            (  144 *  	     W{ȍ            (  237 +   	     W{ȍ            (  351 ,  ŀ	     W{ȍ            (  300 -   	    W{ȍ            (  48 .  	    W{ȍ             (  20 2  l~	    W{ȍ             (  38 3  `	    W{ȍ             (  32 4  	    W{ȍ             (  43 5  `	    W{ȍ             (  54 6  ŀ	    W[{ȍ             (  6 7  	    W{ȍ             (  40 8   @ ( \t`) * h+ , - ̈. L2 th3 4 5 6 7 88 ̈@ ( i) l{x* l+ l, l- l. Ә2 i3 4{x4 45 4x6 47 Ә8 4@ ( _x) q * ̂+ ̔, ̦ - ̷.  2 _3 q 4  5  6  7 P 8 @ ( |U) ,f* ,x+ ,0, ,- ,0. l2 U3 Lf4 Lx5 L6 L7 ܾ8 L0@ ( J) \* m+ , 8- . ̴82 (J3 \4 n85 6 ؑ87 h88 آ@ ( <@ ) Q* c(+ uH, Ȉ- H. ,Ȉ2 @(3 `Q4 `cȈ5 `t6 `Ȉ7 Ȉ8 `H@ ( 5) LG0* LX+ LjЈ, L|P- LЈ. P2 <53 G04 YP5 j06 |P7 |P8 @ ( +8) <* N@+ ``, q- `. 2 +@3 x<4 xN5 x_6 xq7 8 x`@ ( \ ) 2H* CȈ+ U, gh- x. Lh2 T Ȉ3 2H4 Dh5 UH6 gh7 h8 x@ ( P) l'؈* l9X+ lKx, l\- lnx. 2 X3 '؈4 95 J؈6 \7  8 nx@ ( ؈) `* .+ A , R- d . u     \f  <    %s z /  Ȟ@ PA 	!    _\`ր  @         (  233 0  	    w
#            (  Divide the sum of column 3 by thetotal area of the basin. The resultis the average you're looking for! 1  CL2 l3 `4 /5 @`6 R7 u8 d      T|@ <    %QPu 9  $@	"    _`ր  @         (  1273 :  @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ 0 (@: hP@ 0 9: $@ 0 J: X@ 0 [: @ 0 m : \`@ 0 ~`: @ 0 ʏ: ԣh@ 0  : @ ?    0 ߺ :  #    ]N܅  <    <    %vv<1YT ;  l	.    o            (  5.5cm = average <  { 	+    o            (  Close Window =  @   
