Changes between Version 19 and Version 20 of Stream order

Timestamp:

Oct 4, 2010 12:14:48 PM (15 years ago)

Author:

celine

Comment:

--

Stream order

@@ -19 +19 @@
 Because the orders are additive, the numbers from the Shreve method are sometimes referred to as magnitudes instead of orders. The magnitude of a link in the Shreve method is the number of upstream links.[[BR]]
 
-Shreve, R., Statistical Law of Stream Numbers, J. Geol., 74, (1966), 17-37. [[BR]]
-Shreve, R., Variation of Mainstream Length With Basin Area in River Networks. Water Resources Research, vol.10, no.6 [[BR]]
+Shreve, R. (1966). Statistical Law of Stream Numbers, J. Geol., 74, , 17-37. [[BR]]
+Shreve, R. (1974). Variation of Mainstream Length With Basin Area in River Networks. Water Resources Research, vol.10, no.6 [[BR]]
 ||[[Image(source:data/Docs/trac/Stream Order/Strahler.jpg,400px)]]||[[Image(source:data/Docs/trac/Stream Order/Shreve.jpg,400px)]]||
 
@@ -30 +30 @@
 X= [log([2^N] +[2^M])]/log(2)  #Problème avec l'écriture sur le trac de la formule !!! 2 exposant N + 2 exposant M !!
 s'écrit encore log2(2^N + 2^M)[[BR]]
+
 Scheidegger, A.E. (1965). The algebra of stream-order numbers: lIS. Geo/.!SlIrl'ey Prot: Paper, 525B, pp. BI87-BI89. [[BR]]
 Scheidegger, A.E.(1966) 'EFFECT OF MAP SCALE ON STREAM ORDERS', Hydrological Sciences Journal, 11: 3, 56 — 61 [[BR]]