A bit of reorganisation

Author: simon-m-mudd

LSDTT_hillslope_metrics/LSDTT_hillslope_metrics.asc

@@ -12,6 +12,8 @@ Stuart W.D. Grieve, Univeristy College London and Simon M. Mudd, University of E
 
 include::book/01-introduction/introduction.asc[]
 
+include::book/05-coupled-channel-hillslopes/coupled-channel-hillslopes.asc[]
+
 include::book/02-window-size/window-size.asc[]
 
 include::book/03-hillslope-length/hillslope-length.asc[]

LSDTT_hillslope_metrics/book/01-introduction/introduction.asc

@@ -23,8 +23,6 @@ link:LSDTT_installation.html[Instructions on how to install LSDTopoTools]
 In addition, you will need to use some basic linux shell commands. If you have never done this before I suggest reading this brief introduction: link:LSDTT_using_linux.html[Basic use of the linux shell].
 *********************************************
 
-WARNING: As of November 2017 these documents have not been updated to the latest installation instructions. The source code is https://github.com/LSDtopotools/LSDTT_Hillslope_Analysis[on the hillslope analysis page] but the instructions may be slightly out of date. Please contact http://swdg.io/[Stuart Grieve] if you have questions
-
 === Background reading
 
 If you wish to explore some background reading, a good place to look at how topography can be used to test theories about sediment transport is a series of papers by https://blogs.uoregon.edu/jroering/[Josh Roering] and colleagues:

LSDTT_hillslope_metrics/book/02-window-size/window-size.asc

@@ -1,5 +1,7 @@
 :numbered:
-== Selecting A Window Size
+
+
+== Legacy code: Selecting A Window Size
 
 Many of the operations on hillslopes involve selecting a characteristic window size for fitting the surface topograpy. 
 

LSDTT_hillslope_metrics/book/03-hillslope-length/hillslope-length.asc

@@ -1,5 +1,5 @@
 :numbered:
-== Extracting Hillslope Lengths
+== Legacy code: Extracting Hillslope Lengths
 
 This section gives an overview of how to use the hillslope length driver (*LH_Driver.cpp*)
 and it's companion (*LH_Driver_RAW.cpp*) to quickly generate hillslope length data for a

LSDTT_hillslope_metrics/book/04-dimensionless-E-R/dimensionless-e-r.asc

@@ -1,5 +1,5 @@
 :numbered:
-== Dimensionless Erosion and Relief
+== Legacy code: Dimensionless Erosion and Relief
 
 The relationship between topographic relief and erosion rate can be used to interrogate dynamic forces which interact to shape the Earth's surface. Roering et al. (2007) formulated a dimensionless relationship between relief (R*) and erosion rate (E*) which allows comparisons between landscapes of vastly differing forms. Hurst et al. (2013) used this technique to identify topographic uplift and decay along the Dragons Back Pressure Ridge, CA. However, in spite of its utility, it has always been a challenging method to implement. In this chapter we go through the steps required to generate E* R* data using https://lsdtopotools.github.io/[LSDTopoTools] from high resolution topography at a range of spatial scales, following Grieve et al. (2015).