FAQ

01

General

July 12th 2024

Problem:

I get an error when I try to update RAMMS (Help -> Update… -> Web Update). What is going wrong?

Answer:

This is due to the transition of RAMMS from SLF to the new WSL-Spin-off company RAMMS AG. Some links do not work anymore.

Avalanche/Debrisflow:

Please update your version by doing the following:

  • Download the update from here, and unzip the file to a local directory (e.g. C:\Temp\).
  • Then start RAMMS and choose Help -> Update… -> Install Update from local folder.
  • Select your local directory from before, where you unzipped the update.
  • RAMMS should now tell you, that an update is available. Do NOT let RAMMS show you the changelog document, as this link also does not work. Click No.

     

  • In the next window, RAMMS shows you your current version, and the update version. Click Yes to update your RAMMS version.
 
  • You successfully installed the update. Restart RAMMS to use the new version.
 
From version 1.8.27 on, Web Update should work again as usual.
 

Rockfall:

If you still use version 1.7.65, then please download the new version from here (Downloads section at the bottom of the page). Version 1.7.65 will not be updated anymore. 

If you already use the new version 1.8.10 or higher, then you can download the update manually from here, and unzip it into your installation directory (replace all files).

From version 1.8.26 on, Web Update should work again as usual.

Did you already install RAMMS?

If No, you have to download and install RAMMS first, before proceeding to the next steps!

If Yes, then do the following:

Start RAMMS for the first time, and you will see the following screen, where you have to click the upper right button, to create the license request file:


Then choose a location to save the license request file (it’s a txt-file).

An informational window will then tell you where you saved your license request file. Attach this file when ordering a license (full, demo or student license).

February 2nd 2021

Problem:

I try to run a simulation, but instead of the results, I get the following error message:

Error-Messages:
Unable to allocate memory: to make array.
Not enough space
Execution halted at: 

What is going wrong here?

Answer:

The following issues can have an influence on the memory management of RAMMS:

  • Do you use a large ortho-image that you overlay? This could be the problem here. Reduce the resolution of your ortho-image and try again.
  • Calculation domain: Do you use a narrow calculation domain? If not, please have a look in the manual on how to define an ideal calculation domain (for avalanche and debris flow simulations).
  • Dump Step: By increasing the dump step, you decrease the amount of memory needed to open a simulation file.
  • Simulation resolution: A very good (=small) simulation resolution increases the amount of memory needed to open a simulation file.

October 25th 2021


Problem:

I have two tif-files, a topographic map and an orthophoto, but I don’t understand why they don’t appear in the program and why it says that it doesn’t find any map or orthophoto. What can I do?


Answer:

  • Both topo map and orthophoto must be in the same coordinate system as the DEM you used to create the project in RAMMS.
  • For topo map and orthophoto, you need the corresponding world-file (tfw-file) to the tif-file. Otherwise, RAMMS will not find the files.

Problem:

I updated RAMMS::Avalanche (or Debrisflow) to version 1.8.0, but now I cannot run any simulations. RAMMS is stuck with “Create .xy-file”, see Figure 1 below.

Solution 1:

Open the “Additional Preferences” (Help -> Advanced… -> Additional Preferences… -> Edit) and check, if you have the “X64” option set to 1 (see Figure 2 below). If you do not find this option, then just add a new line (before the END tag) and enter

X64 1

Then click “Save” and “OK” and try again to run a simulation. If this does not work, then most probably some C++ libraries are missing on your system. Please see solution 2 below.
Solution 2:

  • Open RAMMS
  • Then use the function “Install C++ libraries” (Help -> Advanced… -> Install C++ libraries) to install the libraries (you will need Admin privileges to do that).
Figure 1: RAMMS is stuck with “Create .xy-file”
Figure 2: X64 option in “Additional Preferences”

Question: 

I tried the new update, but when I try to open an old file, the following error message appears:

Can you help me?

Solution:

  • close RAMMS
  • remove this directory: “C:\Users\<your username>\.idl”    (if you specified Preferences in RAMMS, then you have to re-set them)
  • now you should be able to start and use the new version. I strongly suggest only to use the new version (Rockfall) from now on. The speed of the handling is much improved, much easier to use RAMMS!
  • if you again use the old version (Rockfall), then this problem could happen again…….

Answer:

Yes, you can, but this is work in progress. Please get in contact with us and we gladly help!

02

Avalanche

Answer:

In all RAMMS versions (Avalanche and Debrisflow) up to Version 1.5.01, an ENO (Essentially Non-Oscillatory) scheme was used to numerically solve the governing differential equations (Christen et al., 2010). However, the numerical solution was implemented on strictly orthogonal grids. This improves computational speed, but introduces numerical instabilities especially in steep terrain.
The new Version 1.6.20 uses the same second order ENO scheme, but now on general quadrilateral grid. This new scheme improves numerical stability, but slows the computational speed somewhat. The introduction of this stable ENO scheme allows us to use lower H_cutoff values minimizing mass loss during calculations. The standard value of H_cutoff is 0.000001 m.

Answer:

Avalanches

The Voellmy model – coupled with the calibrated parameters – can be used to

  • (1) predict the runout distance and
  • (2) predict the maximum flow velocity of extreme, large snow avalanches.

This is one of the important research results from the Vallée de la Sionne test site. The Voellmy parameters that we recommend describe the front of a dry-snow avalanche. Because the front defines the runout distance and maximum velocity the Voellmy model will work.

However, the Voellmy model will not describe the avalanche flow behind the front, at the tail of the avalanche. Here, measurements show an increase in the friction (a rapid decrease in speed). This effect causes avalanches to elongate and eventually deposit mass. Therefore, the Voellmy model will not predict the deposition behaviour.

The Voellmy model has difficulties to predict the runout of small avalanches, which sometimes begin immediately to deposit or “to starve”. Of course, small avalanches can be modelled using higher μ and ξ values, but this is a very ad-hoc approach.

Answer

The time required to simulate an avalanche or a debris flow is a function of the finite volume grid resolution and the size of the calculation domain. Typically we use 5m resolutions and the simulations require around 10 minutes. We usually perform the initial simulations at 10 m resolution and therefore we have results in 1 or 2 minutes. When we have a solution that we like we might take a look at the problem at 2m resolution.

03

Rockfall

October 25th 2021

Problem:

I get an error when I import the shapefile of my release areas. What is going wrong?

Answer:

  • The polygon shapefile most probably contains Z and M values. RAMMS does not like them 🙂
  • Convert the shapefile to a polygon shapefile without Z and M values, and it will work.

October 14th 2021

Question:

We have a query about the Zh-height value assumed in the calculations. The manual notes that Zh varies between 5m and 30m, with a default value of 30m, see Figure 1 below. We were therefore expecting to be able to specify a Zh in the calculation but can not see where we can do this. We therefore wondered if the open forest, medium forest and dense forest options assume different Zh values or if they assume the default value of 30m that we can not change.
The maximum tree height we are expecting is also less than 30m and is around 20 to 25 metres. Another reason we were looking to see if we can change the height.

Answer:

  • The default Zh-value for all forest types is 30m.

You can change the Zh-value by doing the following:

  • Open RAMMS
  • click the “Additional Preferences” button (left vertical toolbar, at the bottom)
  • and then add the following line (before the END keyword): SHOW_FOREST_PARAMS  1
  • then click ‘Save’ and ‘OK’, and open one of your input files. You should now be able to change the forest height values, see Figure 2 below.

Beware: you could also change the forest-drag-values. We suggest you use the default values from RAMMS. If you have good reasons to decrease or increase the drag values, this is the way to change the drag-values.

04

Debrisflow

Problem: My debris flow simulation takes ages to calculate. I use a 0.5m resolution. Do you have any suggestions on how to speed up my simulation? And sometimes I get this error message:

Error-Messages:
Unable to allocate memory: to make array.
  Not enough space
Execution halted at:  RAMMS_OPENBINARYOUTPUT 2237                    
 

Answer:

There are several important issues that affect your simulation speed and also your (RAMMS) memory management:

  1. Dump Step: By increasing the dump step (when starting a simulation, e.g. 10s instead of 5s), you decrease the amount of memory needed to open a simulation file.
  2. Calculation domain: Do you use a narrow calculation domain? If not, please have a look in the manual (section 3.5.4) on how to define an ideal calculation domain.
  3. Simulation resolution: A very good (=small) simulation resolution increases the amount of memory needed to open a simulation file.
  4. Do you use a large ortho-image that you overlay? This could also be a memory problem. Reduce the resolution of your ortho-image (do not forget to change the .tfw file too) and try again.

Answer:

There are several good reasons:

Firstly, hazard mitigation experts are often interested in the flow behaviour only near the fan. Calculating the movement of the debris flow in the torrent is a time consuming and often useless task. Therefore using a hydrograph can often cut calculation times dramatically.

Another reason is that it is impossible to describe the initial conditions of debris flows as a “block release”. There are cases where block release is a good approximation of reality (e.g. dam breaks), but, in general, it does not accurately reflect the starting conditions of flows from intense precipitation.

Read this publication for more information on this issue:
Deubelbeiss, Y.; Graf, C., 2013: Two different starting conditions in numerical debris-flow models – case study at Dorfbach, Randa (Valais, Switzerland)

Answer:

Debris flow

The “best” constitutive model for debris flows is still a very open question in the scientific community. We recommend using the Voellmy model until a better model is found. Voellmy basically has only two parameters and after some calibration a useful solution can usually be found. With Voellmy one can control the flow velocity (parameter xi) and runout distance (mu).

One reason Voellmy is useful is that it only requires two parameters to calibrate. The turbulent term dominates the frictional behavior when the flow is moving rapidly and the Coulomb term is dominant when the flow is moving slowly, allowing the model to be approximately calibrated to observations of flow velocity and the stopping location of the flow front.

Finding the “right” debris flow model is more difficult than finding the “right” snow avalanche model because debris flows are two component systems (fluid, solid). Much of the behaviour of a debris flow — including the stopping process — involves the interaction between the fluid-solid components. Thus, without a two component model, it will be unlikely that we are able to model all aspects of debris flows. The Voellmy model mixes the two components and therefore models the debris flow when the components volumes are constant and well mixed. This assumes, of course, that the relative portions of solid and fluid remain the same, from head to tail of the event. This is hardly true

Answer:

Erosion is explained in on this page.

05

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