Changes in landing page and logos (#40)

OGGM · Feb 25, 2019 · 0275b5e · 0275b5e
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diff --git a/docs/glacier_lowpass.rst b/docs/glacier_lowpass.rst
@@ -22,6 +22,8 @@ and do not sell them.
 
 **Code**: `OGGM-edu <https://github.com/OGGM/oggm-edu/blob/master/gen_plots/ela_changes_response_time.ipynb>`_
 
+**Interactive notebook**: `on Binder <https://mybinder.org/v2/gh/OGGM/oggm-edu/master?filepath=gen_plots/ela_changes_response_time.ipynb>`_
+
 **Download**: `zip file <https://github.com/OGGM/glacier-graphics/blob/master/glacier_response/glacier_response.zip>`_
 
 This series of graphics was used right after the graphics above to explain

diff --git a/docs/index.rst b/docs/index.rst
@@ -4,9 +4,11 @@
 Welcome to OGGM-Edu!
 ====================
 
-This platform will become an educational website about glaciers.
+This platform will become an educational website about glaciers. It is
+currently in construction, but we already have several things for you to
+explore!
 
-It is currently in construction, but you can still try a couple of things:
+:ref:`contact` with us if you want to know more and if you want to help us out!
 
 Interactive apps
 ^^^^^^^^^^^^^^^^
@@ -55,3 +57,22 @@ Graphics
 
     glacier_basics.rst
     glacier_lowpass.rst
+
+.. _contact:
+
+Get in touch
+^^^^^^^^^^^^
+
+Interested in OGGM-Edu? We would love to hear from you!
+
+- All of this website and notebooks are located `on GitHub`_.
+- Report bugs or share your ideas on the `issue tracker`_.
+- Improve the website by submitting a `pull request`_.
+- Follow us on `Twitter`_.
+- Or you can always send us an `e-mail`_ the good old way.
+
+.. _e-mail: https://mailman.zfn.uni-bremen.de/cgi-bin/mailman/listinfo/oggm-users
+.. _on GitHub: https://github.com/OGGM/oggm-edu
+.. _issue tracker: https://github.com/OGGM/oggm-edu/issues
+.. _pull request: https://github.com/OGGM/oggm-edu/pulls
+.. _Twitter: https://twitter.com/OGGM1
diff --git a/docs/notebooks_flowline_intro.rst b/docs/notebooks_flowline_intro.rst
@@ -5,11 +5,11 @@ Glacier flowline modelling
 
 .. figure:: _static/intro_fig_flowline.png
 
-    Figure: Geometry of a glacier model after 500 yeras, that moves only by deformation processes.
+    Figure: Geometry of a glacier model after 500 years, that moves only from deformation processes.
 
 This notebook is an introduction to flowline modelling with OGGM. To open the notebook in your browser use the button below:
 
-.. image:: https://mybinder.org/badge_logo.svg
+.. image:: https://img.shields.io/badge/launch-Edu%20Notebooks-579ACA.svg?style=popout&logo=     data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAYAAABzenr0AAAABmJLR0QA/wD/AP+gvaeTAAAACXBIWXMAAC4jAAAuIwF4pT92AAAAB3RJTUUH4wEeDC0U4ki9ZgAAABl0RVh0Q29tbWVudABDcmVhdGVkIHdpdGggR0lNUFeBDhcAAAQFSURBVFjD7ZddaBxVGIafc2Y22+1u0qSxyaZJbBMTxLapUseUIsWWWrRIFhYL9bfgjdirQgX1qhUUb7zwQnqhghZ7IYo4MKJoo1YUtcQxlTRpWkyWGEp+l+zmZ5vs7swcL9yENeruxhi9yXc358z5nvfM9853ZgT/X/gAyXqsx3r8W2FHI9jRyNpDll1X2dFIVbH7CoVYCdgwLexoZA/wDHA34M/lSAE9wNuGaX2/fM2qBCyDnwFOCKU2S9fxCaUAUEKgpHQ8qc0BJvC8YVqTpYjQS3kCOfgrwEnheRvnqrYwuHMv09V1eEISnE2wdahfDw9fr9SczFNKyDvsaOSYYVrDxcohiu0+Bz8CnBeeVz1y2y6utD+AEmIpgRDgIqkeH2aH/QWhZBwl5SfAE4ZpJRfzrMYDF4XnHUjUNtJ16BgqN66UIlxVjtFSzzd9Q0ylXcKjMXb+2MnG2SRKiCeB9wzTcv8utywBbgBNUnn07zmIAny6JBTwo3DZFMpyZ3MYo7Uezc0y1thKvK4JT2oAJ4CyQvlLOQ7bhPJCc5XVpCo2A3BPawOHdjdzIxHj3LdnSaQSNIcrqa0MQNYhXredrD8ASrUX81kpAiqFUr754CZQCp8uOdDWREt9JRv8ccaTE3THekllphhJ/oLrZkgHQniatmhyXyEjliIgpRBuWXoeIXXiswN0DXTj18t45N7DzMyn+CnWw+R0nK7YV8RTN/C5DsLzFterQslLeQ17lBSp8mS8SkyPcmHwQ77sf58zR0/RUL0Vv17G11d/YDw5yeDENbRAI/uSG9CzGRBiCEivqg8YpnXJjkauStdtaLjcyUJgBkcpXvroNVrDzWRdh9j4rwyMDZERkBnto2LMh8/J4sEHgPOPPbBUOyFedGGiZXyC44kgITTG5mf4bqAbD3AFpHVBrSrjyMgs4dk5FGoGOA9kCjG0EpqQnPn5cnzLQx1pJx4/uH1earendSrQUJpECMEtjmTfTT8PJwPctVCGD4GCU8Dnhml5djTCm9eul16CZa49Wb6r7bi/pubizWDwsDY9/fKOBX3/toxGSvrJCtAUBD1ByBMACwpeAM4ZpuUUOwtEkd13AK8D24TuQ7nOgyhlA3sFPAbsB27NOT2m4GPgXeDKIrxQG/5LAXnw3cBbQHtuqhe4zzCtKTsakbnvej3PRx6QBbKGaalS4H8SkAevAc4CR3NTidxu+4olXMm3wJKAfKV2NBIATvN7HRcbSQfwqWFaqpRdrSTkMuUSeDwPDvAscGEt4AAy77EL4H7g1bz5N4B3DNPKrgX8Dx6wo5Fm4DOgNTfUCTxtmNbQWsGXSpAzTSivL/QCp9caDqDnAXrsaORR4DnAMkzr0n/xP/Ebgv/Oed8KI9UAAAAASUVORK5CYII=
     :target: https://mybinder.org/v2/gh/OGGM/oggm-edu/master?urlpath=lab/tree/notebooks/oggm-edu/welcome.ipynb
 
 In this notebook we will set-up a simple model run and visualize it afterwards. Therefore we will learn how to define an easy glacier bed and a suitable grid. The learner will implement mass balance in the form of equilibrium line altitude (ELA) and see how his glacier develops in length, volume and area over certain years.

diff --git a/docs/notebooks_howto.rst b/docs/notebooks_howto.rst
@@ -14,7 +14,7 @@ You can learn about them and try them out on the `Jupyter website <https://jupyt
 
 We also have prepared a tutorial for you on OGGM-Edu. Open it in your browser with:
 
-.. image:: https://mybinder.org/badge_logo.svg
+.. image:: https://img.shields.io/badge/launch-Edu%20Notebooks-579ACA.svg?style=popout&logo=     data:image/png;base64,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
     :target: https://mybinder.org/v2/gh/OGGM/oggm-edu/master?filepath=notebooks/oggm-edu/getting_started_with_notebooks.ipynb
 
 If you are also new to python, be patient! We will provide an introduction to python for OGGM-Edu users here soon.

diff --git a/docs/notebooks_ice_flow_parameters.rst b/docs/notebooks_ice_flow_parameters.rst
@@ -6,13 +6,13 @@ Ice flow parameters
 .. figure::  _static/intro_fig_iceflow_parameters.png
     :width: 70%
 
-    Figure: Geometry of glacier models after 1500 years.  Blue graph: glacier moves by deformation, orange graph: glacier that slides also. 
+    Figure: Geometry of glacier models after 1500 years.  Blue graph: glacier moves by deformation, orange graph: glacier that slides also.
 
 In this notebook we will have a closer look at the parameters that describe ice flow: Glen's creep parameter and the sliding parameter. We will implement them in our model and see their influence on glacier flow.
 
 Open this experiment in your browser with the button below:
 
-.. image:: https://mybinder.org/badge_logo.svg
+.. image:: https://img.shields.io/badge/launch-Edu%20Notebooks-579ACA.svg?style=popout&logo=     data:image/png;base64,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
     :target: https://mybinder.org/v2/gh/OGGM/oggm-edu/master?urlpath=lab/tree/notebooks/oggm-edu/welcome.ipynb
 
 *Prerequisites:* You went through the notebook about `glacier flowline modelling`_, so that you understand the concept of building a simple glacier model with OGGM.

diff --git a/docs/notebooks_mass_balance_gradient.rst b/docs/notebooks_mass_balance_gradient.rst
@@ -4,14 +4,14 @@ Mass balance gradient
 =====================
 
 .. figure:: _static/intro_fig_MBG.png
-    
+
     Left figure: Behaviour of different mass balance gradients. Right figure: Geometry of glaciers with different mass balance gradients after 300 years.
 
 In this notebook you will run experiments with a focus on the mass balance gradient. You will see how different mass balance gradients influence the growth of a glacier. Therefore, we calculate our glacier models until they reach an equilibrium state and compare length, area and volume. In addition, we will calculate the volume response times of the glacier models to small climatic changes.
 
 Open this experiment in your browser with the button below:
 
-.. image:: https://mybinder.org/badge_logo.svg
+.. image:: https://img.shields.io/badge/launch-Edu%20Notebooks-579ACA.svg?style=popout&logo=     data:image/png;base64,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
     :target: https://mybinder.org/v2/gh/OGGM/oggm-edu/master?urlpath=lab/tree/notebooks/oggm-edu/welcome.ipynb
 
 *Prerequisites:* You went through the notebook about `glacier flowline modelling`_, so that you understand the concept of building a simple glacier model with OGGM.

diff --git a/docs/notebooks_surging_glaciers.rst b/docs/notebooks_surging_glaciers.rst
@@ -5,11 +5,11 @@ Surging glaciers
 
 .. figure:: _static/intro_fig_surging_glaciers.png
 
-    Figure: Development of two surging glaciers. Upper graph: length, lower graph: volume. 
+    Figure: Development of two surging glaciers. Upper graph: length, lower graph: volume.
 
 This notebook treats surging glaciers. You will learn how to implement surging in a glacier model and execute a few experiments with it. To open the notebook in your browser use the button below:
 
-.. image:: https://mybinder.org/badge_logo.svg
+.. image:: https://img.shields.io/badge/launch-Edu%20Notebooks-579ACA.svg?style=popout&logo=     data:image/png;base64,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
     :target: https://mybinder.org/v2/gh/OGGM/oggm-edu/master?urlpath=lab/tree/notebooks/oggm-edu/welcome.ipynb
 
 *Prerequisites:*

diff --git a/gen_plots/ela_changes_response_time.ipynb b/gen_plots/ela_changes_response_time.ipynb
diff --git a/notebooks/oggm-edu/mass_balance_gradients.ipynb b/notebooks/oggm-edu/mass_balance_gradients.ipynb
@@ -462,9 +462,7 @@
   {
    "cell_type": "code",
    "execution_count": null,
-   "metadata": {
-    "scrolled": true
-   },
+   "metadata": {},
    "outputs": [],
    "source": [
     "# change Ela\n",

diff --git a/notebooks/oggm-edu/surging_experiment.ipynb b/notebooks/oggm-edu/surging_experiment.ipynb
@@ -387,9 +387,7 @@
   {
    "cell_type": "code",
    "execution_count": null,
-   "metadata": {
-    "scrolled": false
-   },
+   "metadata": {},
    "outputs": [],
    "source": [
     "# Plot the results\n",