Getting started =============== If you have not completed setup yet, read :doc:`prerequisites` first. Quick checklist --------------- .. code-block:: sh pip install --editable ./cryoswath mkdir cd cryoswath create-config cryoswath download-aux-data cryoswath get-tutorials Then open ``cryoswath.cfg`` in your project directory and confirm that the ``[path]`` section points to the intended ``data`` location. The auxiliary data command installs the Zenodo baseline, and the tutorial command copies notebooks into ``tutorials/``. The copied notebooks import CryoSwath from the active Python environment. You can skip initialization for simple workflows and let CryoSwath default to ``./data``, or set ``CRYOSWATH_DATA`` to choose a data directory explicitly. .. warning:: Use a dedicated environment for CryoSwath. Installing into a shared Python environment can break either CryoSwath or unrelated packages. Supported Python version is 3.12 or newer. .. warning:: Starting **Monday, February 16, 2026**, users need an `ESA EO account `_ before running CryoSat download workflows. Processing the first waveform ----------------------------- If you are new to swath processing, it may be informative to follow the tutorial on (processing and) viewing a single waveform. While this is not the kind of data that you will need to analyze a glaciers evolution, this is its foundation. Knowledge about the smallest parts of the data can help you understand the larger picture. Notebook: `tutorials/tutorial__process_first_waveform.ipynb `_ Processing the first swath -------------------------- Similar to viewing a single waveform, you might wonder how swath data of a single track look like. Again, a single track will not tell you much about a glacier's evolution, but it may help to understand higher level data. Notebook: `tutorials/tutorial__process_first_swath.ipynb `_ will give you a hand using CryoSwath to process a single track and visualize the data. General step-by-step tutorial ----------------------------- The general step-by-step tutorial takes you from processing a waveform to producing a map of elevation change trends. It balances understanding the background processes with quickly enabling to use CryoSwath. Notebook: `tutorials/tutorial__general_step-by-step.ipynb `_.