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README2.md
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# Supplemental data for "Widespread and rapid dynamics of subglacial and proglacial-subglacial water in the Canadian Arctic"
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Whyjay Zheng [1]*, Wesley Van Wychen [2] and Tian Li [3]
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[1] Center for Space and Remote Sensing Research, National Central University, Taoyuan City, 320317, Taiwan.
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[2] Department of Geography and Environmental Management, University of Waterloo, Waterloo, N2L 3G1, Ontario, Canada.
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[3] Bristol Glaciology Centre, University of Bristol, Bristol, BS8 1SS, UK.
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*Corresponding author(s). E-mail(s): [email protected]
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Contributing authors: [email protected]; [email protected]
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## What's inside
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This data set contains:
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1. **Inventory:** The inventory of the active subglacial water bodies in the Canadian Arctic.
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2. **Workflows:** Data analysis code that produces the study results.
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3. **Results:** The derived ArcticDEM strip data and visualizations generated by this study.
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## Content structure
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### Inventory
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`subglacial_lake_event_inventory_37locations.gpkg`: GeoPackage file in the NSIDC Sea Ice Polar Stereographic North projection (EPSG:3413) showing the locations of 37 active lakes. The attribute field `no` corresponds to the no. of the lake presented in the paper. (See the Conversion table below.)
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### Workflows
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`[LocationName]/analysis*.ipynb`: Workflow for each [LocationName] (see conversion table below). These Jupyter notebooks start by downloading ArcticDEM and ICESat-2 data and end with the visualization of the lake elevation change. To execute `analysis*.ipynb`, one needs the following auxiliary files which are included in the data set:
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- `ArcticDEM_Strip_Index_s2s041_*.gpkg`: Subset of the ArcticDEM strip index, containing the strip outlines within a single RGI region.
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- `RGI2000-v7.0-G-*.zip`: RGI 7.0 glacier outlines in a single RGI region.
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- `[LocationName]/refgeo-[LocationName].gpkg`: A rectangle extent at the lake area, defining where to process the data.
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- `[LocationName]/[LocationName]-off-ice-exclusion.gpkg`: Polygons that indicate non-stable ground. ICESat-2 points falling within the polygons are not used for aligning the DEMs.
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#### Conversion table between location name and lake number
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| Lake number | Location name |
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| -------------- | ---------------------- |
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| 1 | MilneTerminus |
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| 2 | Milne |
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| 3-a | MilneCentral (left) |
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| 3-b | MilneCentral (top) |
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| 3-c | MilneCentral (right) |
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| 4-a | OttoN (bottom) |
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| 4-b | OttoN (top) |
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| 5 | IcebergE |
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| 6 | AgassizSWMinor1 |
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| 7 | TaggartLake |
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| 8 | MittieNE |
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| 9 | YelvertonNW |
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| 10 | UnnamedFW |
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| 11 | UnnamedHSE |
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| 12 | Antoinette |
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| 13 | AgassizSWMinor2 |
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| 14 | MittieMain |
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| 15 | ClydeRiverSW |
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| 16 | PennyN |
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| 17 | PennyW |
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| 18 | SvenHedin |
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| 19 | MittieMinor |
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| 20 | OttoNW |
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| 21 | Otto |
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| 22 | Disraeli |
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| 23 | UnnamedF |
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| 24 | Airdrop |
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| 25 | LakeToubergE |
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| 26 | GoodFriday (top) |
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| 27 | GoodFriday (bottom) |
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| 28 | Dlberville |
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| 29 | AgassizSWMain (top) |
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| 30 | AgassizSWMain (bottom) |
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| 31 | JolliffeNArm |
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| 32 | MittieNW |
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| 33 | BylotNE |
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| 34 | ClydeRiverW |
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### Results
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1. `[LocationName]/[LocationName]_15m_hydroevent-evmd-bitmask_[Suffix].tif`: Main results for each glacier. Different suffixes mean:
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- `slope`: dh/dt of the linear model; $a_1$ in Eq. (1)
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- `duration`: total length of $t$ of the linear model
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- `dh`: maximum short-term dh of the sigmoid model; see Eq. (4)
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- `t`: timing of the maximum short-term dh of sigmoid model
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- `gp-dh`: maximum short-term dh of the GP model
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- `gp-t`: timing of the maximum short-term dh of the GP model
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2. `[LocationName]/[LocationName]_15m_hydroevent-evmd-bitmask_viz*.png`: Visualization of the results.
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3. `[LocationName]/[LocationName]_15m_median_topo.tif` Median topography of all the available DEM strips.
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4. `[LocationName]/deminput_processed.csv`: List of the ArcticDEM strip DEMs used in the analysis. The third column represents the 1-sigma uncertainty in m.
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5. `[LocationName]/ref_elevs.csv`: reference elevations extracted from the ICESat-2 ATL-6 data; for DEm alignment.
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6. `[LocationName]/refgeo-[LocationName]_15m.tif`: Reference grid geometry. All the resulting geotiffs have the same image extent and size as this image.
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