-
Notifications
You must be signed in to change notification settings - Fork 9
Commit
This commit does not belong to any branch on this repository, and may belong to a fork outside of the repository.
WIP - init config for CALM sites layer
TODOs related to dataset citation and dataset description
- Loading branch information
1 parent
48c65d7
commit a92672d
Showing
2 changed files
with
78 additions
and
1 deletion.
There are no files selected for viewing
47 changes: 47 additions & 0 deletions
47
qgreenland/config/datasets/circumpolar_active_layer_monitoring.py
This file contains bidirectional Unicode text that may be interpreted or compiled differently than what appears below. To review, open the file in an editor that reveals hidden Unicode characters.
Learn more about bidirectional Unicode characters
Original file line number | Diff line number | Diff line change |
---|---|---|
@@ -0,0 +1,47 @@ | ||
from qgreenland.models.config.asset import HttpAsset | ||
from qgreenland.models.config.dataset import Dataset | ||
|
||
circumpolar_layer_monitoring = Dataset( | ||
id="circumpolar_layer_monitoring", | ||
assets=[ | ||
HttpAsset( | ||
id="only", | ||
urls=[ | ||
"https://www2.gwu.edu/~calm/data/CALM_Sites_wData.7z", | ||
], | ||
), | ||
], | ||
metadata={ | ||
"title": "Circumpolar Active Layer Monitoring Network-CALM: Long-Term Observations of the Climate-Active Layer-Permafrost System", | ||
"abstract": ( | ||
"""The primary goal of the Circumpolar Active Layer Monitoring | ||
(CALM) program is to observe the response of the active layer and | ||
near-surface permafrost to climate change over long (multi-decadal) | ||
time scales. The CALM observational network, established in the | ||
1990s, observes the long-term response of the active layer and | ||
near-surface permafrost to changes and variations in climate at more | ||
than 200 sites in both hemispheres. CALM currently has participants | ||
from 15 countries. Majority of sites measure active-layer thickness | ||
on grids ranging from 1 ha to 1 km², and observe soil | ||
temperatures. Most sites in the CALM network are located in Arctic | ||
and Subarctic lowlands. Southern Hemisphere component (CALM-South) | ||
is being organized and currently includes sites in Antarctic and | ||
South America. The broader impacts of this project are derived from | ||
the hypothesis that widespread, systematic changes in the thickness | ||
of the active layer could have profound effects on the flux of | ||
greenhouse gases, on the human infrastructure in cold regions, and | ||
on landscape processes. It is therefore critical that observational | ||
and analytical procedures continue over decadal periods to assess | ||
trends and detect cumulative, long-term changes. | ||
The CALM program began in 1991. It was initially affiliated with the | ||
International Tundra Experiment and has been supported independently and | ||
continuously since 1998 through grants from the U.S. National Science | ||
Foundation*. CALM is funded by the NSF Project OPP-1836377.""" | ||
), | ||
"citation": { | ||
"text": ("""TODO..."""), | ||
"url": "https://www2.gwu.edu/~calm/data/north.htm", | ||
}, | ||
}, | ||
) |
This file contains bidirectional Unicode text that may be interpreted or compiled differently than what appears below. To review, open the file in an editor that reveals hidden Unicode characters.
Learn more about bidirectional Unicode characters