Expansion of Cw in the sub-boreal
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Description
SEE ISSUE #21
**Large Cw feasibility increases in the sub-boreal (e.g., SBSmk1)**
• Driven by increasing temperatures and increasing precipitation (especially in spring and autumn)
• Ensemble is neutral to increasing precipitation
• Analogs are primarily ICHmw(2,3,5) and ICHdw4
• These are climates of the western Columbia mountains from Castlegar to Clearwater.
• Visualization in BGC3D indicates that these appear to be reasonable analogs
Will’s notes
• Cw doing ok in the SBSwk1
• Removing cold constraints and sufficient precipitation.
• Frost pooling likely a hazard. This would be a footnote. Across the board for any of these temperate species
• Recommend warm aspects, frost draining, in order to establish in current transitional climate.
Neutral/increasing summer precipitation, with greater increases in precipitation in spring and autumn.
**E.g. SBSmk1**
Contributor guide
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Research direction
Start by reading the referenced issue #21, then review the SBSmk1 evidence and the attached climate visualizations. The issue does not identify files, tests, or an implementation entry point; completion would require deciding and documenting the scope of Cw expansion and its constraints for the sub-boreal.
Written by the indexing model from the issue text.
Assessment
- Domain
- data
- Issue type
- Feature
- Difficulty
- 5/5
- Estimated time
- Over a week
- Activity status
- Stale
- Clarity
- Needs clarification
- Newbie friendliness
- 20/100