Tree ring width measurements from a Norway site provide a paleoclimate record. The chronology spans 600 years, from 547 to 47 calendar years before present. Data is archived by NOAA's National Centers for Environmental Information and was last updated in 1997.
Use Cases
- Reconstruct past temperature or precipitation anomalies using the tree ring width time-series.
- Calibrate the chronology against other regional proxy records like ice cores or varves.
- Analyze growth trends and extreme events within the 600-year record for climate forcing studies.
- Validate spatial climate models for Northern Europe using this site-specific proxy data.
Strengths
- Chronology covers a 600-year period from 547 to 47 BC.
- Data is curated and archived by the authoritative NOAA World Data Service for Paleoclimatology.
Limitations
- Data is temporally stale, with a last update recorded in 1997.
- Geographic coverage is limited to a single site (Stonglandseidet, Norway).
- Sample size and replication statistics are unknown from the provided metadata.
Provenance
- Source
- NOAA National Centers for Environmental Information (NCEI) World Data Service for Paleoclimatology.
- Collection Method
- Tree ring analysis (dendrochronology) of Pinus sylvestris (PISY) samples.
- Time Range
- 547 to 47 calendar years before present (BP).
- Freshness
- null
- Geography
- Stonglandseidet, Norway, Scandinavia.