Ledston Hall Tree Ring Chronology for Paleoclimate Reconstruction

Tree ring width measurements from the Ledston Hall site in the United Kingdom. The chronology covers 245 years, from 526 to 282 calendar years before present. Data is archived by NOAA's National Centers for Environmental Information under its World Data Service for Paleoclimatology.

Use Cases

• Reconstruct past climate variables like temperature or precipitation using tree ring width as a proxy.
• Calibrate and validate climate models for the British Isles region against the 245-year tree ring chronology.
• Analyze growth patterns and anomalies within the tree ring series to identify extreme historical climate events.
• Perform cross-dating with other regional tree ring chronologies to build a more extensive climate record.

Strengths

• Chronology spans a specific 245-year period (526 to 282 BP).
• Data is curated and archived by the authoritative NOAA NCEI World Data Service.

Limitations

• Sample size and replication depth for individual years are unknown, which affects statistical confidence.
• Geographic coverage is limited to a single site (Ledston Hall) in the United Kingdom.
• The data's temporal coverage ends 282 years BP, limiting analysis of more recent centuries.

Provenance

Source

NOAA National Centers for Environmental Information (NCEI) World Data Service (WDS) for Paleoclimatology.

Collection Method

Tree ring analysis (dendrochronology).

Time Range

526 to 282 calendar years before present (BP).

Freshness

null

Geography

Ledston Hall, United Kingdom, British Isles.