Abstract
By using a single-year discrimination chronology detrended from a δ13C chronology from Chinese pine (Pinus tabulaeformis) tree rings and meteorological data, the δ13C-climatic response is analyzed. The results show that high-frequency δ13C is significantly related to both temperatures of June (with r= -0.65) and the total precipitation of May, June and July (r= -0.46). This suggests that δ13C records reflects some features of the East Asian summer monsoon. In addition, temperature departure for June is reconstructed from a transfer function developed with δ13C-climatic response.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 152-161 |
| Number of pages | 10 |
| Journal | Science in China, Series D: Earth Sciences |
| Volume | 39 |
| Issue number | 2 |
| State | Published - Apr 1996 |
Keywords
- East Asia monsoon
- Huangling
- Temperature departure reconstruction
- δC of tree rings
ASJC Scopus subject areas
- General Earth and Planetary Sciences