Temperature and precipitation in Mongolia based on dendroclimatic investigations

Recent tree-ring studies in Mongolia provide evidence of unusual warming that is in agreement with large-scale reconstructed and recorded temperaturesfor the Northern Hemisphere and the Arctic. One Mongolian proxy record for temperature extends back over 1000 years and several others are over 350 years in length. Precipitation reconstructions based on tree rings reflect recent increasesbut also indicate that the increases are within the long-term range of variations. Spectral analyses of recorded precipitation data and the reconstructions support the hypotheses of quasi-solar periodicity in precipitation variation, previously suggested by others.

作 者： G.Jacoby N.Pederson R.D'Arrigo   作者單位： Lamont-Doherty Earth Observatory, Palisades, NY 10964, USA  刊 名： 科學(xué)通報(bào)(英文版)  SCI 英文刊名： CHINESE SCIENCE BULLETIN  年，卷(期)： 2003 48(14)  分類號： X14  關(guān)鍵詞： tree rings   Mongolia   paleoclimate   climatic change