Growth variations of Dahurian larch plantations across northeast China: Understanding the effects of temperature and precipitation.

Abstract

Climate change is affecting the growth and distribution of trees in the Chinese boreal forest. Such changes in China, the southern terminus of the extensive Eurasian boreal forests, reflect on the changes that could occur further north under a warming climate. Most studies have found that tree growth increases with increasing temperature and precipitation in boreal forests, but there is little observational evidence of the climate thresholds that might slow these growth rates at the more extreme temperatures which are predicted to occur under future global warming. Here, we examine growth responses of this dominant boreal tree species (Larix gmelinii) to climate based on the data from plantation sample plots across a broad region (40° 51 -52° 58 N, 118° 12 E-133° 42 E) in northeast China. From statistically significant fits to quadratic equations, temperature and precipitation are the important climatic factors determining tree growth in L. gmelinii plantations at two age classes (<10 year and 10-30 year-old stands). The maximum rates of tree height and diameter at breast height (DBH) were about 0.53\xa0m/year and 0.46\xa0cm/year at <10 year stands, and about 0.63\xa0m/year and 0.60\xa0cm/year at 10-30 year stands, respectively. For stands with the highest values of mean annual increment (MAI), the corresponding optimal mean annual temperature (MATopt) focused between 0.66\xa0°C and 1.57\xa0°C. The optimal mean annual precipitation (MAPopt) between 663\xa0mm and 708\xa0mm produced the maximal growth increments. With mean annual temperature of -2.4\xa0°C and precipitation of 470\xa0mm averaged over 1954-2005 in Chinese boreal forest region as baseline, we conservatively estimated that trees in Chinese boreal forest appear to have higher growth potentials with the maximum temperature increase of 3.6\xa0°C and precipitation increase of 40%.