De(re)forestation and climate warming in subarctic China
De(re)forestation and climate warming in subarctic China
Jay Gao a,b, Yansui Liu a,*
a Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China
b School of Environment, University of Auckland, Auckland, New Zealand
Abstract: Although tropical deforestation bears a close relationship with climate change, its exact contribution to climate warming and its threshold of exerting a noticeable influence remain unknown. This study attempts to bridge this knowledge gap by analyzing deforestation data of Heilongjiang Province, China in relation to climate data. It is found that forest cover was reduced from 238,335 km2 in 1958 to 216,009 km2 in 1980, and further to 207,629 km2 in 2000. During this period the provincial annual temperature rose by 1.68 C, against the nation-wide warming of 0.99 C during the same period. At the provincial level the observed deforestation caused a warming in the vicinity of 0.69 C. This warming does not bear any definite relationship with latitude and elevation. At the local scale, deforestation is related inversely to the rise in decadal temperature in the form of DT ? 0.013DF ? 0.4114 (R2 ? 0.30). There is a positive relationship between the accuracy (R2 value) of predicting climate warming from deforestation and its severity. The critical threshold for deforestation to exert a noticeable impact on climate warming (e.g., R2 ? 50%) appears to be 5 km2. The amount of forest cover at the beginning of a period can inhibit temperature rise, but its exact effect on climate warming is difficult to quantify.