Response of surface air temperature to small-scale land clearing across latitudes

• Published in: Environmental research letters 2014-03, Vol.9 (3), p.34002-7
• Main Authors: Zhang, Mi, Lee, Xuhui, Yu, Guirui, Han, Shijie, Wang, Huimin, Yan, Junhua, Zhang, Yiping, Li, Yide, Ohta, Takeshi, Hirano, Takashi, Kim, Joon, Yoshifuji, Natsuko, Wang, Wei
• Format: Article
• Language: English
• Subjects: Air temperature; Climate models; Cooling; Cooling effects; Deforestation; diurnal temperature range; Land clearance; Land clearing; Land use; Latitude; latitudinal pattern; surface air temperature; Temperature; Temperature gradients; Weather; Weather stations
• ISSN: 1748-9326; 1748-9326
• DOI: 10.1088/1748-9326/9/3/034002

Climate models simulating continental scale deforestation suggest a warming effect of land clearing on the surface air temperature in the tropical zone and a cooling effect in the boreal zone due to different control of biogeochemical and biophysical processes. Ongoing land-use/cover changes mostly occur at local scales (hectares), and it is not clear whether the local-scale deforestation will generate temperature patterns consistent with the climate model results. Here we paired 40 and 12 flux sites with nearby weather stations in North and South America and in Eastern Asia, respectively, and quantified the temperature difference between these paired sites. Our goal was to investigate the response of the surface air temperature to local-scale (hectares) land clearing across latitudes using the surface weather stations as proxies for localized land clearing. The results show that north of 10°N, the annual mean temperature difference (open land minus forest) decreases with increasing latitude, but the temperature difference shrinks with latitude at a faster rate in the Americas [−0.079 (±0.010) °C per degree] than in Asia [−0.046 (±0.011) °C per degree]. Regression of the combined data suggests a transitional latitude of about 35.5°N that demarks deforestation warming to the south and cooling to the north. The warming in latitudes south of 35°N is associated with increase in the daily maximum temperature, with little change in the daily minimum temperature while the reverse is true in the boreal latitudes.