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Simulating Temperature in a Soil Incubation Experiment
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Afforestation in China cools local land surface temperature.

Shu-Shi Peng1, Shilong Piao, Zhenzhong Zeng

  • 1Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China.

Proceedings of the National Academy of Sciences of the United States of America
|February 12, 2014
PubMed
Summary

China

Keywords:
climate change mitigationplantation effectssurface coolingvegetation feedback

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Area of Science:

  • Environmental science
  • Climate science
  • Forestry

Background:

  • China possesses the world's largest afforested area, crucial for carbon sequestration.
  • The climatic impact of afforestation hinges on energy flux modifications and their effect on surface temperature.
  • Albedo changes in new forests can influence warming, potentially counteracting carbon sequestration benefits.

Purpose of the Study:

  • To investigate the impact of afforestation on land surface temperature (LST) in China.
  • To compare LST in planted forests with adjacent grasslands or croplands.
  • To analyze the drivers of LST changes following afforestation.

Main Methods:

  • Utilized satellite measurements of land surface temperature (LST).
  • Compared LST data from planted forests against adjacent non-forested land.
  • Analyzed temperature variations in relation to latitude and rainfall.

Main Results:

  • Afforestation decreased daytime LST by approximately 1.1 ± 0.5 °C.
  • Afforestation increased nighttime LST by approximately 0.2 ± 0.5 °C.
  • Daytime cooling is attributed to increased evapotranspiration; nighttime warming correlates with latitude and inversely with rainfall.

Conclusions:

  • Afforestation causes significant daytime cooling but moderate nighttime warming.
  • Net warming occurs in dry regions due to nighttime warming offsetting daytime cooling.
  • Strategic site selection is essential for maximizing the climatic benefits of future afforestation projects.