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Climate Dynamics

, Volume 50, Issue 9–10, pp 3745–3755 | Cite as

Vegetation-cloud feedbacks to future vegetation changes in the Arctic regions

  • Mee-Hyun Cho
  • Ah-Ryeon Yang
  • Eun-Hyuk Baek
  • Sarah M. Kang
  • Su-Jong Jeong
  • Jin Young Kim
  • Baek-Min Kim
Article

Abstract

This study investigates future changes in the Arctic region and vegetation-cloud feedbacks simulated using the National Center for Atmospheric Research Community Atmosphere Model Version 3 coupled with a mixed layer ocean model. Impacts of future greening of the Arctic region are tested using altered surface boundary conditions for hypothetical vegetation distributions: (1) grasslands poleward of 60°N replaced by boreal forests and (2) both grasslands and shrubs replaced by boreal forests. Surface energy budget analysis reveals that future greening induces a considerable surface warming effect locally and warming is largely driven by an increase in short wave radiation. Both upward and downward shortwave radiation contribute to positive surface warming: upward shortwave radiation decreases mainly due to the decreased surface albedo (a darker surface) and downward shortwave radiation increases due to reduced cloud cover. The contribution of downward shortwave radiation at surface due to cloud cover reduction is larger than the contribution from surface albedo alone. The increased roughness length also transported surface fluxes to upper layer more efficiently and induce more heating and dry lower atmosphere. A relatively smaller increase in water vapor compared to the large increase in low-level air temperature in the simulation reduces relative humidity and results in reduced cloud cover. Therefore, vegetation-cloud feedbacks induced from land cover change significantly amplify Arctic warming. In addition to previously suggested feedback mechanisms, we propose that the vegetation-cloud feedback should be considered as one of major components that will give rise to an additional positive feedback to Arctic amplification.

Keywords

Arctic greening CAM3 Albedo Roughness Vegetation-cloud feedback 

Notes

Acknowledgements

This study was supported by KMIPA2015-2093 (PN17040) of the Korean government and ‘Development and Application of the Korea Polar Prediction System (KPOPS) for Climate Change and Weather Disaster (PE17130)’ project of the Korea Polar Research Institute. This study was funded by the Ministry of Oceans and Fisheries of the Republic of Korea under the government project, “Quantitative assessment for PM & BC to climate change and development of reduction technology for PM, BC from ships”. Sarah Kang was supported by the National Research Foundation of Korea (NRF) grant funded by the Ministry of Science, ICT & Future Planning (No. 2016R1A1A3A04005520). Su-Jong Jeong was supported by the internal research fund of the South University of Science and Technology of China.

Compliance with ethical standards

Conflict of interest

The authors declare that they have no conflict of interest.

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Copyright information

© Springer-Verlag GmbH Germany 2017

Authors and Affiliations

  • Mee-Hyun Cho
    • 1
  • Ah-Ryeon Yang
    • 2
  • Eun-Hyuk Baek
    • 1
  • Sarah M. Kang
    • 3
  • Su-Jong Jeong
    • 4
  • Jin Young Kim
    • 5
  • Baek-Min Kim
    • 1
  1. 1.Division of Polar Climate ResearchKorea Polar Research InstituteIncheonKorea
  2. 2.Seoul Metropolitan Office of MeteorologySuwonKorea
  3. 3.School of Urban and Environmental EngineeringUNISTUlsanKorea
  4. 4.School of Environmental Science and EngineeringSouth University of Science and Technology of ChinaShenzhenKorea
  5. 5.Green City Technology InstituteKorea Institute of Science and TechnologySeoulKorea

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