Earlier leaf-out warms air in the north
Xiyan Xu,
William J. Riley,
Charles D. Koven,
Gensuo Jia () and
Xiaoyan Zhang
Additional contact information
Xiyan Xu: Institute of Atmospheric Physics, Chinese Academy of Sciences
William J. Riley: Lawrence Berkeley National Laboratory
Charles D. Koven: Lawrence Berkeley National Laboratory
Gensuo Jia: Institute of Atmospheric Physics, Chinese Academy of Sciences
Xiaoyan Zhang: Nanjing University of Information Science and Technology
Nature Climate Change, 2020, vol. 10, issue 4, 370-375
Abstract:
Abstract Earlier leaf-out in response to climate warming has been recorded in northern temperate and boreal regions. In turn, this shift modifies climate by altering seasonal cycles of surface energy, water and carbon budgets. Here, we use the Community Earth System Model 1.2 to investigate climate feedbacks from advanced leaf-out in northern temperate and boreal vegetation. An imposed 12-day earlier leaf-out in this region, consistent with recent observations, enhances annual surface warming in the Northern Hemisphere. We identify warming hotspots in the Canadian Arctic Archipelago (~0.7 °C), east and west edges of Siberia (~0.4 °C) and southeastern Tibetan Plateau (~0.3 °C). We attribute this enhanced warming to combined effects of indirect water vapour, cloud and snow-albedo radiative feedbacks through intensified poleward water vapour transport rather than direct vegetation albedo and latent heat biophysical feedbacks. With continued warming, positive feedbacks between climate and leaf phenology are likely to amplify warming in the northern high latitudes.
Date: 2020
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DOI: 10.1038/s41558-020-0713-4
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