Articles | Volume 18, issue 7
Biogeosciences, 18, 2275–2287, 2021
https://doi.org/10.5194/bg-18-2275-2021
Biogeosciences, 18, 2275–2287, 2021
https://doi.org/10.5194/bg-18-2275-2021

Research article 08 Apr 2021

Research article | 08 Apr 2021

Divergent climate feedbacks on winter wheat growing and dormancy periods as affected by sowing date in the North China Plain

Fengshan Liu et al.

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A, D., Xiong, K., Zhao, W., Gong, Z., Jing, R., and Zhang, L.: Temporal trend of climate change and mutation analysis of North China Plain during 1960 to 2013, Scientia Geographica Sinica, 36, 1555–1564, 2016 (in Chinese). 
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Bohm, K., Ingwersen, J., Milovac, J., and Streck, T.: Distinguishing between early- and late-covering crops in the land surface model Noah-MP: impact on simulated surface energy fluxes and temperature, Biogeosciences, 17, 2791–2805, https://doi.org/10.5194/bg-17-2791-2020, 2020. 
Boisier, J. P., de Noblet-Ducoudre, N., Pitman, A. J., Cruz, F. T., Delire, C., van den Hurk, B. J. J. M., van der Molen, M. K., Müller, C., and Voldoire, A.: Attributing the impacts of land-cover changes in temperate regions on surface temperature and heat fluxes to specific causes: Results from the first LUCID set of simulations, J. Geophys. Res.-Atmos., 117, D12116, https://doi.org/10.1029/2011JD017106, 2012. 
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The sowing date is key to the surface biophysical processes in the winter dormancy period. The climate effect of the sowing date shift is therefore very interesting and may contribute to the mitigation of climate change. An earlier sowing date always had a higher LAI but a higher temperature in the dormancy period and a lower temperature in the growth period. The main reason was the relative contributions of the surface albedo and energy partitioning processes.
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