Department of Organismic and Evolutionary Biology, Harvard University, 22 Divinity Avenue, Cambridge, MA, 02138, USA.
Department of Earth and Environment, Boston University, 675 Commonwealth Avenue, Boston, MA, 02215, USA.
Glob Chang Biol. 2016 Nov;22(11):3675-3688. doi: 10.1111/gcb.13326. Epub 2016 May 14.
A spring phenology model that combines photoperiod with accumulated heating and chilling to predict spring leaf-out dates is optimized using PhenoCam observations and coupled into the Community Land Model (CLM) 4.5. In head-to-head comparison (using satellite data from 2003 to 2013 for validation) for model grid cells over the Northern Hemisphere deciduous broadleaf forests (5.5 million km ), we found that the revised model substantially outperformed the standard CLM seasonal-deciduous spring phenology submodel at both coarse (0.9 × 1.25°) and fine (1 km) scales. The revised model also does a better job of representing recent (decadal) phenological trends observed globally by MODIS, as well as long-term trends (1950-2014) in the PEP725 European phenology dataset. Moreover, forward model runs suggested a stronger advancement (up to 11 days) of spring leaf-out by the end of the 21st century for the revised model. Trends toward earlier advancement are predicted for deciduous forests across the whole Northern Hemisphere boreal and temperate deciduous forest region for the revised model, whereas the standard model predicts earlier leaf-out in colder regions, but later leaf-out in warmer regions, and no trend globally. The earlier spring leaf-out predicted by the revised model resulted in enhanced gross primary production (up to 0.6 Pg C yr ) and evapotranspiration (up to 24 mm yr ) when results were integrated across the study region. These results suggest that the standard seasonal-deciduous submodel in CLM should be reconsidered, otherwise substantial errors in predictions of key land-atmosphere interactions and feedbacks may result.
一种将光周期与累积加热和冷却相结合的春季物候模型,用于预测春季叶片展开日期,该模型使用 PhenoCam 观测结果进行了优化,并耦合到了社区土地模型(CLM)4.5 中。在对北半球落叶阔叶林(550 万平方千米)的模型网格单元进行的直接比较(使用 2003 年至 2013 年的卫星数据进行验证)中,我们发现,与标准的 CLM 季节落叶春季物候子模型相比,修订后的模型在粗(0.9×1.25°)和细(1 千米)尺度上都有了显著的改进。修订后的模型还更好地代表了 MODIS 观测到的全球近期(十年)物候趋势,以及 PEP725 欧洲物候数据集的长期趋势(1950-2014 年)。此外,正向模型运行表明,到 21 世纪末,修订后的模型的春季叶片展开将提前(多达 11 天)。对于修订后的模型,整个北半球北方和温带落叶林地区的落叶林都预测出更早的提前趋势,而标准模型则预测出较冷地区的叶片展开更早,较暖地区的叶片展开更晚,全球则没有趋势。修订后的模型预测的春季叶片展开较早,导致研究区域内的总初级生产力(高达 0.6PgCyr)和蒸散量(高达 24mmyr)增加。这些结果表明,CLM 中的标准季节落叶子模型应该重新考虑,否则可能会导致对关键陆地-大气相互作用和反馈的预测出现重大误差。