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首页> 外文期刊>Global Biogeochemical Cycles >Vapor Pressure Deficit and Sunlight Explain Seasonality of Leaf Phenology and Photosynthesis Across Amazonian Evergreen Broadleaved Forest
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Vapor Pressure Deficit and Sunlight Explain Seasonality of Leaf Phenology and Photosynthesis Across Amazonian Evergreen Broadleaved Forest

机译:水蒸气压差和日照解释了亚马逊常绿阔叶林叶片物候和光合作用的季节性

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Abstract Amazonian evergreen forests show distinct canopy phenology and photosynthetic seasonality but the climatic triggers are not well understood. This imposes a challenge for modeling leaf phenology and photosynthesis seasonality in land surface models (LSMs) across Amazonian evergreen forest biome. On continental scale, we tested two climatic triggers suggested by site observations, vapor pressure deficit (VPD), and short‐wave incoming radiation (SW) for defining leaf shedding and incorporated VPD‐ and SW‐triggered new canopy phenology modules in the ORCHIDEE LSM (hereafter VPD‐AP and SW‐AP versions). Our results show that both VPD and SW are plausible precursors of large scale litterfall seasonality across the basin by comparing against in situ data from 14 sites. Specially, both VPD‐AP and SW‐AP correctly capture the increases in litterfall during the early dry season, followed by a flush of new leaves with increasing photosynthetic rates during the later dry season. The VPD‐AP version performs better than the SW‐AP version in capturing a dry‐season increase of photosynthesis across the wet Amazonia areas where mean annual precipitation exceeds 2,000 mm yr−1, consistent with previous satellite data analysis. Both VPD‐AP and SW‐AP model versions perform well in northern, central and southern Amazon regions where the SW seasonality is unimodal, but miss the seasonality of satellite GPP proxies in the eastern region off the coast of Guyana shield where SW seasonality is bimodal. Our findings imply that atmospheric dryness and sunlight availability likely explain the seasonality of leaf shedding and leaf flush processes, respectively, and consequently control canopy photosynthesis in Amazonian evergreen forests.
机译:摘要 亚马孙常绿林具有明显的冠层物候和光合季节性,但气候触发因素尚不清楚。这给亚马逊常绿森林生物群落地表模型(LSM)的叶片物候和光合作用季节性建模带来了挑战。在大陆尺度上,我们测试了现场观测建议的两个气候触发因素,即蒸气压不足 (VPD) 和短波入射辐射 (SW),用于定义叶片脱落,并在 ORCHIDEE LSM 中纳入了 VPD 和 SW 触发的新冠层物候模块(以下简称 VPD-AP 和 SW-AP 版本)。通过与14个地点的原位数据进行比较,我们的结果表明,VPD和SW都是整个流域大规模凋落物季节性的合理前兆。特别是,VPD-AP和SW-AP都正确地捕捉到了旱季初期凋落物的增加,随后在旱季后期,随着光合速率的增加,新叶的涌动。VPD-AP版本在捕获年平均降水量超过2,000 mm yr-1的亚马逊湿润地区旱季光合作用增加方面表现优于SW-AP版本,这与之前的卫星数据分析一致。VPD-AP 和 SW-AP 模型版本在亚马逊北部、中部和南部地区表现良好,这些地区的西南季节性是单峰的,但在圭亚那地盾海岸附近的东部地区,卫星 GPP 代理的季节性是双峰的。我们的研究结果表明,大气干燥和日照可用性可能分别解释了落叶和冲叶过程的季节性,从而控制了亚马逊常绿森林的冠层光合作用。

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