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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Modeling growing season phenology in North American forests using seasonal mean vegetation indices from MODIS
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Modeling growing season phenology in North American forests using seasonal mean vegetation indices from MODIS

机译:使用MODIS的季节平均植被指数模拟北美森林的生长季节物候

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The phenology of vegetation exerts an important control over the terrestrial ecosystemcarbon (C) cycle. Remote sensing of key phenological phases in forests (e.g., the spring onset and autumn end of growing season) remains challenging due to noise in time series and the limited seasonal variation of canopy greenness in evergreen forests. Using 94 site-years of C flux data from four deciduous broadleaf forests (DBF) and six evergreen needleleaf forests (ENF) in North America, we examine whether growing season phenology can be remotely sensed from mean vegetation indices (VIs) derived from spring (Apr.–May) and autumn (Sep.–Nov) observations. Five VIs were used based on Moderate Resolution Imaging Spectroradiometer (MODIS) data, including the normalized difference vegetation index (NDVI), the land surface water index (LSWI), the enhanced vegetation index (EVI), the wide dynamic range vegetation index (WDRVI) and the optimized soil-adjusted vegetation index (OSAVI). Our results showthat growing season transitions can be inferred from mean seasonal VIs, though the different VIs varied in their predictive strength across sites and plant functional types. Widely used NDVI and EVI exhibited limited potential in tracking growing season phenology of ENF ecosystems, while indices sensitive to water (i.e., LSWI) or less influenced by soil (i.e., OSAVI) may have unrevealed powers in indicating phenological transitions. OSAVI was shown to be a strong predictor of the end of the growing season in ENF ecosystems, suggesting that this VI may offer a new strategy for modeling the phenology of ENF sites. We conclude that combinations of multiple indices may improve the remote sensing of land surface phenology, as evidenced by the good agreement between modeled and observed growing season transitions and its length in our evaluation.
机译:植被物候对陆地生态系统碳(C)循环起重要控制作用。由于时间序列中的噪声以及常绿森林中冠层绿色度的季节性变化有限,因此对森林关键物候期(例如生长季节的春季发作和秋季末期)的遥感仍具有挑战性。利用来自北美4个落叶阔叶林(DBF)和6个常绿针叶林(ENF)的94个站点年的C通量数据,我们研究了是否可以从春季的平均植被指数(VI)上遥感生长季节的物候。 4月至5月)和秋季(9月至11月)观测。根据中分辨率成像光谱仪(MODIS)数据使用了五个VI,包括归一化差异植被指数(NDVI),地表水指数(LSWI),增强植被指数(EVI),宽动态范围植被指数(WDRVI) )和优化的土壤调整植被指数(OSAVI)。我们的结果表明,尽管不同的VI在不同地点和植物功能类型上的预测强度不同,但可以从平均季节VI推断出生长季节的过渡。广泛使用的NDVI和EVI在追踪ENF生态系统的生长期物候方面表现出有限的潜力,而对水敏感的指标(即LSWI)或受土壤影响较小的指标(即OSAVI)在显示物候过渡方面可能没有揭示能力。事实证明,OSAVI是ENF生态系统生长期结束的有力预测指标,这表明该VI可能为ENF站点物候建模提供新策略。我们得出的结论是,多个指数的组合可能会改善对地表物候的遥感,这在我们的评估中通过模拟和观察到的生长季节过渡及其长度之间的良好一致性来证明。

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