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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Empirical evidence of El Nino-Southern Oscillation influence on land surface phenology and productivity in the western United States
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Empirical evidence of El Nino-Southern Oscillation influence on land surface phenology and productivity in the western United States

机译:El Nino-南方涛动对美国西部土地表物候和生产力影响的经验证据

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摘要

Timing of plant life cycle events (phenology) and annual plant productivity represent key interactions between the climate system and the biosphere, with implications and feedbacks for climate and ecosystem functions. The El Nino-Southern Oscillation (ENSO) system is a dominant source of interannual climate variability in the western United States, with important effects on temperature, precipitation, and drought. In this study, we examine the connection between ENSO and terrestrial vegetation dynamics using MOD17 annual net primary productivity (NPP) and land surface phenology derived from MODIS and AVHRR vegetation indices. Three phenology metrics-start of growing season (SOS), end of growing season (EOS), and length of growing season (LOS)-were estimated separately for El Nino and La Nina years by fitting difference logistic functions to split-sample time series of the MODIS enhanced vegetation index (for the period 2000-2011) and AVHRR-derived 3rd generation GIMMS NDVI (NDVI3g) for two temporal periods (2000-2011 and 1982-2011). El Nino events were associated with a significantly earlier SOS than La Nina events in most regions of the western U.S. ENSO-related differences in timing of the end of growing season were generally smaller and more heterogeneous. ENSO impacts on total length of the growing season tended to be spatially heterogeneous but mostly positive in El Nino years. Relative to La Nina events, El Nino events were generally associated with significantly higher NPP in each ecoregion (with mean differences ranging from 2 to 45 gC m(-2) year(-1)). The correlation between total annual production and the Southern Oscillation Index was highest in mid- to late-winter prior to the growing season, suggesting some predictive power in advance of the growing season. These results suggest that future intensification of the ENSO system could have serious consequences for terrestrial ecosystems in the western U.S., especially in regions where ENSO already has a strong impact on interannual climate variability and vegetation dynamics. (C) 2014 Elsevier Inc. All rights reserved.
机译:植物生命周期事件(物候)和植物年生产力的时间是气候系统与生物圈之间的关键相互作用,对气候和生态系统功能具有影响和反馈。 El Nino-Southern Oscillation(ENSO)系统是美国西部年际气候变化的主要来源,对温度,降水和干旱具有重要影响。在这项研究中,我们使用MOD17年净初级生产力(NPP)以及从MODIS和AVHRR植被指数得出的地表物候学,研究了ENSO与陆地植被动态之间的联系。通过将差异逻辑函数拟合到分割样本时间序列来分别估计El Nino和La Nina年的三个物候指标-生长季开始(SOS),生长季结束(EOS)和生长季长度(LOS) MODIS增强植被指数(2000-2011年期间)和AVHRR衍生的第三代GIMMS NDVI(NDVI3g)在两个时间周期(2000-2011年和1982-2011年)中的变化。在美国西部的大多数地区,厄尔尼诺事件与拉尼娜事件的发生明显比拉尼娜事件更早。与ENSO有关的生长季节结束时机的差异通常较小,且异质性更高。 ENSO对生长期总长度的影响在空间上往往是异质的,但在厄尔尼诺时代则大多是积极的。相对于拉尼娜事件,厄尔尼诺事件通常与每个生态区域的NPP显着较高相关(平均差异范围为2至45 gC m(-2)年(-1))。在生长季节之前的冬季中期至晚期,年总产量与南方涛动指数之间的相关性最高,这表明在生长季节之前有一定的预测能力。这些结果表明,ENSO系统的未来集约化可能会对美国西部的陆地生态系统产生严重后果,特别是在ENSO已经对年际气候变化和植被动态产生重大影响的地区。 (C)2014 Elsevier Inc.保留所有权利。

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