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沙漠植被对降雨梯度上降水模式的生产力响应。

Productivity responses of desert vegetation to precipitation patterns across a rainfall gradient.

作者信息

Li Fang, Zhao Wenzhi, Liu Hu

机构信息

Linze Inland River Basin Research Station, Key Laboratory of Inland River Basin Ecohydrology, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, 320 Dong-gang West Road, Lanzhou, 730000, China.

出版信息

J Plant Res. 2015 Mar;128(2):283-94. doi: 10.1007/s10265-014-0685-4. Epub 2015 Jan 23.

Abstract

The influences of previous-year precipitation and episodic rainfall events on dryland plants and communities are poorly quantified in the temperate desert region of Northwest China. To evaluate the thresholds and lags in the response of aboveground net primary productivity (ANPP) to variability in rainfall pulses and seasonal precipitation along the precipitation-productivity gradient in three desert ecosystems with different precipitation regimes, we collected precipitation data from 2000 to 2012 in Shandan (SD), Linze (LZ) and Jiuquan (JQ) in northwestern China. Further, we extracted the corresponding MODIS Normalized Difference Vegetation Index (NDVI, a proxy for ANPP) datasets at 250 m spatial resolution. We then evaluated different desert ecosystems responses using statistical analysis, and a threshold-delay model (TDM). TDM is an integrative framework for analysis of plant growth, precipitation thresholds, and plant functional type strategies that capture the nonlinear nature of plant responses to rainfall pulses. Our results showed that: (1) the growing season NDVIINT (INT stands for time-integrated) was largely correlated with the warm season (spring/summer) at our mildly-arid desert ecosystem (SD). The arid ecosystem (LZ) exhibited a different response, and the growing season NDVIINT depended highly on the previous year's fall/winter precipitation and ANPP. At the extremely arid site (JQ), the variability of growing season NDVIINT was equally correlated with the cool- and warm-season precipitation; (2) some parameters of threshold-delay differed among the three sites: while the response of NDVI to rainfall pulses began at about 5 mm for all the sites, the maximum thresholds in SD, LZ, and JQ were about 55, 35 and 30 mm respectively, increasing with an increase in mean annual precipitation. By and large, more previous year's fall/winter precipitation, and large rainfall events, significantly enhanced the growth of desert vegetation, and desert ecosystems should be much more adaptive under likely future scenarios of increasing fall/winter precipitation and large rainfall events. These results highlight the inherent complexity in predicting how desert ecosystems will respond to future fluctuations in precipitation.

摘要

在中国西北温带沙漠地区,上一年降水量和突发性降雨事件对旱地植物及群落的影响尚未得到充分量化。为了评估在三种不同降水模式的沙漠生态系统中,沿降水 - 生产力梯度,地上净初级生产力(ANPP)对降雨脉冲和季节性降水变化响应的阈值和滞后情况,我们收集了中国西北山丹(SD)、临泽(LZ)和酒泉(JQ)2000年至2012年的降水数据。此外,我们提取了空间分辨率为250米的相应MODIS归一化植被指数(NDVI,作为ANPP的替代指标)数据集。然后,我们使用统计分析和阈值 - 延迟模型(TDM)评估了不同沙漠生态系统的响应。TDM是一个用于分析植物生长、降水阈值和植物功能类型策略的综合框架,能够捕捉植物对降雨脉冲响应的非线性特征。我们的结果表明:(1)在我们的半干旱沙漠生态系统(SD)中,生长季NDVIINT(INT代表时间积分)在很大程度上与暖季(春季/夏季)相关。干旱生态系统(LZ)表现出不同的响应,生长季NDVIINT高度依赖于上一年秋冬的降水量和ANPP。在极端干旱地区(JQ),生长季NDVIINT的变化与冷季和暖季降水同样相关;(2)三个地点的阈值 - 延迟的一些参数有所不同:虽然所有地点NDVI对降雨脉冲的响应均始于约5毫米,但SD、LZ和JQ的最大阈值分别约为55、35和30毫米,随年平均降水量增加而增加。总体而言,上一年秋冬更多的降水量和大降雨事件显著促进了沙漠植被的生长,在未来秋冬降水量增加和大降雨事件可能出现的情况下,沙漠生态系统应更具适应性。这些结果凸显了预测沙漠生态系统如何应对未来降水波动的内在复杂性。

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