...
首页> 外文期刊>Land >Ecosystem Productivity and Water Stress in Tropical East Africa: A Case Study of the 2010–2011 Drought
【24h】

Ecosystem Productivity and Water Stress in Tropical East Africa: A Case Study of the 2010–2011 Drought

机译:东非热带地区的生态系统生产力和水分胁迫:以2010-2011年干旱为例

获取原文
           

摘要

Characterizing the spatiotemporal patterns of ecosystem responses to drought is important in understanding the impact of water stress on tropical ecosystems and projecting future land cover transitions in the East African tropics. Through the analysis of satellite measurements of solar-induced chlorophyll fluorescence (SIF) and the normalized difference vegetation index (NDVI), soil moisture, rainfall, and reanalysis data, here we characterize the 2010–2011 drought in tropical East Africa. The 2010–2011 drought included the consecutive failure of rainy seasons in October–November–December 2010 and March–April–May 2011 and extended further east and south compared with previous regional droughts. During 2010–2011, SIF, a proxy of ecosystem productivity, showed a concomitant decline (~32% lower gross primary productivity, or GPP, based on an empirical SIF–GPP relationship, as compared to the long-term average) with water stress, expressed by lower precipitation and soil moisture. Both SIF and NDVI showed a negative response to drought, and SIF captured the response to soil moisture with a lag of 16 days, even if it had lower spatial resolution and much smaller energy compared with NDVI, suggesting that SIF can also serve as an early indicator of drought in the future. This work demonstrates the unique characteristics of the 2010–2011 East African drought and the ability of SIF and NDVI to track the levels of water stress during the drought.
机译:表征生态系统对干旱的反应的时空模式,对于了解水分胁迫对热带生态系统的影响以及预测东非热带地区未来的土地覆盖变化非常重要。通过对卫星测量的太阳诱发的叶绿素荧光(SIF)和归一化差异植被指数(NDVI),土壤湿度,降雨量以及再分析数据进行分析,在这里我们可以表征2010-2011年东非热带地区的干旱。 2010-2011年的干旱包括2010年10月-11月-12月和2011年3月-4月-2011年5月的雨季连续失败,与以前的区域干旱相比,东部和南部地区进一步扩大。在2010-2011年期间,作为生态系统生产力的代表的SIF在伴随水分胁迫的情况下出现了伴随的下降(与长期平均值相比,基于经验的SIF-GPP关系,总初级生产力或GPP降低了约32%) ,以较低的降水量和土壤湿度表示。 SIF和NDVI均显示出对干旱的负响应,即使与NDVI相比空间分辨率较低且能量要小得多,SIF仍能在16天的滞后时间内捕获到对土壤水分的响应,这表明SIF也可以作为早期干旱。未来干旱的指标。这项工作证明了2010-2011年东非干旱的独特特征以及SIF和NDVI追踪干旱期间水分胁迫水平的能力。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号