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Monitoring of vegetation condition using the NDVI/ENSO anomalies in Central Asia and their relationships with ONI (very strong) phases

机译:利用中亚的NDVI / ENSO异常监测植被状况及其与ONI(非常强)阶段的关系

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An investigation of temporal dynamics of El Nino-Southern Oscillation (ENSO) and spatial patterns of dryness/wetness period over arid and semi-arid zones of Central Asia and their relationship with Normalized Difference Vegetation Index (NDVI) values (1982-2011) have explored in this article. For identifying periodical oscillations and their relationship with NDVI values have selected El Nino 3.4 index and thirty years of new generation bi-weekly NDVI 3g acquired by the Advanced Very High Resolution Radiometer (AVHRR) satellites time-series data. Based on identification ONI (Oceanic Nino Index) is a very strong El Nino (warm) anomalies observed during 1982-1983, 1997-1998 and very strong La Nino (cool) period events have observed 1988-1989 years. For correlation these two factors and seeking positive and negative trends it has extracted from NDVI time series data as "low productivity period" following years: 1982-1983,1997-1998; and as "high productivity period" following years: 1988 -1989. Linear regression observed warm events as moderate phase period selected between moderate El Nino (ME) and NDVI with following periods:1986-1987; 1987-1988; 1991-1992; 2002-2003; 2009-2010; and moderate La Nina (ML) periods and NDVI (1998-1999; 1999-2000; 2007-2008) which has investigated a spatial patterns of wetness conditions. The results indicated that an inverse relationship between very strong El Nino and NDVI, decreased vegetation response with larger positive ONI value; and direct relationship between very strong La Nina and NDVI, increased vegetation response with smaller negative ONI value. Results assumed that significant impact of these anomalies influenced on vegetation productivity. These results will be a beneficial for efficient rangeland/grassland management and to propose drought periods for assessment and reducing quantity of flocks' due to a lack of fodder biomass for surviving livestock flocks on upcoming years in rangelands. Also results demonstrate that a non-anthropogenic drivers of variability effected to land surface vegetation signals, understanding of which will be beneficial for efficient rangeland and agriculture management and establish ecosystem services in precipitation-driven drylands of Central Asia.
机译:对中亚干旱和半干旱地区的厄尔尼诺-南方涛动(ENSO)的时间动态和干燥/湿润期的空间格局及其与归一化植被指数(NDVI)的关系(1982-2011)的研究本文探讨。为了识别周期性振荡及其与NDVI值的关系,已选择了El Nino 3.4指数,并通过先进超高分辨率辐射计(AVHRR)卫星时间序列数据获得了30年的新一代双周NDVI 3g。根据识别,ONI(海洋Nino指数)是在1982-1983年,1997-1998年期间观测到的非常强烈的El Nino(暖)异常,并且在1988-1989年期间观测到了非常强烈的La Nino(冷)时期事件。为了使这两个因素相互关联并寻找正趋势和负趋势,它从NDVI时间序列数据中提取了以下年份为“低生产力时期”:1982-1983,1997-1998; 2002-1983。并在随后的几年中称为“高生产率时期”:1988 -1989。线性回归观察到暖事件是在中等厄尔尼诺现象(ME)和NDVI之间选择的中等时期,其周期为1986- 1987年; 1987-1988年; 1991-1992年; 2002-2003; 2009-2010;中尼拉(ML)时期和NDVI(1998-1999; 1999-2000; 2007-2008)研究了湿度条件的空间格局。结果表明,非常强的厄尔尼诺现象与NDVI之间存在反比关系,当ONI值为正时,植被响应降低。以及非常强的拉尼娜和NDVI之间的直接关系,以较小的ONI负值增加植被响应。结果假设这些异常现象对植被生产力产生了重大影响。这些结果对于牧场/草地的有效管理将是有益的,并且由于干旱的草料生物量不足,无法在牧场上存活下来,因此建议干旱时期进行评估并减少鸡群的数量。结果还表明,非人为变化的驱动因素影响了地表植被信号,对此的理解将有助于有效的牧场和农业管理,并在中亚降水驱动的干旱地区建立生态系统服务。

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