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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:使用中亚NDVI / ENSO异常的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:EL Nino-Southern振荡(ENSO)时间动态的调查及中亚干旱和半干旱区干旱/湿润时期的空间模式及其与归一化差异植被指数(NDVI)的关系(1982-2011)在本文中探讨。为了确定期刊振荡及其与NDVI值的关系,选择了EL Nino 3.4索引和三十年的新一代Bi-Weynly NDVI 3G,由先进的非常高分辨率辐射计(AVHRR)卫星时间序列数据获得。基于识别oni(海洋Nino指数)是1982-1983,1997-1998期间观察到的一个非常强壮的El Nino(温暖的)异常,1988-1989年录得非常强大的La Nino(酷)期间事件。相关性,这两个因素并寻求积极和消极趋势,它从NDVI时间序列数据提取为“低生产率期”持续多年:1982-1983,1997 -1998;并作为“高生产率期”持续多年:1988 -1989。线性回归观察温度事件作为中等阶段期间在中等El Nino(ME)和NDVI之间选择的中等相周期,随后的时间:1986-1987; 1987-1988; 1991-1992; 2002-2003; 2009-2010;和中度La Nina(ML)期间和NDVI(1998-1999; 1999-2000; 2007-2008),其研究了湿度条件的空间模式。结果表明,非常强的EL NINO和NDVI之间的反比关系,较大的正面值较大的植被响应减少;在极强的La Nina和NDVI之间的直接关系,增加了较少的负面oni值的植被响应。结果假设这些异常影响对植被生产率的影响。这些结果对于有效的牧场/草地管理是有益的,并提出羊群的评估和减少量的促进期由于缺乏饲存的牲畜群,在牧场上即将到来的牧场群。结果表明,对土地表面植被信号的可变异的非人体化驱动因素,了解,对其有利的牧场和农业管理,以及建立中亚降水驱动的旱地生态系统服务。

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