Assessment of changes in the normalized difference vegetation index (NDVI) of farmlands of Stavropol Territory, Russia, during the period of active vegetation in 2020 based on medium spatial resolution images

IF 0.3 Q4 ECOLOGY
S. Savinova, V. Bratkov, I. D. Murashova, P. Klyushin, N. O. Guseynova
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Abstract

Aim. Assess changes in the NDVI of agricultural land in Stavropol Territory under the influence of weather and climate conditions.Methods. Based on earth remote sensing data, the spectral/vegetation index NDVI was calculated. We used data from the Meteor‐M satellite with a spatial resolution of 60 m for the active vegetation period of 2020 (May to September), which made it possible to calculate the NDVI value at different times of the active vegetation period of the main types of agricultural land in the Stavropol Territory. To explain the spatial and temporal variability of NDVI, an analysis of the conditions of heat and moisture supply was carried out using Walter's climatograms at weather stations located in the steppe and semi‐desert landscapes of Stavropol Territory.Results. In 2020, the period of active vegetation in the steppe and semidesert landscapes of Stavropol Territory began in the first ten days of April, when the air temperature rose above +10°С, and ended in mid‐October. In accordance with the change in heat and moisture supply, the NDVI value changed: in general, maximum values were observed in spring and early summer and, as aridity increased, the areas corresponding to low NDVI values increased everywhere. In the steppe zone, where the main crops of winter wheat are located, the NDVI value decreased from 0.45–0.3 at the beginning of the active vegetation period to 0.15 at the end. NDVI values of 0.15–0.30, corresponding to different types of herbaceous vegetation, prevailed at the end of the active vegetation period.Conclusion. The spatial and temporal distribution of the NDVI value over the territory of the Stavropol Territory reflects, first of all, changes in the conditions of heat and moisture supply. The timing of the course of the phenological phases of natural and cultivated vegetation depends on the latter. 2020 was characterized by sufficient moisture at the beginning of active vegetation, as reflected in the high density of seedlings, and, accordingly, a large area of NDVI, corresponding not only to herbaceous, but also to shrubby vegetation within the steppe landscapes. The increase in moisture deficit and harvesting in the second half and end of summer leveled the differences between the steppe and semi‐desert landscapes, since the maximum areas were occupied by territories with NDVI values of 0.15–0.3.
基于中分辨率影像的俄罗斯斯塔夫罗波尔地区2020年植被活跃期农田归一化植被指数(NDVI)变化
的目标。评估天气和气候条件影响下斯塔夫罗波尔地区农业用地NDVI的变化。基于地球遥感数据,计算了光谱/植被指数NDVI。利用流星- M卫星2020年(5 - 9月)植被活跃期60 M空间分辨率数据,计算了斯塔夫罗波尔地区主要农用地不同时期植被活跃期的NDVI值。为了解释NDVI的时空变化,利用位于斯塔夫罗波尔地区草原和半沙漠景观的气象站的Walter气候图对热量和水分供应条件进行了分析。2020年,斯塔夫罗波尔境内草原和半沙漠景观的植被活动期开始于4月上旬,当时气温上升至+10°С以上,并于10月中旬结束。NDVI值随热、湿供应的变化而变化,总体上在春季和初夏出现最大值,随着干旱程度的增加,低NDVI值对应的面积也普遍增加。在以冬小麦为主要作物的草原地带,植被活跃期开始时NDVI值为0.45 ~ 0.3,后期NDVI值为0.15。植被活跃期结束时NDVI值为0.15 ~ 0.30,与不同类型的草本植被相对应。斯塔夫罗波尔领土上NDVI值的时空分布首先反映了热量和水分供应条件的变化。自然植被和人工植被物候阶段过程的时间取决于后者。2020年植被活跃初期水分充足,幼苗密度高,NDVI面积大,不仅对应于草原景观中的草本植被,也对应于草原景观中的灌木植被。由于NDVI值在0.15-0.3之间的区域占据了最大的面积,因此夏末和夏末的水分亏缺和收获量的增加使草原和半沙漠景观之间的差异趋于平衡。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
0.80
自引率
50.00%
发文量
73
审稿时长
8 weeks
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