THE ANALYSIS OF SATELLITE MEASUREMENT OF THE VEGETATION INDEX IN THE FOOTHILL AND PLAIN AREAS OF THE RSO-ALANIA

E. Kamenetsky, A. Radionov, V. Timchenko
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Abstract

To analyze the seasonal and long-term variability of the normalized relative vegetation index NDVI, the multichannel MODIS spectroradiometer measurements with a 10x10 km resolution over a 20-year period of time are used. On the territory of the RNO-Alania in the foothill areas and on the plains near the border of the Stavropol Territory five geographical locations are selected, located at different distances from the Northern spurs of the Caucasian Ridge. For each geographical location the sets of time series are obtained for: 16-day NDVI composites, daily temperature at an altitude of 2 m and precipitation for the 20-years period from 01.01.2000 to 31.12.2019. By calculating the integral characteristic for an annual period of time for every location, the series of 20 annual values are obtained. According to the obtained series, three 20-year trends are built and the trend parameters of a first-order polynomial are calculated using the least squares method. The NDVI trend slope switch is observed in the Mozdok-Russkoe location for transition from the time period 2000–2009 to the period 2010–2019, when the slope changes from positive to negative. Similar NDVI trend slope switches are observed for other locations. This may be due changing the level of soil moisture over time, taking into account mainly the downward trends in precipitation. The trend slope of the NDVI integral characteristic 5–15 % increases with the increasing of the distance from the mountain ridge. The temperature trends for all locations are ascending, that indicates an average increase of the number of warm days from year to year. At the same time, the maximum temperature during the summer period does not significantly increase. The trend of the integral characteristic for the amount of precipitation is mainly downward. However, its specific values have a fairly large spread, which means that the amount of precipitation varies significantly from year to year. In addition, the amount of precipitation decreases with distance from mountain ridges. These factors should be taken into account when choosing agricultural products for cultivation and planning additional land-reclamations in the flat and foothill areas on the south of the Russian Federation.
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青藏高原丘陵平原植被指数卫星测量分析
为了分析标准化相对植被指数NDVI的季节和长期变化,使用了分辨率为10 × 10 km的多通道MODIS光谱辐射计20年的测量数据。在阿拉尼亚共和国境内的山麓地区和斯塔夫罗波尔边境线附近的平原上,选择了五个地理位置,它们距离高加索山脊的北端不同距离。对于每个地理位置,分别获得了2000年1月1日至2019年12月31日20年的16天NDVI复合资料、2 m海拔日温度和降水的时间序列集。通过计算每个地点的年周期的积分特征,得到20个年值的序列。根据得到的序列,建立了3个20年的趋势,并用最小二乘法计算了一阶多项式的趋势参数。Mozdok-Russkoe地区NDVI趋势坡度从2000-2009年向2010-2019年转变,坡度由正变为负。在其他地点也观察到类似的NDVI趋势坡度变化。这可能是由于考虑到降水的下降趋势,随着时间的推移土壤湿度水平发生了变化。随着离山脊距离的增加,NDVI积分特征的趋势斜率增大5 ~ 15%。所有地点的温度趋势都是上升的,这表明温暖天数的平均数量逐年增加。与此同时,夏季最高气温没有明显升高。降水量的整体特征趋势以下降为主。但是,其具体值具有相当大的分布,这意味着每年的降水量变化很大。此外,离山脊越远,降水量越少。在俄罗斯联邦南部平原和山麓地区选择用于种植的农产品和规划更多的土地复垦时,应考虑到这些因素。
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