首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Spatio-temporal variability of vegetation cover over Morocco (1982-2008): linkages with large scale climate and predictability
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Spatio-temporal variability of vegetation cover over Morocco (1982-2008): linkages with large scale climate and predictability

机译:摩洛哥植被覆盖的时空变化(1982-2008年):与大规模气候和可预测性的联系

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摘要

The dominant patterns of vegetation cover interannual variability over Morocco are isolated using rotated extended empirical orthogonal functions applied to AVHRR NDVI data (1982-2008). The three leading modes capture the NDVI signal at the vegetation peak for three distinct locations: mode 1 (18.7% of total variance) is located along the Atlantic coastline, mode 2 (13.1%) is southwest of the Riff Mountain whilst mode 3 (11.2%) is along the Mediterranean coastline. Correlations between the NDVI time coefficients for the modes 'Atlantic' and 'Mediterranean' dominated by annuals and precipitation amount during the early stage of the vegetation cycle (NDJ) are found. Significant fluctuations of NDVI time coefficients are isolated: a quasi-biennial signal is present in the three modes and an additional quasiquadriennial (~4.4 years) signal is identified for the 'Atlantic' mode only. Connection between vegetation activity and atmospheric and oceanic climate signals are sought using time-lag correlation analyses. The NAO during fall-beginning of winter (NDJ) is found to impact vegetation peak for the 'Atlantic' mode while the Scandinavian Pattern is related to NDVI peak over the 'Atlantic' and 'Riff' latter in the season (DJF). A significant connection is also found between vegetation over the 'Atlantic' mode and the 'Riff' and the 'Atlantic Ni?o' mode leading the SST variability in the equatorial Atlantic with a 6-months lag. Finally, linkages between NDVI and climate information are used to build a seasonal prediction model for NDVI using multiple linear regression. The NDVI anomalies during March-April may be predicted with a reasonable accuracy from January with 79% of explained variance, 60% and 72% for the 'Atlantic', the 'Riff' and the 'Mediterranean' regions, respectively. Results have (1) direct impacts for a better understanding of the role of large-scale climate signals on vegetation cover over Morocco and (2) contribute to the implementation of an agricultural early warning system.
机译:使用应用于AVHRR NDVI数据(1982-2008年)的旋转扩展经验正交函数,可以分离出摩洛哥植被覆盖率年际变化的主要格局。三种主要模式捕获了三个不同位置的植被峰值处的NDVI信号:模式1(占总方差的18.7%)位于大西洋沿岸,模式2(占总方差的13.1%)位于里夫山西南,而模式3(占11.2) %)沿地中海海岸线。在植被周期(NDJ)的早期阶段,以年和降水量为主的模式“大西洋”和“地中海”的NDVI时间系数之间存在相关性。 NDVI时间系数的显着波动被隔离:在这三种模式中存在准两年期信号,并且仅针对“大西洋”模式确定了另外的准四年期(约4.4年)信号。使用时滞相关分析来寻找植被活动与大气和海洋气候信号之间的联系。发现冬季(NDJ)初秋时的NAO影响“大西洋”模式的植被高峰,而斯堪的纳维亚模式与该季节(DJF)后期的“大西洋”和“ Riff”的NDVI高峰相关。在“大西洋”模式与“ Riff”模式和“大西洋Ni?o”模式之间的植被之间也发现了显着的联系,导致赤道大西洋海表温度的变化滞后了六个月。最后,将NDVI与气候信息之间的联系用于使用多元线性回归建立NDVI的季节性预测模型。从1月开始,可以预测3月至4月的NDVI异常,以合理的准确度解释了79%的解释方差,“大西洋”,“ Riff”和“地中海”地区的NDVI异常分别为60%和72%。结果具有(1)直接影响,可以更好地理解大规模气候信号对摩洛哥植被覆盖的作用,(2)有助于实施农业预警系统。

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