Predicting precipitation and NDVI utilization of the multi-level linear mixed-effects model and the CA-markov simulation model
Fatima Belhaj, Hlila Rachid, Abdessalam Ouallali, Aqil Tariq, Abdeldjalil Belkendil, Beroho Mohamed, Hassan Alzahrani, Hajra Mustafa, Hesham El‐Askary
Abstract
• Climate change modifies the distribution of a set of climate variables. • The study proposes scenarios for the evolution of precipitation and NDVI. • Determines their correlation coefficient for the available and predict period. • Decline of dense spaces in the eastern and western parts in 2029 (−12.89%) and 2040 (−12.78%). • Geoinformation and prediction models maximize environmental planning. The current work intends to reconstruct the spatiotemporal evolution of precipitation and the Normalized Differentiate Vegetation Index (NDVI) in the Loukkos watershed and provide scenarios for their recent and future evolution, therefore determining the degree of association. We conducted a study on the time series data of precipitation and NDVI from 1999 to 2019. The NDVI prediction is conducted using the CA-Markov model and the linear mixed-effects multi-level model (LME) with precipitation data from 2019 to 2040. The CA-Markov model was employed to predict the vegetation indices for 2029 and 2040 using 1999, 2009, and 2019 data. The model simulates future precipitation estimates for up to 2040 using different daily precipitation data series obtained from ten meteorological stations between 1999 and 2019. The accuracy of NDVI simulation is evaluated using kappa indices, specifically K location of 88%, K n 0 of 86%, and K s t a n d a r d of 83%, indicating that the consistency between the simulated NDVI map of 2019 and the actual one is nearly perfect, indicating statistical reliability of our model. The precipitation forecast for the Loukkos watershed predicts that average annual precipitation will decrease by 11.4% between 1999 and 2040. In contrast, based on 2019, there will be an increase in low vegetation areas and a decline in dense regions in the eastern and western parts of the basin in 2029 (−12.89%) and 2040 (−12.78%), respectively. The findings of this study suggest that by 2040, the Loukkos watershed will be exposed to future climate hazards, such as reduced precipitation and vegetation. The integration of geoinformation and prediction models is a great resource for optimizing environmental planning to prepare and potentially mitigate the harmful effects of climate change and its consequences for both humanity and the environment.