Description:
Abdi-Basid ADAN, 09–2025
馃幆 The detailed methodology and results can be accessed through this link:
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Abdi-Basid ADAN, 09–2025
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The variables used in the analysis encompass vegetation, climate, and environmental conditions in the Godoria region. The Normalized Difference Vegetation Index (NDVI) reflects vegetation status derived from satellite data, while soil moisture and land surface temperature (LST) provide information on water availability and surface heat. Climatic factors include rainfall, the Standardized Precipitation Index (SPI) as a measure of drought conditions, and both minimum and maximum temperatures (Temp Min and Temp Max), which influence plant physiology and evapotranspiration. Potential evapotranspiration (PET) indicates the potential water deficit driven by climatic conditions. Finally, sea level serves as a relevant oceanographic indicator in the arid coastal context of Djibouti, with potential indirect impacts on local climate dynamics and water availability.
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Fig. 1. (a)Estimation of relative importance of climate variables as predictors of
NDVI. (b) Pearson correlation coefficient between NDVI and climate variables. |
Table 1. Mann Kendall Trend and
Theil-sen slope statistics of NDVI and climate variables from 1987 to 2022.
|
Theil-sen
slope |
p.value |
p.value |
|
NDVI |
0.858 |
0.859 |
||
Sea level |
0.646 |
0.646 |
||
0.000 |
NA |
0.000 |
NA |
|
SPI |
0.000 |
0.917 |
0.000 |
0.917 |
Temp
Min |
0.057 |
0.109 |
0.194 |
0.109 |
Temp
Max |
0.072 |
0.173 |
0.166 |
0.172 |
0.739 |
0.739 |
|||
0.046 |
0.649 |
0.085 |
0.649 |
|
LST |
0.720 |
0.720 |
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Abdi-Basid ADAN, 2025
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This study provides a detailed spatiotemporal analysis of the impacts of early wildfires occurring between February 26 and March 16, 2024, in North America, with a focus on the localities of Stinnett (35.82°N, -101.44°W) and Canadian, TX (35.91°N, -100.38°W). Utilizing data from NetCDF files (v10m, u10m, AOD500nm, t2m, coplev, comlev), the analysis employs the xarray library to process meteorological and atmospheric variables, including aerosol optical depth (AOD at 550 nm), 2-meter temperature (converted to °F), carbon monoxide (CO) at 1000 hPa and model level 1 (in ppb), and 10-meter wind components (u10, v10). Visualizations, created using matplotlib and cartopy, include spatial maps of daily averages of AOD, temperature, and CO, overlaid with wind vectors to illustrate their role in pollutant dispersion. Time series analyses reveal the daily evolution of these variables for both localities, highlighting significant AOD peaks in Stinnett, indicative of smoke plume passage. Hourly heatmaps confirm the immediate impact of wildfires on air quality, showing a marked increase in AOD within hours. Wind rose diagrams, generated for each locality, quantify the frequency and intensity of winds, emphasizing their influence on pollutant spread. Finally, a pixel-by-pixel Pearson correlation analysis between AOD and CO reveals a strong positive relationship (R close to +1) in affected areas, confirming the common origin of aerosols and CO from biomass burning. These findings, contextualized within an extreme meteorological event characterized by high temperatures and dry conditions, underscore the complex interactions between meteorological and atmospheric dynamics, with implications for air quality monitoring and environmental crisis management in North America.
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Abdi-Basid ADAN, 2025
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