Urbanization Drives Rising Land Surface Temperatures in Sunland Park, New Mexico
Urbanization Drives Rising Land Surface Temperatures in Sunland Park, New Mexico
US · Published Aug 31, 2026
A study analyzing land surface temperature (LST) and urban heat island (UHI) dynamics in Sunland Park, New Mexico, has revealed significant thermal changes between 2010 and
Using Landsat satellite imagery, researchers observed an increase in urban land from 7.53 km² to 12.23 km², while rangeland decreased from 17.82 km² to 12.30 km². The study found that barren and sparsely vegetated areas experienced the highest daytime LSTs, while urban zones with vegetation showed lower temperatures. A strong inverse relationship between vegetation (measured by the Normalized Difference Vegetation Index, NDVI) and LST (R² = 0.60–0.80) highlighted the cooling effects of greenery. The findings emphasize that urbanization and land management practices significantly influence thermal conditions in arid environments.

Impact & Risks

The increase in urban land and reduction in rangeland in Sunland Park have led to higher daytime temperatures, particularly in barren and sparsely vegetated areas. This intensification of the UHI effect can exacerbate heat-related health risks, increase energy consumption for cooling, and contribute to environmental degradation. The study underscores the importance of vegetation in mitigating these effects, as areas with higher NDVI values experienced lower temperatures due to shading and evapotranspiration. Without sustainable land management practices, the region may face worsening thermal conditions, impacting both human health and local ecosystems.

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