Coupling between evapotranspiration, water use efficiency, and evaporative stress index strengthens after wildfires in New Mexico, USA

•ET and ESI increase immediately after a wildfire.•WUE has a decreasing trend during a fire but no correlation.•Post-fire ET and WUE are negatively correlated, but pre-fire ET and WUE are not.•Savannas had a disproportionately high acreage burned in the 2022 New Mexico fires. Examine the effects of...

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Veröffentlicht in:International journal of applied earth observation and geoinformation 2024-12, Vol.135, p.104238, Article 104238
Hauptverfasser: Joshi, Ryan C., Jensen, Annalise, Pascolini-Campbell, Madeleine, Fisher, Joshua B.
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Sprache:eng
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Zusammenfassung:•ET and ESI increase immediately after a wildfire.•WUE has a decreasing trend during a fire but no correlation.•Post-fire ET and WUE are negatively correlated, but pre-fire ET and WUE are not.•Savannas had a disproportionately high acreage burned in the 2022 New Mexico fires. Examine the effects of evapotranspiration (ET), water use efficiency (WUE), and evaporative stress index (ESI) on wildfire temperature and extent. Compare land cover type proportions in burned area with land cover type proportions in New Mexico. We used remotely sensed data from NASA’s ECOsystem and Spaceborne Thermal Radiometer Experiment on Space Station (ECOSTRESS) to collect ET, WUE, & ESI data. Data were analyzed for burned areas of 10 wildfires that occurred in New Mexico between 2020 and 2022, segmenting the following land cover types: evergreen needleleaf forests, closed shrublands, open shrublands, savannas, woody savannas, grasslands, and other. ET & ESI increased throughout the duration of the wildfires, while WUE decreased. ET vs. WUE were more strongly correlated post-fire (R2 = 0.85) than pre-fire (R2 = 0.20), as was WUE vs. ESI (post-fire, R2 = 0.59; pre-fire, R2 = 0.04). Pre- and post-fire ET and ESI were positively correlated (R2 = 0.61 pre-fire, R2 = 0.53 post-fire), while post-fire WUE was negatively correlated with both post-fire ET (R2 = 0.85) and ESI (R2 = 0.59). We found that the land cover composition of the areas burned by the 10 studied wildfires differs from the land cover composition of New Mexico as a whole (p 
ISSN:1569-8432
DOI:10.1016/j.jag.2024.104238