Preprints
https://doi.org/10.5194/egusphere-2026-3814
https://doi.org/10.5194/egusphere-2026-3814
22 Jul 2026
 | 22 Jul 2026
Status: this preprint is open for discussion and under review for SOIL (SOIL).

Soil moisture as the dominant driver of CO₂ efflux in Mediterranean urban green spaces: evidence for a Gaussian temperature response and mechanistic modelling of moisture and temperature interactions

Teresa Alía, Sergio González-Ubierna, Abel Sánchez-Jiménez, Rubén Abad-Calderón, and Miguel Ángel Casermeiro

Abstract. Soil respiration, the release of carbon dioxide (CO₂) from the soil to the atmosphere, is a major component of the global carbon cycle, yet its dynamics in urban Mediterranean environments remain poorly understood. This study investigated the effects of soil temperature, soil moisture, and plant community identity on soil CO₂ efflux in urban green spaces of Madrid (Spain), a city with a Mediterranean climate characterized by pronounced summer drought. Four dominant ruderal plant communities (Diplotaxis virgata, Hordeum leporinum, Malva spp, and Dactylis glomerata) were monitored across three urban parks, with CO₂ efflux, temperature, and moisture measured biweekly over one year using an infrared gas analyzer. Contrary to the Q₁₀ exponential assumption, soil respiration showed a Gaussian relationship with temperature, with a positive correlation below a breakpoint of 18.4 °C and a negative effect above this threshold, consistent across plant communities. Soil respiration exhibited a positive exponential relationship with soil moisture and a logarithmic relationship with a rewetting index for values below 20. A mechanistic model described soil respiration as the joint outcome of temperature-driven moisture loss and moisture-stimulated CO₂ emissions. Plant community identity had a limited effect, with the exception of Malva spp., which consistently produced higher emissions. These findings challenge the universal applicability of temperature-based respiration models and highlight soil moisture as the dominant driver of CO₂ efflux in water-limited urban ecosystems. As climate change is expected to intensify both the urban heat island effect and summer drought in Mediterranean cities, soil moisture emerges as a critical variable for projecting urban soil CO₂ fluxes and for designing evidence-based management strategies for Mediterranean urban green spaces, including improved soil infiltration capacity, moisture-sensitive irrigation planning, and the incorporation of moisture-temperature coupling into urban carbon monitoring protocols.

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Teresa Alía, Sergio González-Ubierna, Abel Sánchez-Jiménez, Rubén Abad-Calderón, and Miguel Ángel Casermeiro

Status: open (until 02 Sep 2026)

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Teresa Alía, Sergio González-Ubierna, Abel Sánchez-Jiménez, Rubén Abad-Calderón, and Miguel Ángel Casermeiro
Teresa Alía, Sergio González-Ubierna, Abel Sánchez-Jiménez, Rubén Abad-Calderón, and Miguel Ángel Casermeiro
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Latest update: 22 Jul 2026
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Short summary
Urban parks store and release carbon, but what controls this process in Mediterranean cities remains poorly understood. We monitored carbon dioxide emissions from soils in three Madrid parks over one year and found that soil moisture, not temperature, is the main driver. Surprisingly, emissions declined at high temperatures, not because heat suppresses soil life, but because hot summers dry out the soil. Keeping urban soils moist is key to managing their carbon balance under climate change.
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