The carbon and water balances of high-elevation (>2500 m) Alpine grasslands still offer important open questions. Understanding whether those grasslands act as a net carbon either source or sink, and quantifying the evapotranspiration – also depending on the meteorological and soil conditions - is still a challenge. In this analysis, a focus on two years of measurements (dry year 2022 and closer to normal conditions 2023) collected at a high elevation grassland site (2600 m a.s.l.) is presented. The interannual variations of ecosystem respiration, gross primary production (GPP), net ecosystem exchange (NEE) and actual evapotranspiration (ETa) give insights on how the ecosystem reacts to different atmospheric and soil conditions, including the Winter snowpack coverage extent, depth and duration. First results show that the greater duration and depth of 2023 Winter snowpack may influence the grassland behaviour, being characterised by a higher emission in early growing season just after the snowmelt. Hence, the grassland sink ability in 2023 (-1.5  gC m-2 ) is strongly reduced, if compared to the 2022 one (-73.4  gC m-2) even if the 2023 year was more wet if compared to very dry 2022. Limiting the analysis to the period January-October (end of the very late growing season), results indicate that the cumulative ecosystem respiration reaches 420.0 gC m-2 in 2023 whereas in 2022, the cumulative value is 345 gC m-2. GPP cumulative values are instead -454 gC m-2 and -469.1 gC m-2 in 2022 and 2023, respectively.Considering the most important part of the growing season (June-September), the cumulative ETa does not show particular differences among the two years. In addition, the ETa and NEE drivers can be analysed. Results indicate that the most significant drivers are net radiation, air temperature, wind speed, matric potential and ground heat flux for ETa. Photosynthetic photon flux density, vapour pressure deficit, soil temperature and soil water content are the most important drivers for NEE.

Year-round eco-hydrological monitoring of a high-elevation Alpine grassland / Gisolo, Davide; Gentile, Alessio; Hamza, Tanzeel; Bechis, Stefano; Canone, Davide; Ferraris, Stefano. - (2025). ( EGU General Assembly 2025 Vienna 27 aprile - 2 maggio 2025) [10.5194/egusphere-egu25-17896].

Year-round eco-hydrological monitoring of a high-elevation Alpine grassland

Davide Gisolo;ALESSIO GENTILE;Tanzeel Hamza;Stefano Bechis;Davide Canone;Stefano Ferraris
2025

Abstract

The carbon and water balances of high-elevation (>2500 m) Alpine grasslands still offer important open questions. Understanding whether those grasslands act as a net carbon either source or sink, and quantifying the evapotranspiration – also depending on the meteorological and soil conditions - is still a challenge. In this analysis, a focus on two years of measurements (dry year 2022 and closer to normal conditions 2023) collected at a high elevation grassland site (2600 m a.s.l.) is presented. The interannual variations of ecosystem respiration, gross primary production (GPP), net ecosystem exchange (NEE) and actual evapotranspiration (ETa) give insights on how the ecosystem reacts to different atmospheric and soil conditions, including the Winter snowpack coverage extent, depth and duration. First results show that the greater duration and depth of 2023 Winter snowpack may influence the grassland behaviour, being characterised by a higher emission in early growing season just after the snowmelt. Hence, the grassland sink ability in 2023 (-1.5  gC m-2 ) is strongly reduced, if compared to the 2022 one (-73.4  gC m-2) even if the 2023 year was more wet if compared to very dry 2022. Limiting the analysis to the period January-October (end of the very late growing season), results indicate that the cumulative ecosystem respiration reaches 420.0 gC m-2 in 2023 whereas in 2022, the cumulative value is 345 gC m-2. GPP cumulative values are instead -454 gC m-2 and -469.1 gC m-2 in 2022 and 2023, respectively.Considering the most important part of the growing season (June-September), the cumulative ETa does not show particular differences among the two years. In addition, the ETa and NEE drivers can be analysed. Results indicate that the most significant drivers are net radiation, air temperature, wind speed, matric potential and ground heat flux for ETa. Photosynthetic photon flux density, vapour pressure deficit, soil temperature and soil water content are the most important drivers for NEE.
File in questo prodotto:
Non ci sono file associati a questo prodotto.
Pubblicazioni consigliate

I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11583/3008992
 Attenzione

Attenzione! I dati visualizzati non sono stati sottoposti a validazione da parte dell'ateneo