Valmassoi, Arianna
(2016)
Impact of irrigation in the Po valley (Italy) on meteorological parameters through numerical simulation.
[Laurea magistrale], Università di Bologna, Corso di Studio in
Fisica del sistema terra [LM-DM270], Documento ad accesso riservato.
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Abstract
Recent studies found that soil-atmosphere coupling features, through soil moisture, have been crucial to simulate well heat waves amplitude, duration and intensity.
Moreover, it was found that soil moisture depletion both in Winter and Spring anticipates strong heat waves during the Summer. Irrigation in geophysical studies can be intended as an anthropogenic forcing to the soil-moisture, besides changes in land proprieties.
In this study, the irrigation was add to a LAM hydrostatic model (BOLAM) and coupled with the soil.
The response of the model to irrigation perturbation is analyzed during a dry Summer season.
To identify a dry Summer, with overall positive temperature anomalies, an extensive climatological characterization of 2015 was done.
The method included a statistical validation on the reference period distribution used to calculate the anomalies.
Drought conditions were observed during Summer 2015 and previous seasons, both on the analyzed region and the Alps.
Moreover July was characterized as an extreme event for the referred distribution.
The numerical simulation consisted on the summer season of 2015 and two run: a control run (CTR), with the soil coupling and a perturbed run (IPR).
The perturbation consists on a mask of land use created from the Cropland FAO dataset, where an irrigation water flux of 3 mm/day was applied from 6 A.M. to 9 A.M. every day.
The results show that differences between CTR and IPR has a strong daily cycle. The main modifications are on the air masses proprieties, not on to the dynamics. However, changes in the circulation at the boundaries of the Po Valley are observed, and a diagnostic spatial correlation of variable differences shows that soil moisture perturbation explains well the variation observed in the 2 meters height temperature and in the latent heat fluxes.On the other hand, does not explain the spatial shift up and downslope observed during different periods of the day.
Given the results, irrigation process affects the atmospheric proprieties on a larger scale than the irrigation, therefore it is important in daily forecast, particularly during hot and dry periods.
Abstract
Recent studies found that soil-atmosphere coupling features, through soil moisture, have been crucial to simulate well heat waves amplitude, duration and intensity.
Moreover, it was found that soil moisture depletion both in Winter and Spring anticipates strong heat waves during the Summer. Irrigation in geophysical studies can be intended as an anthropogenic forcing to the soil-moisture, besides changes in land proprieties.
In this study, the irrigation was add to a LAM hydrostatic model (BOLAM) and coupled with the soil.
The response of the model to irrigation perturbation is analyzed during a dry Summer season.
To identify a dry Summer, with overall positive temperature anomalies, an extensive climatological characterization of 2015 was done.
The method included a statistical validation on the reference period distribution used to calculate the anomalies.
Drought conditions were observed during Summer 2015 and previous seasons, both on the analyzed region and the Alps.
Moreover July was characterized as an extreme event for the referred distribution.
The numerical simulation consisted on the summer season of 2015 and two run: a control run (CTR), with the soil coupling and a perturbed run (IPR).
The perturbation consists on a mask of land use created from the Cropland FAO dataset, where an irrigation water flux of 3 mm/day was applied from 6 A.M. to 9 A.M. every day.
The results show that differences between CTR and IPR has a strong daily cycle. The main modifications are on the air masses proprieties, not on to the dynamics. However, changes in the circulation at the boundaries of the Po Valley are observed, and a diagnostic spatial correlation of variable differences shows that soil moisture perturbation explains well the variation observed in the 2 meters height temperature and in the latent heat fluxes.On the other hand, does not explain the spatial shift up and downslope observed during different periods of the day.
Given the results, irrigation process affects the atmospheric proprieties on a larger scale than the irrigation, therefore it is important in daily forecast, particularly during hot and dry periods.
Tipologia del documento
Tesi di laurea
(Laurea magistrale)
Autore della tesi
Valmassoi, Arianna
Relatore della tesi
Correlatore della tesi
Scuola
Corso di studio
Ordinamento Cds
DM270
Parole chiave
Modeling, heat waves, irrigation, 2015, climatological characterization
Data di discussione della Tesi
31 Marzo 2016
URI
Altri metadati
Tipologia del documento
Tesi di laurea
(NON SPECIFICATO)
Autore della tesi
Valmassoi, Arianna
Relatore della tesi
Correlatore della tesi
Scuola
Corso di studio
Ordinamento Cds
DM270
Parole chiave
Modeling, heat waves, irrigation, 2015, climatological characterization
Data di discussione della Tesi
31 Marzo 2016
URI
Gestione del documento: