Ιδρυματικό Αποθετήριο
Πολυτεχνείο Κρήτης
Πολυτεχνείο Κρήτης
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| URI | http://purl.tuc.gr/dl/dias/65B5C6F9-CD7F-4BDF-A1C4-DEC124EE2444 | - |
| Αναγνωριστικό | https://journals.lww.com/soilsci/Fulltext/2016/06000/Climate_Induced_Shifts_in_Global_Soil_Temperature.6.aspx | - |
| Αναγνωριστικό | https://doi.org/10.1097/SS.0000000000000156 | - |
| Γλώσσα | en | - |
| Μέγεθος | 9 pages | en |
| Τίτλος | Climate-induced shifts in global soil temperature regimes | en |
| Δημιουργός | Gryllakis Emmanouil | en |
| Δημιουργός | Γρυλλακης Εμμανουηλ | el |
| Δημιουργός | Koutroulis Aristeidis | en |
| Δημιουργός | Κουτρουλης Αριστειδης | el |
| Δημιουργός | Papadimitriou Labrini | en |
| Δημιουργός | Παπαδημητριου Λαμπρινη | el |
| Δημιουργός | Daliakopoulos Ioannis | en |
| Δημιουργός | Δαλιακοπουλος Ιωαννης | el |
| Δημιουργός | Tsanis Giannis | en |
| Δημιουργός | Τσανης Γιαννης | el |
| Εκδότης | Wolters Kluwer Health | en |
| Περίληψη | Soil temperature is a key factor of plant growth and biological enzyme activities occurring in the soil, affected by the land cover, the evapotranspiration rate, the albedo, and the energy budget of the soil surface. In recent decades, efforts have been made to conserve soils against nonsustainable anthropogenic pressures. Changes in climate can impose additional threats on soil sustainability, as global scale soil temperature regime alterations are expected under global warming. Here, data from three well-established global climate models, spanning from 1981 to as far as 2120, are used to force the JULES (Joint UK Land Environment Simulator) model and produce simulations of soil temperature, calculating the water and energy budgets of the land surface. Modeled soil temperature data are used to estimate the climate-induced changes in the global soil temperature regimes at three different global warming levels. The results show significant shifts in the soil temperature regime for extended areas of the world, especially in the northern hemisphere. Pergelic and Cryic areas are reduced, whereas the Mesic and Thermic soils gain large areas in all three studied scenarios. Implications of the warming patterns might indicate the northward shift of various croplands in regions that until now their cultivation was not possible. | en |
| Τύπος | Peer-Reviewed Journal Publication | en |
| Τύπος | Δημοσίευση σε Περιοδικό με Κριτές | el |
| Άδεια Χρήσης | http://creativecommons.org/licenses/by/4.0/ | en |
| Ημερομηνία | 2018-10-12 | - |
| Ημερομηνία Δημοσίευσης | 2016 | - |
| Θεματική Κατηγορία | Climate change | en |
| Θεματική Κατηγορία | Global climate models | en |
| Θεματική Κατηγορία | Joint UK Land Environment Simulator | en |
| Θεματική Κατηγορία | Soil temperature | en |
| Θεματική Κατηγορία | Specific warming levels | en |
| Βιβλιογραφική Αναφορά | M. G. Grillakis, A. G. Koutroulis, L. V. Papadimitriou, I. N. Daliakopoulos and I. K. Tsanis, "Climate-induced shifts in global soil temperature regimes," Soil Sci., vol. 181, no. 6, pp. 264-272, Jun. 2016. doi: 10.1097/SS.0000000000000156 | en |
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