Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Fabrizio Falasca"'
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-10 (2024)
Abstract The 2015 Paris agreement was established to limit Greenhouse gas (GHG) global warming below 1.5°C above preindustrial era values. Knowledge of climate sensitivity to GHG levels is central for formulating effective climate policies, yet its
Externí odkaz:
https://doaj.org/article/39fbfa5ebf704dbbaf31e57f851614e1
Publikováno v:
Environmental Data Science, Vol 2 (2023)
Studies agree on a significant global mean sea level rise in the 20th century and its recent 21st century acceleration in the satellite record. At regional scale, the evolution of sea level probability distributions is often assumed to be dominated b
Externí odkaz:
https://doaj.org/article/9b3ba7eff10a47bbb31271625e3b265f
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-9 (2021)
Abstract A foundational paradigm in marine ecology is that Oceans are divided into distinct ecoregions demarking unique assemblages of species where the characteristics of water masses, and quantity and quality of environmental resources are generall
Externí odkaz:
https://doaj.org/article/5de846078a704c51830f0f49b3e29be1
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 6, Pp 1479-1515 (2019)
Abstract A framework for analyzing and benchmarking climate model outputs is built upon δ‐MAPS, a recently developed complex network analysis method. The framework allows for the possibility of highlighting quantifiable topological differences acr
Externí odkaz:
https://doaj.org/article/2381668c6d754db5b8084545ac6604b0
Autor:
Fabrizio Falasca, Annalisa Bracco
Publikováno v:
Physical Review X, Vol 12, Iss 2, p 021054 (2022)
The threat of global warming and the demand for reliable climate predictions pose a formidable challenge because the climate system is multiscale, high-dimensional and nonlinear. Spatiotemporal recurrences of the system hint to the presence of a low-
Externí odkaz:
https://doaj.org/article/349c6fe070ad489390e8da02bd0e0409
Publikováno v:
Frontiers in Climate, Vol 3 (2021)
Global warming is posed to modify the modes of variability that control much of the climate predictability at seasonal to interannual scales. The quantification of changes in climate predictability over any given amount of time, however, remains chal
Externí odkaz:
https://doaj.org/article/45bad171a2c44efdbea274cdd1ff9fcc
Most climate models show a precipitation increase with warming that is smaller than the increase in moisture, which requires a weakening of the convective mass flux and a slowing of the overturning circulation. In this study we use global-storm resol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::91140e7e423a427fd0ade200cfcc8803
https://doi.org/10.5194/egusphere-egu23-14787
https://doi.org/10.5194/egusphere-egu23-14787
Climate sensitivity expresses how average global temperature responds to an increase in greenhouse gas concentration. It is a key metric to assess climate change, and to formulate policy decisions, but its estimation from the Earth System Models (ESM
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::670159ea45b1b1d1fed5b945b63fed6c
https://doi.org/10.5194/egusphere-egu22-7034
https://doi.org/10.5194/egusphere-egu22-7034
Autor:
Fabrizio Falasca, Annalisa Bracco
The threat of global warming and the demand for reliable climate predictions pose a formidable challenge being the climate system multiscale, high-dimensional and nonlinear. Spatiotemporal recurrences of the system hint to the presence of a low-dimen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b31df1843b9cc8c54fbb1070ca73aa5c
http://arxiv.org/abs/2110.03614
http://arxiv.org/abs/2110.03614
Publikováno v:
Climate Dynamics
Climate Dynamics, 2022, 59, pp.753-766. ⟨10.1007/s00382-022-06153-z⟩
Climate Dynamics, 2022, 59, pp.753-766. ⟨10.1007/s00382-022-06153-z⟩
International audience; Changes in climate mean state profoundly impact climate variability. Here, we quantify slow changes in the mean climate induced by the variations in the Earth’s orbit from mid- to late Holocene, and their feedback on the mai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8a3e83e32799653f93f9d6bc16dfa889
https://doi.org/10.21203/rs.3.rs-322105/v1
https://doi.org/10.21203/rs.3.rs-322105/v1