Heavy precipitation is a major hazard over Europe. It is well established that climate model projections indicate a tendency towards more extreme daily rainfall events. It is still uncertain, however, how this changing intensity translates at the sub-daily time scales. The main goal of the present study is to examine possible differences in projected changes in intense precipitation events over Europe at the daily and sub-daily (3-hourly) time scales using a state-of-the-science climate model. The focus will be on one Representative Concentration Pathway (RCP 8.5), considered as illustrative of a high rate of increase in greenhouse gas concentrations over this century. There are statistically significant differences in intense precipitation...
[1] Regional multi-model ensembles are used to both increase the spatial resolution of the global si...
Extreme precipitation occurring on consecutive days may substantially increase the risk of related i...
Climate model outputs can be used to assess the expected behaviour of extreme precipitations in the ...
Abstract Heavy precipitation is a major hazard over Europe. It is well established th...
Two regional climate model experiments for northern and central Europe are studied focussing on gree...
While daily extreme precipitation intensities increase with global warming on average at approximate...
At regional to local scales internal variability is expected to be a dominant source of uncertainty ...
The intensity and distribution of daily precipitation is predicted to change under scenarios of incr...
Extreme precipitation and flood are among the major climate-related disasters which cause thousands ...
An extreme-value analysis of projected changes in heavy precipitation is carried out for an ensemble...
We investigate the space-time structure of extreme precipitation in Europe over the last century, us...
The effect of climate change on potentially infrastructure-damaging heavy precipitation events in Eu...
Precipitation over western Europe (WE) is projected to increase (decrease) roughly northward (equato...
Historical observations show a significant change of globe temperature distribution as a consequenc...
Two Regional Climate Model (RCM) projections of changes in extreme precipitation over Europe are ass...
[1] Regional multi-model ensembles are used to both increase the spatial resolution of the global si...
Extreme precipitation occurring on consecutive days may substantially increase the risk of related i...
Climate model outputs can be used to assess the expected behaviour of extreme precipitations in the ...
Abstract Heavy precipitation is a major hazard over Europe. It is well established th...
Two regional climate model experiments for northern and central Europe are studied focussing on gree...
While daily extreme precipitation intensities increase with global warming on average at approximate...
At regional to local scales internal variability is expected to be a dominant source of uncertainty ...
The intensity and distribution of daily precipitation is predicted to change under scenarios of incr...
Extreme precipitation and flood are among the major climate-related disasters which cause thousands ...
An extreme-value analysis of projected changes in heavy precipitation is carried out for an ensemble...
We investigate the space-time structure of extreme precipitation in Europe over the last century, us...
The effect of climate change on potentially infrastructure-damaging heavy precipitation events in Eu...
Precipitation over western Europe (WE) is projected to increase (decrease) roughly northward (equato...
Historical observations show a significant change of globe temperature distribution as a consequenc...
Two Regional Climate Model (RCM) projections of changes in extreme precipitation over Europe are ass...
[1] Regional multi-model ensembles are used to both increase the spatial resolution of the global si...
Extreme precipitation occurring on consecutive days may substantially increase the risk of related i...
Climate model outputs can be used to assess the expected behaviour of extreme precipitations in the ...