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You can start or join in a discussion here. Visit emeraldpublishing. Abstract Purpose The purpose of this paper is to advance the dialogue between the disaster risk reduction DRR and adaptation community by investigating their differences, similarities and potential synergies. Please note you might not have access to this content.
Figures used Landslide susceptibility for weather induced landslides: ICG left and b JRC models right A distinct difference can be observed between the two models, where JRC model in general defines larger areas being exposed to landslides than the ICG model.
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This already shows that classification of landslide zonation maps is subjective and depends on the choice of the experts. The classified hazard map of JRC is definitely more conservative although it does incorporate hotspots of known hazard such as north-west Scotland, which the ICG model does not. Red circles show possible hotspots. White colour represent region without landslide hazard. River floods on rivers Sava and Bosnia in Bosnia and Herzegovina Left figure shows normal situation in the region and right figure shows extend of river flooding on 22 May Baseline period is — Expected variations in abundance or activity of four landslide types, driven by the projected climate change Expected variations in abundance or activity of four landslide types, driven by the projected climate change.
Recorded track of the medicane occurring in January Medicane track from a high-resolution simulation of January Total observed precipitation for the events of 30 May-2 June Map shows cumulative precipitation amount over the period between 30 May and 2 June Locations of European tide gauges with length of records Colours represent different lengths of the datasets, ranging from less than 30 years white to over years black.
Observed trends in maximum annual five-day consecutive precipitation in winter and summer Grid boxes outlined in solid black contain at least three stations and so are likely to be more representative of the grid box.
Change in the frequency of flooding events under projected sea level rise This map shows the estimated multiplication factor, by which the frequency of flooding events of a given height changes between and due to projected regional sea relative level rise under the RCP4. Values larger than 1 indicate an increase in flooding frequency.
Observed trends in frequency and severity of meteorological droughts Trends in frequency upper and severity lower of meteorological droughts between and Projected change in the frequency of meteorological droughts The maps show changes in the frequency of meteorological droughts for two future periods , left and , right and for two emissions scenarios RCP4.
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Drought frequency is defined as the number of months in a 30 year period with the Standardised Precipitation Index accumulated over a 6 month period SPI-6 having a value below Deaths related to flooding in Europe This map shows the number of deaths related to flooding per million inhabitants cumulative over the period —, with respect to population. Projected change in summer soil moisture Changes are presented as mean multi-model change between and using 12 Regional Climate Models RCMs ; with red indicating drier and blue indicating wetter conditions.
Projected changes in extreme wind speed based on GCM and RCM ensembles Ensemble mean of changes in extreme wind speed defined as the 98th percentile of daily maximum wind speed for A1B — relative to — Left: based on 9 GCMs.
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Right: based on 11 RCMs. Preparing Europe for climate change: coordination is key to reduce risks posed by extreme weather Building stronger links between climate change adaptation and disaster risk reduction experts is more important than ever in wake of recent devastating and extreme weather events across Europe and elsewhere. Closer cooperation, including better policy alignment, will be crucial to reduce the impacts of weather- and climate-related hazards like floods, heatwaves, forest fires, or storm surges.
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Increasing coherence in actions and using innovative methods can improve the handling of these events, according to a report by the European Environment Agency EEA published today. Wind storms Storm location, frequency and intensity have shown considerable decadal variability across Europe over the past century, such that no significant long-term trends are apparent.
Recent studies on changes in winter storm tracks generally project an extension eastwards of the North Atlantic storm track towards central Europe and the British Isles. Climate change simulations show diverging projections on changes in the number of winter storms across Europe.
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However, most studies agree that the risk of severe winter storms, and possibly of severe autumn storms, will increase for the North Atlantic and northern, north-western and central Europe over the 21st century. Meteorological and hydrological droughts Drought has been a recurrent feature of the European climate. The severity and frequency of meteorological and hydrological droughts have increased in parts of Europe, in particular in south-western and central Europe.
Available studies project large increases in the frequency, duration and severity of meteorological and hydrological droughts in most of Europe over the 21st century, except for northern European regions. The greatest increase in drought conditions is projected for southern Europe, where it would increase competition between different water users, such as agriculture, industry, tourism and households. River floods Almost 1 floods have been reported for Europe since , of which more than half have occurred since The number of very severe flood events in Europe increased over the period —, but with large interannual variability.
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