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More precipitation in the North, less in the South, but what about Central Europe?

A summer thunderstorm sweeping over downtown Prague (photo: Ville Miettinen, www.flickr.com)
A summer thunderstorm sweeping over downtown Prague (photo: Ville Miettinen, www.flickr.com)

There is growing evidence that climate change impacts the hydrological cycle.

A recent study by researchers at the Institute of Atmospheric Physics CAS, Prague in the Czech Republic investigates a little-explored area of types of precipitation, modelling implications for soil, flooding and droughts across Europe’s regions.

Central Europe, transition zone

In plain words, rain falls in three distinct ways: by large-scale depressions, by local intensive showers, and when moist air is forced upwards over rising terrain, such as a mountain. In scientific terms these forms of precipitation are called stratiform, convective, and orographic, respectively. In Europe convective precipitation typically occurs in summer, for instance during thunderstorms. The precipitation is generally intense but of short duration. Stratiform precipitation occurs throughout the year.

The general future trend for Europe is an increase of mean precipitation in northern Europe, and a decrease in the south. The overall character of precipitation in Europe will also change. The contribution of convective precipitation to total yearly precipitation amounts will probably increase, especially in summer (and to a lesser degree in spring and autumn). Again in plain words: the number of intense showers will increase. The difference in future projections for northern and southern Europe is quite clear, but what about Central Europe, the transition zone between increasing and decreasing precipitation?

Future changes in precipitation in this transition zone were studied by looking at the Czech Republic. Projections of future precipitation patterns were made with regional climate models for an intermediate and high-end scenario of climate change. This was done for the period 2071 – 2100 against 1971 – 2000 (as a reference).

Both summer drying and more intense summer showers

According to these simulations, mean seasonal amounts of total precipitation tend to increase in all seasons except summer. The part of this precipitation related to large-scale depressions (stratiform) showed a similar pattern (highest increase in winter and spring, by about 15 per cent, slight decrease in summer by a few per cent) while local intense (convective) precipitation tends to increase throughout the year (especially in spring and summer, by about 10-20 per cent).

The projected summer drying in Central Europe is mainly associated with a decrease of stratiform precipitation; this decrease could be caused by a decrease in the frequency of frontal systems reaching Central Europe in summer (and autumn) due to a northward shift of the Atlantic-European storm track. Local intense (convective) precipitation, therefore, will contribute more to summer rainfall in Central Europe. Currently, convective precipitation In the Czech Republic contributes 50 per cent to summer rainfall, and 35 per cent and 15 per cent in spring and autumn, respectively.

Overall, it will rain harder in Europe in the future, both during heavy showers and during large-scale depressions. This increase will be more pronounced under the high-end end than the intermediate scenario of climate change: higher temperatures lead to more intense rainfall.

Consequences for agriculture and natural hazards

The steady rainfall of large-scale depressions (stratiform) is by its nature more important for agriculture; a decrease in combination with higher temperatures can lead to larger soil moisture deficits. More frequent and intense precipitation (convective), projected for the future climate, is not able to fully compensate the deficit of light and moderate precipitation because dry soil cannot absorb all water from intense precipitation events. Furthermore, extreme convective precipitation may cause flash floods and landslides, thus representing additional hazards and damages.

 


This article first appeared on ClimateChangePost, and  is a digest of a study by Rulfová et al., 2017. International Journal of Climatology 37: 2451–2465

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