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Researchers report on recent drought in the eastern Hungarian plains

Alleviate the drought in the east Hungarian plains
A typical situation of summer 2022: There were clouds and medium-to-high levels of moisture in the atmosphere but no precipitation. The topsoil was completely dry, and the crops to be harvested in autumn had 100% yield loss in many places (26 July 2022). Credit: Gusztáv Jakab

Intensive agricultural cultivation and the resulting changes in soil structure cause low humidity in the near-surface air during heat waves in really dry years. As a result, summer cold fronts roar across the Great Hungarian Plain without the usual thunderstorms and precipitation.

Researchers at the Institute of Geography and Earth Sciences at Eötvös Loránd University explain this weather in a review of articles on topics ranging from the geodynamics to the soil science to the meteorology that made the summer of 2022 so severe in the eastern part of the country.

In 2022, the 7-week period starting in mid-June was disastrous for eastern Hungary. Almost no rain fell for weeks, and in the eastern part of the country, the economic loss of autumn crops was almost total. The , which had brought showers and rain to the western part of the country, dried up as they reached the Great Plain, passing through without precipitation and with only strong winds, making the drought situation even worse. Rumors had already started that some mysterious experiment influencing the weather had caused the almost complete drying out and destruction of the maize and sunflower crops in the lowlands that year.

Gábor Timár and Balázs Székely of the Department of Geophysics and Space Science, and Gusztáv Jakab of the Department of Environment and Landscape Geography show in their review article published in journal Land that this is not the case. Rather, the atmosphere was missing one of the most natural things: water.

Alleviate the drought in the east Hungarian plains
Severity of the drought occurred in Europe in the extremely hot 2022 summer heat wave. While the western and eastern parts of the continent were damaged by elongated anticyclonic periods, in the Great Hungarian Plain, the fronts occurred at almost normal rates, but they passed without precipitation. Map is made by European Commission GDO Analytical Report 2022. Credit: European Commission, Joint Research Centre, Toreti, A., Bavera, D., Acosta Navarro, J. et al., Drought in Europe—August 2022—GDO analytical report, Publications Office of the European Union, 2022, https://data.europa.eu/doi/10.2760/264241

Because of the unusually severe drought, one of the conditions for the formation of thunderstorms—a layer of humid air near the surface—was missing. As a result, the thunderstorms that provided the bulk of the summer rainfall were absent, exacerbating the situation and precluding the possibility of further storms over a period of several weeks.

The researchers conclude that the main reason for this is that the landscape water storage capacity has been significantly reduced due to intensive agricultural cultivation, following the water regulation measures.

In many places, large-scale cultivation and have created a secondary and almost impermeable layer in the soil, which prevents autumn-winter, and early summer precipitation from being stored in the deeper layers of the soil.

Alleviate the drought in the east Hungarian plains
An old, dried-up watercourse in autumn 2022 with some renewed vegetation after the September rains, showing the severity of the 2022 drought. Credit: Gusztáv Jakab

The upper 20-30 cm of the soil, however, dries out very quickly in the , and the chances of the remaining evaporation of moisture in the lower layers of the air and the formation of thunderstorms are then greatly reduced. The moisture in the higher air layers therefore does not reach the ground.

Their proposal is therefore to restore wetlands, meadows and pastures in a part of the lowland landscape, estimated to be at least one county in total, and even to divert excess water from elsewhere during the winter and snowmelt floods. Here, in addition to natural or accelerated restoration of , the re-establishment of vegetation that is highly evaporative during the summer period should be allowed or encouraged.

This can guarantee that rainfall can return in drought years, which will also bring rainwater to . These "evapotranspiration areas" could be created in the lowest areas of the lowlands, on the lowest-value agricultural land with a lower "golden crown" value, where the soil is not optimal for arable farming anyway.

More information: Gábor Timár et al, A Step from Vulnerability to Resilience: Restoring the Landscape Water-Storage Capacity of the Great Hungarian Plain—An Assessment and a Proposal, Land (2024). DOI: 10.3390/land13020146

Citation: Researchers report on recent drought in the eastern Hungarian plains (2024, January 31) retrieved 23 April 2024 from https://phys.org/news/2024-01-drought-eastern-hungarian-plains.html
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