Abstract

The potential impacts of climate change on the Great Hungarian Plain based on two regional climate models, REMO and ALADIN, were analyzed using indicators for environmental hazards. As the climate parameters (temperature, precipitation, and wind) will change in the two investigated periods (2021–2050 and 2071–2100), their influences on drought, wind erosion, and inland excess water hazards are modeled by simple predictive models. Drought hazards on arable lands will increasingly affect the productivity of agriculture compared to the reference period (1961–1990). The models predict an increase between 12.3 % (REMO) and 20 % (ALADIN) in the first period, and between 35.6 % (REMO) and 45.2 % (ALADIN) in the second period. The increase of wind erosion hazards is not as obvious (+15 % for the first period in the REMO model). Inland excess water hazards are expected to be slightly reduced (−4 to 0 %) by both model predictions in the two periods without showing a clear tendency on reduction. All three indicators together give a first regional picture of potential hazards of climate change. The predictive model and data combinations of the regional climate change models and the hazard assessment models provide insights into regional and subregional impacts of climate change and will be useful in planning and land management activities.

Highlights

  • Climate change strongly impacts the Carpathian Basin

  • The potential impacts of climate change on the Great Hungarian Plain based on two regional climate models, REMO and ALADIN, were analyzed using indicators for environmental hazards

  • The models predict an increase between 12.3 % (REMO) and 20 % (ALADIN) in the first period, and between 35.6 % (REMO) and 45.2 % (ALADIN) in the second period

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Summary

Introduction

Climate change strongly impacts the Carpathian Basin. Many natural hazards—for example drought (Blanka et al 2013), inland excess water (Rakonczai et al 2011), and wind erosion (Mez}osi, Blanka, et al 2013)—cause social, economic, and environmental problems. In the Carpathian Basin drought is one of the most severe environmental hazards (Bakonyi 2010; Palfai and Herceg 2011; Bihari 2012; Gosic and Trajkovic 2013; WMO 2013) that occurs every 3–5 years. Excess water affects mostly lowland areas, causing damages to agriculture, soil structure, and inundated urban areas (Likens 2009; Rakonczai et al 2011; van Leeuwen 2012; Julian et al 2013; Shi et al 2013). The incidence of wind erosion and the rate of damage are determined by several environmental factors, such as soil texture, lithology, climate, vegetation, and human land use (agricultural techniques). According to Loczy et al (2012) 26.5 % of the Carpathian Basin is affected strongly or moderately by wind erosion

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