In: Journal of Hydrology and Hydromechanics, vol. 68, no. 2
Péter Csáki - Kitti Gyimóthy - Péter Kalicz - Ján Szolgay - Katalin Zagyvai-Kiss - Zoltán Gribovszki
Detaily:
Rok, strany: 2020, 200 - 210
Jazyk: eng
Kľúčové slová:
Evapotranspiration; Runoff; Budyko-model; Water balance; Climate change.
URL originálneho zdroja: http://www.ih.sav.sk/jhh
O článku:
Providing information on the impacts of climate change on hydrological processes is becoming ever more
critical. Modelling and evaluating the expected changes of the water resources over different spatial and time scales can
be useful in several fields, e.g. agriculture, forestry and water management. Previously a Budyko-type spatially distributed
long-term climate-runoff model was developed for Hungary. This research includes the validation of the model using
historical precipitation and streamflow measurements for three nested sub-catchments of the Zala River Basin (Hungary),
an essential runoff contributing region to Lake Balaton (the largest shallow lake in Central Europe). The differences
between the calculated (from water balance) and the estimated (by the model) mean annual evapotranspiration varied
between 0.4% and 3.6% in the validation periods in the sub-catchments examined. Predictions of the main components
of the water balance (evapotranspiration and runoff) for the Zala Basin are also presented in this study using precipitation
and temperature results of 12 regional climate model simulations (A1B scenario) as input data. According to the projections,
the mean annual temperature will be higher from period to period (2011–2040, 2041–2070, 2071–2100), while the
change of the annual precipitation sum is not significant. The mean annual evapotranspiration rate is expected to increase
slightly during the 21st century, while for runoff a substantial decrease can be anticipated which may exceed 40% by
2071–2100 relative to the reference period (1981–2010). As a result of this predicted reduction, the runoff from the Zala
Basin may not be enough to balance the increased evaporation rate of Lake Balaton, transforming it into a closed lake
without outflow.
Ako citovať:
ISO 690:
Csáki, P., Gyimóthy, K., Kalicz, P., Szolgay, J., Zagyvai-Kiss, K., Gribovszki, Z. 2020. Multi-model climatic water balance prediction in the Zala River Basin
(Hungary) based on a modified Budyko framework. In Journal of Hydrology and Hydromechanics, vol. 68, no.2, pp. 200-210. 0042-790X (until 2019) . DOI: https://doi.org/10.2478/johh-2020-0016
APA:
Csáki, P., Gyimóthy, K., Kalicz, P., Szolgay, J., Zagyvai-Kiss, K., Gribovszki, Z. (2020). Multi-model climatic water balance prediction in the Zala River Basin
(Hungary) based on a modified Budyko framework. Journal of Hydrology and Hydromechanics, 68(2), 200-210. 0042-790X (until 2019) . DOI: https://doi.org/10.2478/johh-2020-0016
O vydaní:
Vydavateľ: VEDA, Publishing House of the Slovak Academy of Sciences, Bratislava, Slovakia
Publikované: 15. 6. 2020