The spatial and temporal variability of hydrological drought in the Polish Carpathians

Title:

The spatial and temporal variability of hydrological drought in the Polish Carpathians

Creator:

Baran-Gurgul, Katarzyna

Identifier:

https://cdk.lib.cas.cz/client/handle/uuid:411379e7-87e9-40b4-b35d-5a087f79a79b
uuid:411379e7-87e9-40b4-b35d-5a087f79a79b
doi:10.2478/johh-2022-0007

Subject:

hydrological drought, long-term variability, seasonal variability, vistula, the Polish Carpathian, and drought hazard

Type:

model:article and TEXT

Format:

počítač and online zdroj

Description:

The aim of the study was to evaluate the climate and geographic factors controlling the hydrological drought of the rivers located in the Upper Vistula catchment in the Polish Carpathians. Drought was identified based on the daily flow (based on water stage measered once a day at 6 UTC) series dating from between 1975 and 2019 at 49 gauging cross-sections. Four physico-geographical regions were identified in the Polish Carpathians and spatial variabilities of the basic drought characteristics were developed within these regions. Such spatial distributions were treated as maps indicating drought hazard areas in the region. In addition, an analysis was undertaken to study the seasonality of the start and end times of the drought (all in the multi-annual period), the longest duration of droughts, the droughts of the highest volume in multi-annual period, as well as the number of drought days. Multi-annual variability of the number of drought days was also analysed. The results suggest that droughts in the Polish Carpathians are events characteristic of summer and autumn, whereas in the Tatra Mountains and the Podhale region - of autumn and winter. The greatest hazard of a prolonged and highvolume drought occurs in the Podhale region and the Tatra Mountains, while the lowest hazard is observed in the Bieszczady Mountains and the eastern part of the studied area.

Language:

Slovak

Rights:

http://creativecommons.org/licenses/by-nc-sa/4.0/
policy:public

Coverage:

156-169

Source:

Journal of hydrology and hydromechanics | 2022 Volume:70 | Number:2

Harvested from:

CDK

Metadata only:

false