Classification of Synoptic Conditions of Summer Floods in Polish Sudeten Mountains

Atmospheric processes leading to extreme floods in the Polish Sudeten Mountains were described in this study. A direct impact of heavy precipitation on extremely high runoff episodes was confirmed, and an essential role of synoptic conditions in triggering abundant rainfall was proved. Synoptic cond...

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Main Authors: Ewa Bednorz, Dariusz Wrzesiński, Arkadiusz M. Tomczyk, Dominika Jasik
Format: Article
Language:English
Published: MDPI AG 2019-07-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/11/7/1450
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spelling doaj-091cc9d6cd8a4b1381404ca6ed51fa172020-11-24T21:54:59ZengMDPI AGWater2073-44412019-07-01117145010.3390/w11071450w11071450Classification of Synoptic Conditions of Summer Floods in Polish Sudeten MountainsEwa Bednorz0Dariusz Wrzesiński1Arkadiusz M. Tomczyk2Dominika Jasik3Department of Climatology, Adam Mickiewicz University, 61-680 Poznań, PolandDepartment of Hydrology and Water Management, Adam Mickiewicz University, 61-680 Poznań, PolandDepartment of Climatology, Adam Mickiewicz University, 61-680 Poznań, PolandDepartment of Hydrology and Water Management, Adam Mickiewicz University, 61-680 Poznań, PolandAtmospheric processes leading to extreme floods in the Polish Sudeten Mountains were described in this study. A direct impact of heavy precipitation on extremely high runoff episodes was confirmed, and an essential role of synoptic conditions in triggering abundant rainfall was proved. Synoptic conditions preceding each flood event were taken into consideration and the evolution of the pressure field as well as the moisture transport was investigated using the anomaly-based method. Maps of anomalies, constructed for the days prior to floods, enabled recognizing an early formation of negative centers of sea level pressure and also allowed distinguishing areas of positive departures of precipitable water content over Europe. Five cyclonic circulation patterns of different origin, and various extent and intensity, responsible for heavy, flood-triggering precipitation in the Sudetes, were assigned. Most rain-bringing cyclones form over the Mediterranean Sea and some of them over the Atlantic Ocean. A meridional southern transport of moisture was identified in most of the analyzed cases of floods. Recognizing the specific meteorological mechanisms of precipitation enhancement, involving evolution of pressure patterns, change in atmospheric moisture and occurrence of precipitation may contribute to a better understanding of the atmospheric forcing of floods in mountain areas and to improve predicting thereof.https://www.mdpi.com/2073-4441/11/7/1450Sudeten Mountainsfloodextreme precipitationatmospheric circulationsynoptic conditionssea level pressurecyclone tracksprecipitable water
collection DOAJ
language English
format Article
sources DOAJ
author Ewa Bednorz
Dariusz Wrzesiński
Arkadiusz M. Tomczyk
Dominika Jasik
spellingShingle Ewa Bednorz
Dariusz Wrzesiński
Arkadiusz M. Tomczyk
Dominika Jasik
Classification of Synoptic Conditions of Summer Floods in Polish Sudeten Mountains
Water
Sudeten Mountains
flood
extreme precipitation
atmospheric circulation
synoptic conditions
sea level pressure
cyclone tracks
precipitable water
author_facet Ewa Bednorz
Dariusz Wrzesiński
Arkadiusz M. Tomczyk
Dominika Jasik
author_sort Ewa Bednorz
title Classification of Synoptic Conditions of Summer Floods in Polish Sudeten Mountains
title_short Classification of Synoptic Conditions of Summer Floods in Polish Sudeten Mountains
title_full Classification of Synoptic Conditions of Summer Floods in Polish Sudeten Mountains
title_fullStr Classification of Synoptic Conditions of Summer Floods in Polish Sudeten Mountains
title_full_unstemmed Classification of Synoptic Conditions of Summer Floods in Polish Sudeten Mountains
title_sort classification of synoptic conditions of summer floods in polish sudeten mountains
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2019-07-01
description Atmospheric processes leading to extreme floods in the Polish Sudeten Mountains were described in this study. A direct impact of heavy precipitation on extremely high runoff episodes was confirmed, and an essential role of synoptic conditions in triggering abundant rainfall was proved. Synoptic conditions preceding each flood event were taken into consideration and the evolution of the pressure field as well as the moisture transport was investigated using the anomaly-based method. Maps of anomalies, constructed for the days prior to floods, enabled recognizing an early formation of negative centers of sea level pressure and also allowed distinguishing areas of positive departures of precipitable water content over Europe. Five cyclonic circulation patterns of different origin, and various extent and intensity, responsible for heavy, flood-triggering precipitation in the Sudetes, were assigned. Most rain-bringing cyclones form over the Mediterranean Sea and some of them over the Atlantic Ocean. A meridional southern transport of moisture was identified in most of the analyzed cases of floods. Recognizing the specific meteorological mechanisms of precipitation enhancement, involving evolution of pressure patterns, change in atmospheric moisture and occurrence of precipitation may contribute to a better understanding of the atmospheric forcing of floods in mountain areas and to improve predicting thereof.
topic Sudeten Mountains
flood
extreme precipitation
atmospheric circulation
synoptic conditions
sea level pressure
cyclone tracks
precipitable water
url https://www.mdpi.com/2073-4441/11/7/1450
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AT dariuszwrzesinski classificationofsynopticconditionsofsummerfloodsinpolishsudetenmountains
AT arkadiuszmtomczyk classificationofsynopticconditionsofsummerfloodsinpolishsudetenmountains
AT dominikajasik classificationofsynopticconditionsofsummerfloodsinpolishsudetenmountains
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