Aridity in the Central and Southern Pannonian Basin

For the investigation of geographical, monthly, seasonal, and annual distributions of aridity and its annual trend in the region of the Central and Southern Pannonian Basin (CSPB), which includes the territories of Hungary and Vojvodina (Northern Serbia), the De Martonne Aridity Index (DMAI) was use...

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Main Authors: Milivoj B. Gavrilov, Milica G. Radaković, György Sipos, Gábor Mezősi, Gavrilo Gavrilov, Tin Lukić, Biljana Basarin, Balázs Benyhe, Károly Fiala, Péter Kozák, Zoran M. Perić, Dragan Govedarica, Yang Song, Slobodan B. Marković
Format: Article
Language:English
Published: MDPI AG 2020-11-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/11/12/1269
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spelling doaj-43d8d1274870458b96fb6d9d2156d44e2020-11-27T07:55:59ZengMDPI AGAtmosphere2073-44332020-11-01111269126910.3390/atmos11121269Aridity in the Central and Southern Pannonian BasinMilivoj B. Gavrilov0Milica G. Radaković1György Sipos2Gábor Mezősi3Gavrilo Gavrilov4Tin Lukić5Biljana Basarin6Balázs Benyhe7Károly Fiala8Péter Kozák9Zoran M. Perić10Dragan Govedarica11Yang Song12Slobodan B. Marković13Chair for Physical Geography, Faculty of Science, University of Novi Sad, Trg Dositeja Obradovića 3, 21000 Novi Sad, SerbiaChair for Physical Geography, Faculty of Science, University of Novi Sad, Trg Dositeja Obradovića 3, 21000 Novi Sad, SerbiaDepartment of Physical Geography and Geoinformatics, University of Szeged, Egyetem u. 2-6, 672 Szeged, HungaryDepartment of Physical Geography and Geoinformatics, University of Szeged, Egyetem u. 2-6, 672 Szeged, HungaryChair for Physical Geography, Faculty of Science, University of Novi Sad, Trg Dositeja Obradovića 3, 21000 Novi Sad, SerbiaChair for Physical Geography, Faculty of Science, University of Novi Sad, Trg Dositeja Obradovića 3, 21000 Novi Sad, SerbiaChair for Physical Geography, Faculty of Science, University of Novi Sad, Trg Dositeja Obradovića 3, 21000 Novi Sad, SerbiaLower Tisza District Water Directorate, Stefánia 4, H-6720 Szeged, HungaryLower Tisza District Water Directorate, Stefánia 4, H-6720 Szeged, HungaryLower Tisza District Water Directorate, Stefánia 4, H-6720 Szeged, HungaryResearch Group for Terrestrial Paleoclimates, Max Planck Institute for Chemistry, Hahn Meitner Weg 1, 55128 Mainz, GermanyDepartment of Oil and Petrochemical Engineering, Faculty of Technology, University of Novi Sad, Bulevar Cara Lazara 1, 21000 Novi Sad, SerbiaBeijing Research Center of Urban System Engineering, Xizhimen South Street, Xicheng District, Beijing 100035, ChinaChair for Physical Geography, Faculty of Science, University of Novi Sad, Trg Dositeja Obradovića 3, 21000 Novi Sad, SerbiaFor the investigation of geographical, monthly, seasonal, and annual distributions of aridity and its annual trend in the region of the Central and Southern Pannonian Basin (CSPB), which includes the territories of Hungary and Vojvodina (Northern Serbia), the De Martonne Aridity Index (DMAI) was used. The DMAI was originally calculated from a total of 78 meteorological stations with the maximum available time series of climatological data in three cases: 1931–2017 for Hungary; 1949–2017 for Vojvodina; and 1949–2017 for Hungary and Vojvodina jointly. The Palmer Drought Severity Index (PDSI) was used to control the DMAI results. Temperature and precipitation trends were also investigated to understand their effects on the aridity trend. Three aridity types are distinguished on the annual level, five on the seasonal level, and four on the monthly level. The annual aridity had no trends in all three periods. It seems that aridity can be considered a more stable climate indicator of climate change than the temperature, at least in the CSPB.https://www.mdpi.com/2073-4433/11/12/1269De Martonne Aridity IndexPalmer Drought Severity IndexHungaryVojvodinaSerbia
collection DOAJ
language English
format Article
sources DOAJ
author Milivoj B. Gavrilov
Milica G. Radaković
György Sipos
Gábor Mezősi
Gavrilo Gavrilov
Tin Lukić
Biljana Basarin
Balázs Benyhe
Károly Fiala
Péter Kozák
Zoran M. Perić
Dragan Govedarica
Yang Song
Slobodan B. Marković
spellingShingle Milivoj B. Gavrilov
Milica G. Radaković
György Sipos
Gábor Mezősi
Gavrilo Gavrilov
Tin Lukić
Biljana Basarin
Balázs Benyhe
Károly Fiala
Péter Kozák
Zoran M. Perić
Dragan Govedarica
Yang Song
Slobodan B. Marković
Aridity in the Central and Southern Pannonian Basin
Atmosphere
De Martonne Aridity Index
Palmer Drought Severity Index
Hungary
Vojvodina
Serbia
author_facet Milivoj B. Gavrilov
Milica G. Radaković
György Sipos
Gábor Mezősi
Gavrilo Gavrilov
Tin Lukić
Biljana Basarin
Balázs Benyhe
Károly Fiala
Péter Kozák
Zoran M. Perić
Dragan Govedarica
Yang Song
Slobodan B. Marković
author_sort Milivoj B. Gavrilov
title Aridity in the Central and Southern Pannonian Basin
title_short Aridity in the Central and Southern Pannonian Basin
title_full Aridity in the Central and Southern Pannonian Basin
title_fullStr Aridity in the Central and Southern Pannonian Basin
title_full_unstemmed Aridity in the Central and Southern Pannonian Basin
title_sort aridity in the central and southern pannonian basin
publisher MDPI AG
series Atmosphere
issn 2073-4433
publishDate 2020-11-01
description For the investigation of geographical, monthly, seasonal, and annual distributions of aridity and its annual trend in the region of the Central and Southern Pannonian Basin (CSPB), which includes the territories of Hungary and Vojvodina (Northern Serbia), the De Martonne Aridity Index (DMAI) was used. The DMAI was originally calculated from a total of 78 meteorological stations with the maximum available time series of climatological data in three cases: 1931–2017 for Hungary; 1949–2017 for Vojvodina; and 1949–2017 for Hungary and Vojvodina jointly. The Palmer Drought Severity Index (PDSI) was used to control the DMAI results. Temperature and precipitation trends were also investigated to understand their effects on the aridity trend. Three aridity types are distinguished on the annual level, five on the seasonal level, and four on the monthly level. The annual aridity had no trends in all three periods. It seems that aridity can be considered a more stable climate indicator of climate change than the temperature, at least in the CSPB.
topic De Martonne Aridity Index
Palmer Drought Severity Index
Hungary
Vojvodina
Serbia
url https://www.mdpi.com/2073-4433/11/12/1269
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