Forestry Aridity Index in Vojvodina, North Serbia

In investigating aridity in Vojvodina (a region in the northern part of Serbia), the Forestry Aridity Index (FAI) was used. This index was chosen due to being one of the most suitable indices for the analysis of the interaction of climate and vegetative processes, especially in forestry. The spatial...

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Main Authors: Gavrilov Milivoj B., Lukić Tin, Janc Natalija, Basarin Biljana, Marković Slobodan B.
Format: Article
Language:English
Published: De Gruyter 2019-08-01
Series:Open Geosciences
Subjects:
nao
Online Access:https://doi.org/10.1515/geo-2019-0029
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spelling doaj-ded899f2d2fe49d981c99e34f1adf8f62021-09-05T20:50:50ZengDe GruyterOpen Geosciences2391-54472019-08-0111136737710.1515/geo-2019-0029geo-2019-0029Forestry Aridity Index in Vojvodina, North SerbiaGavrilov Milivoj B.0Lukić Tin1Janc Natalija2Basarin Biljana3Marković Slobodan B.4Chair of Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, 21000Novi Sad, SerbiaChair of Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, 21000Novi Sad, Serbia415 Old Trail Rd, Baltimore, Maryland 21212, United States of AmericaChair of Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, 21000Novi Sad, SerbiaChair of Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, 21000Novi Sad, SerbiaIn investigating aridity in Vojvodina (a region in the northern part of Serbia), the Forestry Aridity Index (FAI) was used. This index was chosen due to being one of the most suitable indices for the analysis of the interaction of climate and vegetative processes, especially in forestry. The spatial distribution of the FAI for annual and decennial periods, as well as its annual trend, is analysed. Satisfactory compatibility between the low (forest) and high (steppe) FAI values with the forest and steppe vegetation on the Vojvodina terrains was obtained. The calculated values of the FAI showed that there was no particular annual trend. These results correspond to the earlier calculated values of the De Martonne aridity index and the Pinna combinative index. Therefore, it can be concluded that there were no recent changes in aridity during the observed period. Results of the correlation indicate weak linearity between the FAI, and the North Atlantic Oscillation and El-Niño South Oscillation.https://doi.org/10.1515/geo-2019-0029aridity in vojvodinaaridity trendaridity climate classificationclimatological hazardnaoenso
collection DOAJ
language English
format Article
sources DOAJ
author Gavrilov Milivoj B.
Lukić Tin
Janc Natalija
Basarin Biljana
Marković Slobodan B.
spellingShingle Gavrilov Milivoj B.
Lukić Tin
Janc Natalija
Basarin Biljana
Marković Slobodan B.
Forestry Aridity Index in Vojvodina, North Serbia
Open Geosciences
aridity in vojvodina
aridity trend
aridity climate classification
climatological hazard
nao
enso
author_facet Gavrilov Milivoj B.
Lukić Tin
Janc Natalija
Basarin Biljana
Marković Slobodan B.
author_sort Gavrilov Milivoj B.
title Forestry Aridity Index in Vojvodina, North Serbia
title_short Forestry Aridity Index in Vojvodina, North Serbia
title_full Forestry Aridity Index in Vojvodina, North Serbia
title_fullStr Forestry Aridity Index in Vojvodina, North Serbia
title_full_unstemmed Forestry Aridity Index in Vojvodina, North Serbia
title_sort forestry aridity index in vojvodina, north serbia
publisher De Gruyter
series Open Geosciences
issn 2391-5447
publishDate 2019-08-01
description In investigating aridity in Vojvodina (a region in the northern part of Serbia), the Forestry Aridity Index (FAI) was used. This index was chosen due to being one of the most suitable indices for the analysis of the interaction of climate and vegetative processes, especially in forestry. The spatial distribution of the FAI for annual and decennial periods, as well as its annual trend, is analysed. Satisfactory compatibility between the low (forest) and high (steppe) FAI values with the forest and steppe vegetation on the Vojvodina terrains was obtained. The calculated values of the FAI showed that there was no particular annual trend. These results correspond to the earlier calculated values of the De Martonne aridity index and the Pinna combinative index. Therefore, it can be concluded that there were no recent changes in aridity during the observed period. Results of the correlation indicate weak linearity between the FAI, and the North Atlantic Oscillation and El-Niño South Oscillation.
topic aridity in vojvodina
aridity trend
aridity climate classification
climatological hazard
nao
enso
url https://doi.org/10.1515/geo-2019-0029
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