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Volume XX |
Climatology

Ecoclimatic characteristics of the south-western slope of the Pirin Mountains (Bulgaria)

1,, 1, 2

Abstract: The paper characterizes thermal and humidity conditions within one of the insufficiently investigated parts of Bulgaria from the climate point of view, namely the south-western slope of the Pirin Mountains. The initial data for the study (monthly temperatures and precipitation amounts) were obtained from our own meteorological monitoring station for the period 2013-2021, organized by the Department of Climatology, Hydrology and Geomorphology, Sofia University, Bulgaria. By the calculation of Mayr tetratherm (MT), monthly De Martonne aridity index (Im) and Compensated Summer Ombrothermic index (CSOi) the predominance of humid conditions in the studied area is established. There is a large inter-annual variability of the De Martonne aridity index and the Compensated Summer Ombrothermic index, which are more influenced by precipitation than air temperature in the middle part of the mountains. On the other hand, in combination with low precipitation amounts, high temperatures in recent years have contributed to the manifestation of arid features of the climate. The results of the study supplement the insufficient information about the bioclimatic characteristics of the Pirin Mountains and clarify the peculiarities of the climate in these mountains, which have two clearly distinguishable macroslopes with west-southwest and east-northeast exposure.

Keywords: , , ,
Full article 10.5775/fg.2021.046.dDates:
Received: 21-01-2021 Accepted: 01-07-2021 Printed: 30-12-2021 Online: 14-02-2022
Affiliations:
  • 1 Faculty of Geology and Geography, Sofia University “St. Climent Ohridski”, Tsar Osvoboditel Blvd., 15, Sofia 1504, Bulgaria
  • 2 Geography Department, University of Craiova, str. Al. I. Cuza, no. 13, 200585
Corresponding author:
  • nina@gea.uni-sofia.bg
Citation:
APA 6 | Harvard 2008 | Turabian 6 | MLA 7
RIS | BibTeX
Acknowledgements: This work has been carried out in the framework of the “Environment under climate change in the Pirin Mountain“, contract N ДН 14/6, 13.12.2017, financed by National Scientific Fund, Ministry of Education and Science – Bulgaria.
Copyright: © 2022 The Author(s). Published by Forum geografic.
Provided under the Creative Commons Attribution-NonCommercial-NoDerivatives License.
Open Access article.
Volume XVI |
Climatology

Analysis of the Mean of Daily Maximum Temperature within the Romanian Plain (1961-2015)

1,

Abstract: The present study aims at rendering the characteristics of the means of the daily maximum temperature at monthly, seasonal and annual level within the Romanian Plain, as well as their trends. The time series cover a 55-year period (1961-2015) and data come from 8 meteorological stations. In order to assess the distribution of the data, there were calculated two coefficients (Skewness – S and Kurtosis – K) and also applied the Kolmogorov-Smirnov test for normal distribution. The positive S values and negative K values indicate that the distribution is not symmetrical but, taking into account that the values are quite close to 0, we may assume, it is not far from normal. The KS test also indicates a normal distribution. Homogeneity of the annual temperatures was tested by means of Pettitt test, Standard Normal Homogeneity Test (SNTH) and t test, which emphasized that the change point was registered before 2000. At three stations (D.T. Severin, Bechet, Buzău) all three applied tests indicated the same year 1988, respectively 1989 as break point, while at the other stations, it is the same year according to SNHT and T test, and a different one based on MWP. Based on Mann-Kendall test and Sen’s slope estimation, there were emphasized temperature trends and their statistical significance. The highest temperature increase and upward trend was registered for mean annual and mean summer values (0.001 level of significance within the entire region). However, except for autumn, which is generally characterized by statistically insignificant negative trends, all the other seasons display significant upward trends. At monthly level, only the summer months registered upwards trends within the entire plain (level of significance oscillating between 0.05 and 0.001), while in autumn months there were not registered any statistically significant trends.

Keywords: , , , , ,
Full article 10.5775/fg.2017.040.iDates:
Received: 20-01-2017 Accepted: 25-05-2017 Printed: 30-06-2017 Online: 13-02-2018
Affiliations:
  • 1 Faculty of Sciences, Department of Geography, University of Craiova, 13 A. I. Cuza street, Craiova, Romania
Corresponding author:
  • vladut_alina2005@yahoo.com
Citation:
APA 6 | Harvard 2008 | Turabian 6 | MLA 7
RIS | BibTeX
Copyright: © 2018 The Author(s). Published by Forum geografic.
Provided under the Creative Commons Attribution-NonCommercial-NoDerivatives License.
Open Access article.
Volume XIII |
Climatology

Analysis of precipitation characteristics and trends for the Getic Piedmont and Subcarpathians, Oltenia region, Romania

1,, 2

Abstract: Changes in precipitation characteristics of the hilly area of Oltenia, covering the western parts of the Getic Piedmont and SubCarpathians, were analysed, based on monthly rainfall data, for the timeframe 1961 to 2010. The precipitation trend analysis for the period 1961-2010 shows different results–increasing precipitation in winter half part of the year for most of the Subcarpathian area and a rainfall decrease in summer half of the year for the entire region. The piedmont part of the study area, with dominant agricultural land use, shows the highest spring precipitation decrease, whereas in the Subcarpathian area, summer and autumn precipitation increase is more pronounced. The positive trends are spatially the most homogenous in August, September and October, while the most uniform negative trends were recorded in February, May and November. At annual level, the most significant decrease corresponds to the piedmont, while the rest of the region displays an insignificant positive trend. The SPA emphasized that normal years (deviations oscillating between -1.00 and +1.00) predominate; however, in the eastern part of the region there are lower percentages compared to the western part (70-74% compared to 64-66%). At the same time, in the east, the share of dry weather is double compared to the western part, where rainy weather predominates.

Keywords: , , , ,
Full article 10.5775/fg.2067-4635.2014.036.dDates:
Received: 15-09-2014 Accepted: 01-12-2014 Printed: 30-12-2014 Online: 22-03-2015
Affiliations:
  • 1 University of Craiova, Department of Geography, Romania
  • 2 University of Bucharest, Faculty of Geography, Romania
Corresponding author:
  • vladut_alina2005@yahoo.com
Citation:
APA 6 | Harvard 2008 | Turabian 6 | MLA 7
RIS | BibTeX
Copyright: © 2015 The Author(s). Published by Forum geografic.
Provided under the Creative Commons Attribution-NonCommercial-NoDerivatives License.
Open Access article.
Volume IX |
Climatology

Ecoclimatic Indexes within the Oltenia Plain

1,

Abstract: The Oltenia Plain represents an important agricultural region of Romania, which displays vast surfaces that can be properly cultivated if one takes into account the climatic restrictions that generates a series of dysfunctions. In order to underline the problems related to the aridization tendency within the region, as well as to determine the most adequate plants, there were calculated many indexes used in different agroclimatic and biogeographical studies. Thus, according to the processed data, the Oltenia Plain generally belongs to the steppe and forest steppe domain and, with regard to the cultivable plants, there are recommended the thermophilous and xerothermophilous ones, which can get good productions even in the pluvial-thermal conditions characteristic to the region. The thermal regime imposes itself through a slight increasing tendency because of the extremely high values registered in summer, while the pluviometric regime registers obvious fluctuations and a decreasing tendency. Consequently, the issue related to the aridization of the southern part of the Oltenia Plain is confirmed, an issue that is presently stressed by other factors, such as massive deforestation, destruction of the irrigation systems etc., which led to the reactivation of certain areas covered by sands. However, the partial results of the study do not sustain the idea of desertification in the area.

Keywords: , , , , ,
Full article Dates:
Printed: 01-11-2010 Online: 21-11-2010
Affiliations:
  • 1 Faculty of Social Sciences, Department of Geography, University of Craiova, 13 Al. I. Cuza Street, Craiova, Romania
Corresponding author:
  • vladut_alina2005@yahoo.com
Citation:
APA 6 | Harvard 2008 | Turabian 6 | MLA 7
RIS | BibTeX
Acknowledgements: This work was supported by the strategic grant POSDRU/89/1.5/S/61968, Project ID61968 (2009), co-financed by the European Social Fund within the Sectorial Operational Program Human Resources Development 2007 – 2013.
Copyright: © 2010 The Author(s). Published by Forum geografic.
Provided under the Creative Commons Attribution-NonCommercial-NoDerivatives License.
Open Access article.

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