TY  - JOUR
AU  - Belij, Srđan
AU  - Ducić, Vladan
AU  - Radovanović, Milan
AU  - Milovanović, Boško
PY  - 2007
UR  - https://gery.gef.bg.ac.rs/handle/123456789/236
AB  - In the distinctive mountsinod area of the Mt. Stara Planina, mesoclimate zoning was performed with certain generalization level in climate zone separation. Furthermore, due to lack of available data base, the aforementioned altitude zoning must not be considered strictly within presented altitude volumes. Outstanding terrain dissection, different level of vegetation covering and enhanced impact of secondary, i.e. tertiary climate modificators in certain parts of the Mt. Stara Planina, may create microclimate or topoclimate conditions which essentially differ from the present quantitative values of climatic elements in sub-mountainous, mountainous or high-mountainous areas. This fact is particularly apparent if we have in mind that the climate is one of the essential factors for creation of the relief periglacial forms; their inventory and systematization as well as complex population analysis could indirectly offer data on climate conditions in huge areas which are not covered by meteorological monitoring. However, quantification of climate elements in this region is a methodological problem which requires qualitatively different access and a different data base. Substantial lack of appropriate climatologic data has been substituted by particularly detailed study on vegetation of this mountain area with data on climatogene communities and communities for which there are good climatic indicators (particularly communities with detailed measurements in other mountainous areas); as far as the areas above the upper forest limit are concerned, detailed research has been performed regarding the recent periglacial processes and their relief forms as direct climatic-geomorphologic indicators of the high mountains (periglacial) climate. We believe that this attempt of climate zoning of the Mt. Stara Planina, as distinctive mountainous area, by comparison of detailed vegetation and periglacial-geomorphologic research as well as research of the upper forest limit, is the only proper way of performing this task due to lack of instrumental measurements at high altitudes. .
AB  - U radu je učinjen pokušaj da se kompleksnim istraživanjima različitih oblasti (klimatologija, botanika, geomorfologija) i međusobnom komparacijom dobijenih rezultata nadoknadi nedostatak instrumentalnih meteoroloških merenja na većim visinama. Dobijena klimatska rejonizacija koja se u uslovima Stare planine svodi na visinsku pojasnost jasno pokazuje direktnu uslovljenost klime, savremenog stanja u rasporedu vegetacije i savremenih periglacijalnih geomorfoloških procesa iznad gornje šumske granice. .
PB  - Zavod za zaštitu prirode, Beograd
T2  - Zaštita prirode
T1  - Climate zoning and position of the upper forest limit on the Mt. Stara Planina
T1  - Klimatsko rejoniranje i položaj gornje šumske granice na Staroj Planini
VL  - 57
IS  - 1-2
SP  - 21
EP  - 34
UR  - https://hdl.handle.net/21.15107/rcub_gery_236
ER  - 

@article{
author = "Belij, Srđan and Ducić, Vladan and Radovanović, Milan and Milovanović, Boško",
year = "2007",
abstract = "In the distinctive mountsinod area of the Mt. Stara Planina, mesoclimate zoning was performed with certain generalization level in climate zone separation. Furthermore, due to lack of available data base, the aforementioned altitude zoning must not be considered strictly within presented altitude volumes. Outstanding terrain dissection, different level of vegetation covering and enhanced impact of secondary, i.e. tertiary climate modificators in certain parts of the Mt. Stara Planina, may create microclimate or topoclimate conditions which essentially differ from the present quantitative values of climatic elements in sub-mountainous, mountainous or high-mountainous areas. This fact is particularly apparent if we have in mind that the climate is one of the essential factors for creation of the relief periglacial forms; their inventory and systematization as well as complex population analysis could indirectly offer data on climate conditions in huge areas which are not covered by meteorological monitoring. However, quantification of climate elements in this region is a methodological problem which requires qualitatively different access and a different data base. Substantial lack of appropriate climatologic data has been substituted by particularly detailed study on vegetation of this mountain area with data on climatogene communities and communities for which there are good climatic indicators (particularly communities with detailed measurements in other mountainous areas); as far as the areas above the upper forest limit are concerned, detailed research has been performed regarding the recent periglacial processes and their relief forms as direct climatic-geomorphologic indicators of the high mountains (periglacial) climate. We believe that this attempt of climate zoning of the Mt. Stara Planina, as distinctive mountainous area, by comparison of detailed vegetation and periglacial-geomorphologic research as well as research of the upper forest limit, is the only proper way of performing this task due to lack of instrumental measurements at high altitudes. ., U radu je učinjen pokušaj da se kompleksnim istraživanjima različitih oblasti (klimatologija, botanika, geomorfologija) i međusobnom komparacijom dobijenih rezultata nadoknadi nedostatak instrumentalnih meteoroloških merenja na većim visinama. Dobijena klimatska rejonizacija koja se u uslovima Stare planine svodi na visinsku pojasnost jasno pokazuje direktnu uslovljenost klime, savremenog stanja u rasporedu vegetacije i savremenih periglacijalnih geomorfoloških procesa iznad gornje šumske granice. .",
publisher = "Zavod za zaštitu prirode, Beograd",
journal = "Zaštita prirode",
title = "Climate zoning and position of the upper forest limit on the Mt. Stara Planina, Klimatsko rejoniranje i položaj gornje šumske granice na Staroj Planini",
volume = "57",
number = "1-2",
pages = "21-34",
url = "https://hdl.handle.net/21.15107/rcub_gery_236"
}

Belij, S., Ducić, V., Radovanović, M.,& Milovanović, B.. (2007). Climate zoning and position of the upper forest limit on the Mt. Stara Planina. in Zaštita prirode
Zavod za zaštitu prirode, Beograd., 57(1-2), 21-34.
https://hdl.handle.net/21.15107/rcub_gery_236

Belij S, Ducić V, Radovanović M, Milovanović B. Climate zoning and position of the upper forest limit on the Mt. Stara Planina. in Zaštita prirode. 2007;57(1-2):21-34.
https://hdl.handle.net/21.15107/rcub_gery_236 .

Belij, Srđan, Ducić, Vladan, Radovanović, Milan, Milovanović, Boško, "Climate zoning and position of the upper forest limit on the Mt. Stara Planina" in Zaštita prirode, 57, no. 1-2 (2007):21-34,
https://hdl.handle.net/21.15107/rcub_gery_236 .

TY  - JOUR
AU  - Belij, Srđan
AU  - Ducić, Vladan
AU  - Milovanović, Boško
AU  - Luković, Jelena
AU  - Mišćević, Igor
PY  - 2004
UR  - https://gery.gef.bg.ac.rs/handle/123456789/98
AB  - When new localities with active periglacial processes are discovered, that leads to detailed study of these areas that is multidisciplinary in character. Especially interesting are results of climatologic research where climatic or frost potentials were used to determine the climatic conditions necessary for appearance of frost grass mounds. This is not strictly connected only with conditions on Pešter, but has a universal character. The newly recorded locality, complete with the geomorphologic patterns of periglacial relief in the southern foothills of Trojan on Pešter, is very interesting for broader scientific community, and is suggested for protection so it could be studied and promoted further.
AB  - Otkrivanje novih lokaliteta sa aktivnim periglacijalnim procesima dovodi do njihovog detaljnijeg istraživanja multidisciplinarnog karaktera. Posebno su interesantni rezultati klimatoloških istraživanja, gde se putem mraznog potencijala došlo do preduslova za pojavu mraznih travnih humki. To nije strogo namenjeno uslovima na Pešteru, već ima univerzalni karakter. Novootkrivena lokacija sa geomorfološkim oblicima periglacijalnog reljefa na južnom podnožju Trojana na Pešteru je veoma interesantna i za širu naučnu javnost i predlaže se za zaštitu radi daljih istraživanja i promocije.
PB  - Zavod za zaštitu prirode, Beograd
T2  - Zaštita prirode
T1  - Frosted grass mounds-tufurs on the Pešter peripheral area
T1  - Mrazne travne humke-tufuri na obodu Pešterskog polja
VL  - 55
IS  - 1-2
SP  - 15
EP  - 27
UR  - https://hdl.handle.net/21.15107/rcub_gery_98
ER  - 

@article{
author = "Belij, Srđan and Ducić, Vladan and Milovanović, Boško and Luković, Jelena and Mišćević, Igor",
year = "2004",
abstract = "When new localities with active periglacial processes are discovered, that leads to detailed study of these areas that is multidisciplinary in character. Especially interesting are results of climatologic research where climatic or frost potentials were used to determine the climatic conditions necessary for appearance of frost grass mounds. This is not strictly connected only with conditions on Pešter, but has a universal character. The newly recorded locality, complete with the geomorphologic patterns of periglacial relief in the southern foothills of Trojan on Pešter, is very interesting for broader scientific community, and is suggested for protection so it could be studied and promoted further., Otkrivanje novih lokaliteta sa aktivnim periglacijalnim procesima dovodi do njihovog detaljnijeg istraživanja multidisciplinarnog karaktera. Posebno su interesantni rezultati klimatoloških istraživanja, gde se putem mraznog potencijala došlo do preduslova za pojavu mraznih travnih humki. To nije strogo namenjeno uslovima na Pešteru, već ima univerzalni karakter. Novootkrivena lokacija sa geomorfološkim oblicima periglacijalnog reljefa na južnom podnožju Trojana na Pešteru je veoma interesantna i za širu naučnu javnost i predlaže se za zaštitu radi daljih istraživanja i promocije.",
publisher = "Zavod za zaštitu prirode, Beograd",
journal = "Zaštita prirode",
title = "Frosted grass mounds-tufurs on the Pešter peripheral area, Mrazne travne humke-tufuri na obodu Pešterskog polja",
volume = "55",
number = "1-2",
pages = "15-27",
url = "https://hdl.handle.net/21.15107/rcub_gery_98"
}

Belij, S., Ducić, V., Milovanović, B., Luković, J.,& Mišćević, I.. (2004). Frosted grass mounds-tufurs on the Pešter peripheral area. in Zaštita prirode
Zavod za zaštitu prirode, Beograd., 55(1-2), 15-27.
https://hdl.handle.net/21.15107/rcub_gery_98

Belij S, Ducić V, Milovanović B, Luković J, Mišćević I. Frosted grass mounds-tufurs on the Pešter peripheral area. in Zaštita prirode. 2004;55(1-2):15-27.
https://hdl.handle.net/21.15107/rcub_gery_98 .

Belij, Srđan, Ducić, Vladan, Milovanović, Boško, Luković, Jelena, Mišćević, Igor, "Frosted grass mounds-tufurs on the Pešter peripheral area" in Zaštita prirode, 55, no. 1-2 (2004):15-27,
https://hdl.handle.net/21.15107/rcub_gery_98 .