Vitosha Mountain (SW Bulgaria) during the Little Ice Age in the context of past climate changes in the Balkans

Jordan Tzvetkov
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Abstract

This study aims to present and analyse several descriptions of snow cover conditions on Vitosha Mountain over the last five centuries. It uses the written historical sources and diachronic method. They are discussed in the context of available climate and environmental data for Bulgaria and the adjacent areas of the Balkans during the Little Ice Age (LIA). It can be concluded from the presented descriptions of Vitosha during the LIA that probably in the 17th and early 18th centuries Vitosha had significantly longer snow retention with the presence of permanent or semi-permanent snow patches, a situation that is significantly different from the present environmental conditions. The analysis of the climatic conditions during the LIA in other regions of Bulgaria, as well as in neighboring countries in the Balkans, shows that during this period, especially in the southern parts of the Balkan Peninsula, there was a significant climate cooling. Future studies of the (high resolution) natural archives in Bulgaria are needed to provide more information about the nature of climatic and environmental changes during the LIA.
在巴尔干地区过去气候变化的背景下,小冰河期的维托沙山(保加利亚西南部)
本研究旨在介绍和分析过去五个世纪以来维托沙山积雪状况的几种描述。它使用书面的历史资料和历时法。它们是在保加利亚和巴尔干邻近地区在小冰期(LIA)的现有气候和环境数据的背景下进行讨论的。从对小冰期维托沙的描述可以得出结论,可能在17世纪和18世纪初,维托沙的雪滞留时间明显更长,存在永久或半永久的雪块,这种情况与现在的环境条件有很大的不同。对保加利亚其他地区以及巴尔干周边国家在LIA期间气候条件的分析表明,在此期间,特别是在巴尔干半岛南部,气候明显变冷。今后需要对保加利亚的(高分辨率)自然档案进行研究,以便提供更多关于低冰期气候和环境变化性质的资料。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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