Abstract
The last 10,000 years, the Holocene warm period, were characterized by relatively stable temperature conditions in southwestern Bulgaria, which is documented in the altitude range of the alpine timberline and the variability of glaciers and moraines of the high mountains. The climate of the Modern Time Era (including the Little Ice Age period) can be described in higher resolution by means of the geoarchive Pinus heldreichii. The 500-year dendrology-based reconstruction of the temperature and precipitation course gives indications, although compared to other proxy-data it certainly needs further improvement and crosschecking. The present trends of global warming are clearly detectable in the Pirin region. But the climate change in the twentieth century was not as distinct as in other European regions nor considered global.
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Grunewald, K., Scheithauer, J. (2011). Specifics of the Regional Climate and Landscape History. In: Landscape Development and Climate Change in Southwest Bulgaria (Pirin Mountains). Springer, Dordrecht. https://doi.org/10.1007/978-90-481-9959-4_5
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