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2nd International Congress of Alpine and Arctic Botanical Gardens

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Detection <strong>of</strong> climate change impacts in alpine <strong>and</strong><br />

arctic botanic gardens: a phenology program<br />

Andreas GRÖGER<br />

Alpengarten auf dem Schachen/ Botanischer Garten München, Germany<br />

Annette MENZEL<br />

Fachgebiet für Ökoklimatologie / Technische Universität München, Germany<br />

Since decades many Botanic <strong>Gardens</strong> in the lowl<strong>and</strong>s are conducting st<strong>and</strong>ardized phenological observations<br />

<strong>of</strong> cloned plants, recording timing <strong>of</strong> leaf unfolding, flowering, fruit ripening, leaf coloring, <strong>and</strong> leaf<br />

fall (e. g. <strong>International</strong> Phenological <strong>Gardens</strong> project, since 1959). But long term observations from higher<br />

elevations, which are affected even more severely by climate change, are still very scarce. <strong>Alpine</strong> <strong>and</strong> <strong>Arctic</strong><br />

Botanic <strong>Gardens</strong> (AABGs) <strong>of</strong>fer a perfect field for these studies, allowing to compare the effect <strong>of</strong> climate<br />

change on genetically identical plants under alpine as well as arctic conditions. Following AABGs agreed to<br />

cooperate in a joint phenological program: Alpengarten auf dem Schachen (Germany), Giardino Botanico<br />

Alpino Viotte (Italy), Jardin Botanique Alpin du Lautaret (France), Tromsø <strong>Arctic</strong>-<strong>Alpine</strong> Botanic Garden<br />

(Norway) <strong>and</strong> Reykjavik Botanic Garden (Icel<strong>and</strong>).<br />

Effects <strong>of</strong> climate change on plant life<br />

In 2007, the Intergovernmental Panel on<br />

Climate Change (IPCC) has drawn very different<br />

scenarios. Two years later, rising CO emissions<br />

2<br />

<strong>and</strong> further results in climate research pro<strong>of</strong>,<br />

that the worst case scenario becomes more than<br />

probable, i.e. an average increase <strong>of</strong> atmosphere<br />

temperature <strong>of</strong> more than 4°C until 2100. The<br />

effects on biodiversity will be drastic (Rosenzweig<br />

et al. 2007).<br />

One <strong>of</strong> the hard hit environments will be subalpine<br />

<strong>and</strong> alpine biomes. But nevertheless, data<br />

on the effects <strong>of</strong> climate change to ecosystems<br />

in high altitudes are still quite scarce. In general,<br />

with each °C increase <strong>of</strong> temperature in the<br />

mountains, the duration <strong>of</strong> snow cover decreases<br />

by several weeks, the glacier line shifts upward<br />

by 60 to 140 m <strong>and</strong> the treeline shifts upward by<br />

several 100 m.<br />

The only options for plant species to respond<br />

to these changes are migration to higher altitudes<br />

or higher latitudes (Parmesan & Yohe,<br />

2003) or adaptation (ecological plasticity, microevolution).<br />

Especially temperature <strong>and</strong> drought<br />

sensitive species <strong>and</strong> species which are poor<br />

dispersers, will face the risk <strong>of</strong> extinction. For<br />

some mountain ranges the prognosis <strong>of</strong> loss<br />

<strong>of</strong> local plant species exceeds 60%, assuming a<br />

temperature increase <strong>of</strong> 4°C.<br />

Research <strong>and</strong> Conservation Activities 47

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