The Global Observation Research Initiative in Alpine Environments (GLORIA) established an international long-term monitoring program and site-based network dealing with high-mountain vegetation and its biological diversity. Its purpose is the in-situ observation and comparative assessment of alpine biodiversity patterns under the impact of accelerating anthropogenic climate change. [1] GLORIA involves sets of permanent plots established at pristine or near-natural sites set aside and monitored to observe the migration of plant species due to climate change. [2] Founded in 2001, the program has grown to more than 120 sites (status January 2016) around the world, distributed from the poles to the tropics."
The idea to monitor alpine plant communities in the context of anthropogenic climate and global change was first discussed in 1996 during a workshop of the International Geosphere-Biosphere Programme in Kathmandu. In consequence, the GLORIA monitoring approach was initiated by the Austrian ecologists Georg Grabherr, Michael Gottfried and Harald Pauli at the turn of the century, by running experiments in alpine habitats to determine what a good sample method might be. In 2001, GLORIA-Europe was launched. This major pilot project, with 18 sites in 13 different European nations, was a way to test out the idea before going worldwide. [3] Since the spring of 2004, GLORIA has been successively expanding into other regions and across all major climate zones of the world.
Comparability, simplicity and economy were the main considerations in designing GLORIA's standard recording design and method (Multi-Summit Approach), in order to build a world-wide network of operable sites. In each study region (target region) a suite of four monitoring locations in summit areas at different altitudes represents an elevation gradient from the treeline ecotone to the upper limits of plant life. At each location, vascular plant species and abundances are to be recorded in standardized permanent plots of different size at intervals of 5 to 10 years, along with continuous measurements of soil temperature. [2] Several supplementary approaches, e.g., focusing on other organism groups, soil ecology or on socio-ecological features, are applied or are under development in some study regions. The network consists of dedicated ecologists and biologists from over hundred research institutions and many protected area authorities, distributed over six continents and it cooperates with other international efforts such as the Global Mountain Biodiversity Assessment of the Future Earth programme and the LTSER network. GLORIA's head office and central data base is affiliated to at the Austrian Academy of Sciences (Institute for Interdisciplinary Mountain Research) and the University of Natural Resources and Life Sciences Vienna (Center for Global Change and Sustainability), Austria.
On a pan-European scale, repeated surveys showed widespread thermophilisation of alpine vegetation, i.e., species compositions changed towards a larger percentage of thermophilous species at a concurrent decline of cold-adapted high-elevation species. [4] Across Europe, species predominantly were shifting to higher elevations during the past decade. In central and northern Europe, this led to increasing species numbers in the permanent plots, whereas in Mediterranean mountains, species numbers were stagnating or declining, probably owing to combined effects of increasing temperatures and decreasing precipitation. [5] Recent declines of high elevation specialist species, however, were also observed in the European Alps. [6] Comparisons with results from other continents are not yet available on a larger scale, because permanent sites were established at a later date.
The Alps are one of the highest and most extensive mountain ranges in Europe, stretching approximately 1,200 km (750 mi) across eight Alpine countries : Monaco, France, Switzerland, Italy, Liechtenstein, Germany, Austria and Slovenia.
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (980 ft) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges.
The Alpine region of Switzerland, conventionally referred to as the Swiss Alps, represents a major natural feature of the country and is, along with the Swiss Plateau and the Swiss portion of the Jura Mountains, one of its three main physiographic regions. The Swiss Alps extend over both the Western Alps and the Eastern Alps, encompassing an area sometimes called Central Alps. While the northern ranges from the Bernese Alps to the Appenzell Alps are entirely in Switzerland, the southern ranges from the Mont Blanc massif to the Bernina massif are shared with other countries such as France, Italy, Austria and Liechtenstein.
A cloud forest, also called a water forest, primas forest, or tropical montane cloud forest, is a generally tropical or subtropical, evergreen, montane, moist forest characterized by a persistent, frequent or seasonal low-level cloud cover, usually at the canopy level, formally described in the International Cloud Atlas (2017) as silvagenitus. Cloud forests often exhibit an abundance of mosses covering the ground and vegetation, in which case they are also referred to as mossy forests. Mossy forests usually develop on the saddles of mountains, where moisture introduced by settling clouds is more effectively retained.
Alpine tundra is a type of natural region or biome that does not contain trees because it is at high elevation, with an associated harsh climate. As the latitude of a location approaches the poles, the threshold elevation for alpine tundra gets lower until it reaches sea level, and alpine tundra merges with polar tundra.
A meadow is an open habitat or field, vegetated by grasses, herbs, and other non-woody plants. Trees or shrubs may sparsely populate meadows, as long as these areas maintain an open character. Meadows can occur naturally under favourable conditions, but are often artificially created from cleared shrub or woodland for the production of hay, fodder, or livestock. Meadow habitats, as a group, are characterized as "semi-natural grasslands", meaning that they are largely composed of species native to the region, with only limited human intervention.
The tree line is the edge of a habitat at which trees are capable of growing and beyond which they are not. It is found at high elevations and high latitudes. Beyond the tree line, trees cannot tolerate the environmental conditions. The tree line is sometimes distinguished from a lower timberline, which is the line below which trees form a forest with a closed canopy.
Alpine climate is the typical climate for elevations above the tree line, where trees fail to grow due to cold. This climate is also referred to as a mountain climate or highland climate.
Silene acaulis, known as moss campion or cushion pink, is a small wildflower that is common all over the high arctic and tundra and in high mountains of Eurasia and North America. It is an evergreen perennial flowering plant in the carnation family Caryophyllaceae.
Jade Dragon Snow Mountain is a mountain massif or small mountain range in Yulong Naxi Autonomous County, Lijiang, in Yunnan province, China. Its highest peak is named Shanzidou or Shan-Tzu-tou (扇子陡) and it is 5,596 m (18,360 ft) above sea level.
Altitudinal zonation in mountainous regions describes the natural layering of ecosystems that occurs at distinct elevations due to varying environmental conditions. Temperature, humidity, soil composition, and solar radiation are important factors in determining altitudinal zones, which consequently support different vegetation and animal species. Altitudinal zonation was first hypothesized by geographer Alexander von Humboldt who noticed that temperature drops with increasing elevation. Zonation also occurs in intertidal and marine environments, as well as on shorelines and in wetlands. Scientist C. Hart Merriam observed that changes in vegetation and animals in altitudinal zones map onto changes expected with increased latitude in his concept of life zones. Today, altitudinal zonation represents a core concept in mountain research.
There is an ongoing decline in plant biodiversity, just like there is ongoing biodiversity loss for many other life forms. One of the causes for this decline is climate change. Environmental conditions play a key role in defining the function and geographic distributions of plants. Therefore, when environmental conditions change, this can result in changes to biodiversity. The effects of climate change on plant biodiversity can be predicted by using various models, for example bioclimatic models.
Montane ecosystems are found on the slopes of mountains. The alpine climate in these regions strongly affects the ecosystem because temperatures fall as elevation increases, causing the ecosystem to stratify. This stratification is a crucial factor in shaping plant community, biodiversity, metabolic processes and ecosystem dynamics for montane ecosystems. Dense montane forests are common at moderate elevations, due to moderate temperatures and high rainfall. At higher elevations, the climate is harsher, with lower temperatures and higher winds, preventing the growth of trees and causing the plant community to transition to montane grasslands and shrublands or alpine tundra. Due to the unique climate conditions of montane ecosystems, they contain increased numbers of endemic species. Montane ecosystems also exhibit variation in ecosystem services, which include carbon storage and water supply.
Geum talbotianum, also known as the Tasmanian snowrose, is a perennial rosette herb endemic to Tasmania and confined to the high rocky places of Tasmania's Southern mountains.
The Himalayan Alpine Dynamics Research Initiative (HIMADRI) involves a set of pristine sites set aside and monitored to observe the migration of plant species due to climate change. Established in 2013, the program has taken care of gap in Indian Himalaya monitoring.
Jan Salick is an American botanist who researches the interaction between humans and plants (ethnobotany) and conservation biology. Her specialisms include alpine environments, climate change, indigenous peoples and traditional knowledge. She is a past-president of the Society for Economic Botany and holds their Distinguished Economic Botanist award. She is also Fellow of the American Association for the Advancement of Science and received the Fairchild Medal for Plant Exploration. In 2019 she retired as Senior Curator of Ethnobotany at the Missouri Botanical Garden, and now has emerita status.
Climate change is affecting Austrian temperatures, weather, ecosystems and biodiversity. Since 1950 temperatures have risen by 1.8 °C, and in the past 150 years glaciers have melted, losing a significant amount of their volume. Changed precipitation patterns, increased temperatures, reduced snowfall, melting glaciers and more frequent extreme weather phenomenon, such as droughts, are expected effects from climate change. Ecosystems and biodiversity in Austria are facing changes due to increasing temperatures and the spread of thermophile species, heat and drought stress on animals and plants, an increase in alien and invasive species and an increase in pathogenic organisms and the spread of disease.
Constance I. Millar is an American research ecologist working for the United States Forest Service at the Pacific Southwest Research Station in Berkeley, California. Her work focuses on the effects of climate change on high-elevation ecosystems in both the past and the present. She has also developed ways to evolve management techniques of forest ecosystems to improve the ability to protect them against climate change.
Carex tristis is a species of sedge, native to the Caucasus Mountains and adjoining areas. It is the most abundant plant species found on summits.
An alpine lake is a high-altitude lake in a mountainous area, usually near or above the tree line, with extended periods of ice cover. These lakes are commonly glacial lakes formed from glacial activity but can also be formed from geological processes such as volcanic activity or landslides. Many alpine lakes that are fed from glacial meltwater have the characteristic bright turquoise green color as a result of glacial flour, suspended minerals derived from a glacier scouring the bedrock. When active glaciers are not supplying water to the lake, such as a majority of Rocky Mountains alpine lakes in the United States, the lakes may still be bright blue due to the lack of algal growth resulting from cold temperatures, lack of nutrient run-off from surrounding land, and lack of sediment input. The coloration and mountain locations of alpine lakes attract lots of recreational activity.
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