International Permafrost Association
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International Permafrost Association
The International Permafrost Association (IPA), founded in 1983, has as its objectives to foster the dissemination of knowledge concerning permafrost and to promote cooperation among persons and national or international organisations engaged in scientific investigation and engineering work related to permafrost and seasonally frozen ground. The IPA became an Affiliated Organisation of the International Union of Geological Sciences in July 1989. The Association’s primary responsibilities are to convene International Permafrost Conferences, undertake special projects such as preparing databases, maps, bibliographies, and glossaries, and coordinate international field programmes and networks. The International Conference On Permafrost (ICOP) is regularly held since 1965. Permafrost or perennially frozen ground is defined as earth material that remains at or below 0 °C for at least two consecutive years. As such, upwards of 25% of Planet Earth is underlain to some degree by ...
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International Nongovernmental Organization
An international non-governmental organization (INGO) is an organization which is independent of government involvement and extends the concept of a non-governmental organization (NGO) to an international scope. NGOs are independent of governments and can be seen as two types: ''advocacy NGOs'', which aim to influence governments with a specific goal, and ''operational NGOs'', which provide services. Examples of NGO mandates are environmental preservation, human rights promotions or the advancement of women. NGOs are typically not-for-profit, but receive funding from companies or membership fees. Many large INGOs have components of operational projects and advocacy initiatives working together within individual countries. The technical term "international organizations" describes intergovernmental organizations (IGOs) and include groups such as the United Nations or the International Labour Organization, which are formed by treaties among sovereign states. In contrast, INGOs are ...
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Periglacial
Periglaciation (adjective: "periglacial", also referring to places at the edges of glacial areas) describes geomorphic processes that result from seasonal thawing of snow in areas of permafrost, the runoff from which refreezes in ice wedges and other structures. "Periglacial" suggests an environment located on the margin of past glaciers. However, freeze and thaw cycles influence landscapes outside areas of past glaciation. Therefore, periglacial environments are anywhere that freezing and thawing modify the landscape in a significant manner. Tundra is a common ecological community in periglacial areas. History Periglaciation became a distinct subject within the study of geology after Walery Łoziński, a Polish geologist, introduced the term in 1909. Łoziński drew upon the early work of Johan Gunnar Andersson. According to Alfred Jahn, his introduction of his work at the 1910 International Geological Congress held in Stockholm caused significant discussion. In the field trip ...
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International Geographical Union
The International Geographical Union (IGU; french: Union Géographique Internationale, UGI) is an international geographical society. The first International Geographical Congress was held in Antwerp in 1871. Subsequent meetings led to the establishment of the permanent organization in Brussels, Belgium, in 1922. The International Geographical Union adheres to the International Science Council (ISC), which it recognizes as the coordinating body for the international organisations of science. Objectives The IGU has seven objectives or aims: # to promote the study of geographical problems; # to initiate and co-ordinate geographical research requiring international co-operation and to promote its scientific discussion and publication; # to provide for the participation of geographers in the work of relevant international organizations; # to facilitate the collection and diffusion of geographical data and documentation in and between all member countries; # to promote Internationa ...
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Permafrost Young Researchers Network
The Permafrost Young Researcher’s Network (PYRN) is a network formed in 2005 to formally facilitate and strengthen contacts among young scientists in the permafrost community. It arose from the need for an integrated single source of information for specific resources vital to young scientists (fellowships, conference travel funding, position opportunities, etc.). Additionally, the imminence of the International Polar Year (IPY) prompted the need for a visible representation of the young permafrost community at the international level. The Permafrost Young Researchers Network has therefore been formally established within the International Permafrost Association (IPA) framework and has created and maintains means of communication among young researchers involved in permafrost research. It reports on young researchers’ activities to the IPA membership and working parties and represents permafrost scientists and engineers within broader international and national assemblages. ...
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Global Carbon Project
The Global Carbon Project (GCP) is an organisation that seeks to quantify global greenhouse gas emissions and their causes. Established in 2001, its projects include global budgets for three dominant greenhouse gases—carbon dioxide (), methane (), and nitrous oxide ()—and complementary efforts in urban, regional, cumulative, and negative emissions. The main object of the group has been to fully understand the carbon cycle. The project has brought together emissions experts, earth scientists, and economists to tackle the problem of rising concentrations of greenhouse gases. In 2020, the project released its newest Global Methane Budget and first Global Nitrous Oxide Budget, the two anthropogenic trace gases most dominant for warming after carbon dioxide. The Global Carbon Project collaborates with many groups to gather, analyze, and publish data on greenhouse gas emissions in an open and transparent fashion, making datasets available on its website and through its publicatio ...
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Cryosols
Gelisols are an order in USDA soil taxonomy. They are soils of very cold climates which are defined as containing permafrost within two meters of the soil surface. The word "Gelisol" comes from the Latin ''gelare'' meaning "to freeze", a reference to the process of cryoturbation that occurs from the alternating thawing and freezing characteristic of Gelisols. In the World Reference Base for Soil Resources (WRB), Gelisols are known as Cryosols. In soil taxonomy, Gelisols key out before the Histosols. In the WRB, the Histosols key out before the Cryosols. Organic permafrost soils are therefore Gelisols (Histels) in the soil taxonomy and Histosols (Cryic Histosols) in the WRB. Structurally, Gelisols may have a B horizon and more commonly have an A horizon and/or O horizon resting on the permafrost. Because soil organic matter accumulates in the upper layer, most Gelisols are black or dark brown in soil color, followed by a shallow mineral layer. Despite the influence of glaciation ...
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Glaciers
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur only ...
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Data Assimilation
Data assimilation is a mathematical discipline that seeks to optimally combine theory (usually in the form of a numerical model) with observations. There may be a number of different goals sought – for example, to determine the optimal state estimate of a system, to determine initial conditions for a numerical forecast model, to interpolate sparse observation data using (e.g. physical) knowledge of the system being observed, to set numerical parameters based on training a model from observed data. Depending on the goal, different solution methods may be used. Data assimilation is distinguished from other forms of machine learning, image analysis, and statistical methods in that it utilizes a dynamical model of the system being analyzed. Data assimilation initially developed in the field of numerical weather prediction. Numerical weather prediction models are equations describing the dynamical behavior of the atmosphere, typically coded into a computer program. In order to use th ...
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Global Terrestrial Network For Permafrost
The Global Terrestrial Network for Permafrost (GTN‐P) is the primary international programme concerned with monitoring permafrost parameters. GTN‐P was developed in the 1990s by the International Permafrost Association (IPA) under the Global Climate observing System (GCOS) and thGlobal Terrestrial Observing Network (GTOS) with the long-term goal of obtaining a comprehensive view of the spatial structure, trends and variability of changes in the active layer thickness and permafrost temperature. GCOS and GTOS established 50 Essential Climate Variables (ECVs),{{cite web , url=https://public.wmo.int/en/programmes/global-climate-observing-system/essential-climate-variables , title=Essential Climate Variables , author= , date=2018 , publisher= World Meteorological Organization , access-date=2018-02-13 of which one is permafrost. Within the GTN-P, involving the senior and young permafrost scientific community, two permafrost key variables have been identified as ECV's: * thTher ...
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University Of Lisbon
The University of Lisbon (ULisboa; pt, Universidade de Lisboa, ) is a public research university in Lisbon, and the largest university in Portugal. It was founded in 2013, from the merger of two previous public universities located in Lisbon, the former University of Lisbon (1911–2013) and the Technical University of Lisbon (1930–2013). History The first Portuguese university was established in Lisbon between 1288 and 1290, when Dinis I promulgated the letter ''Scientiae thesaurus mirabili'', granting several privileges to the students of the ''studium generale'' in Lisbon, proving that it was already founded on that date. There was an active participation in this educational activity by the Portuguese Crown and its king, through its commitment of part of the subsidy of the same, as by the fixed incomes of the Church. This institution moved several times between Lisbon and Coimbra, where it settled permanently in 1537. The current University of Lisbon is the result of the ...
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University Of Évora
The University of Évora (''Universidade de Évora'') is a public university in Évora, Portugal. It is the second oldest university in the country, established in 1559 by the cardinal Henry, and receiving University status in April of the same year from Pope Paul IV, as documented in his ''Cum a nobis'' papal bull. Running under the aegis of the Society of Jesus (also known as Jesuits) meant that the university was a target of the Marquis of Pombal's Jesuit oppression, being closed down permanently in 1779 and its masters either incarcerated or exiled. It was reopened nearly two hundred years later in 1973 as ''Instituto Universitário de Évora'' (University Institute of Évora) by decree of the Minister of Education, José Veiga Simão, in the site of the older university, as part of a set of education policies during the early 1970s that were attempting to reshape Portuguese higher education. Six years later, in 1979, the name was changed to ''Universidade de Évora''. His ...
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Fourth European Conference On Permafrost (EUCOP IV)
Fourth or the fourth may refer to: * the ordinal form of the number 4 * ''Fourth'' (album), by Soft Machine, 1971 * Fourth (angle), an ancient astronomical subdivision * Fourth (music), a musical interval * ''The Fourth'' (1972 film), a Soviet drama See also * * * 1/4 (other) * 4 (other) 4 is a number, numeral, and digit. 4 or four may also refer to: Months and years * AD 4, the fourth year of the AD era * 4 BC, the fourth year before the AD era * 1904 * 2004 * The month of April Places * Four, Isère, a French commune ... * The fourth part of the world (other) * Forth (other) * Quarter (other) * Independence Day (United States), or The Fourth of July {{Disambiguation ...
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