Greenland ice core project (original) (raw)
Il Greenland Ice Core Project (GRIP) era un progetto di ricerca multinazionale europeo, condotto in Groenlandia sotto la supervisione della Fondazione europea per la scienza. Il progetto era finanziato da otto nazioni europee: Belgio, Danimarca, Francia, Germania, Islanda, Italia, Svizzera e Regno Unito, oltre all'Unione europea.
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| dbo:abstract | Das Greenland Ice Core Project (abgekürzt: GRIP) war ein multinationales europäisches Projekt zur Erforschung des grönländischen Inlandseises. In den Jahren 1989 bis 1992 wurde der Eisschild in Zentralgrönland 73° N, 38° W nahe Summit, dem höchsten Punkt des Eisschilds, bis in eine Tiefe von 3029 Metern erbohrt, wo man auf felsigen Grund stieß. Die ältesten Teile des Eisbohrkerns kommen aus einer Tiefe, in der das Eis ein Alter von mehr als 200.000 Jahren erreicht hat. Der Bohrkern kann Aufschluss über die Ökologie und Klimageschichte der letzten rund 100.000 Jahre geben, das ist der Bereich, in dem der Kern ungestört und eindeutig datierbar ist. Organisiert wurde das Projekt von der Europäischen Wissenschaftsstiftung, die Finanzierung kam aus Belgien, Dänemark, Deutschland, Frankreich, Island, Italien, der Schweiz, dem Vereinigten Königreich und der Europäischen Union. Etwa 28 km westlich davon wurde zur etwa gleichen Zeit im Rahmen des von US-Forschungsinstitutionen finanzierten Greenland Ice Sheet Project (GISP) ein weiterer Eisbohrkern (GISP2) gewonnen. (de) El Proyecto de muestras de hielo de Groenlandia (acrónimo en inglés GRIP,Greenland ice core project) fue un proyecto multinacional europeo de investigación, organizado por la Fundación europea de la Ciencia, con fondos de 8 naciones: Bélgica, Dinamarca, Francia, Alemania, Islandia, Italia, Suiza, RU), y de la Unión Europea. GRIP perforó exitosamente hasta una profundidad de 3.028 m de muestras de hielo hasta la base de la Capa de hielo de Groenlandia en Summit, Groenlandia Central de 1989 a 1992, en 72°35′N 37°38′O / 72.583, -37.633. Los estudios de isótopos y varios constituyentes atmosféricos en las muestras revelan los detallados registros de variaciones climáticas alcanzando más de 100 ka (kiloaños) en el tiempo. Los resultados indican que el clima del Holoceno ha estado remarcablemente estable, y confirmando la ocurrencia de variaciones climáticas vertiginosas durante la última Era Glaciar (la glaciación de Würm o Wisconsin). Las variaciones δ18O observadas en parte de las muestras hacen creer en la exactitid del fechaje del Interglacial Riss-Würm (o interglacial Eemiano) que no habían sido confirmadas por otros registros [1] incluyendo al Proyecto NGRIP (o Proyecto de muestras de hielo del norte de Groenlandia), y parecen indicar que el evento intergracial Eemiano aparece ser tan estable como el Holoceno. (es) The Greenland Ice Core Project (GRIP) was a multinational European research project, organised through the European Science Foundation (ESF). The project ran from 1989 to 1995, with drilling seasons from 1990 to 1992. In 1988, the project was first accepted as an ESF associated program, and in the summer of 1989, the fieldwork was started in Greenland. GRIP aimed to collect and investigate 3000-metre-long ice cores drilled at the apex of the Greenland ice sheet, also known as Summit Camp. The Greenland ice sheet occupies more than 90% of the total ice sheet and glacier ice on the Earth, excluding the Antarctic ice sheet. The project was managed by the Steering Committee called Physikalisches Institut der Universität Bern, Switzerland, chaired by Professor Bernhard Stauffer. Funding came from 8 nations (Belgium, Denmark, France, Germany, Iceland, Italy, Switzerland, and United Kingdom), and from the European Union. The Commission of the European Community has offered a part of the funding through the European Research Network of Excellence in Open Cultural Heritage (EPOCH) program. (en) Il Greenland Ice Core Project (GRIP) era un progetto di ricerca multinazionale europeo, condotto in Groenlandia sotto la supervisione della Fondazione europea per la scienza. Il progetto era finanziato da otto nazioni europee: Belgio, Danimarca, Francia, Germania, Islanda, Italia, Svizzera e Regno Unito, oltre all'Unione europea. (it) |
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| dbo:wikiPageExternalLink | http://neem.dk/documentation/2015/Renland-EGRIP2015FieldPlan.pdf%7Ctitle=Field http://www.iceandclimate.nbi.ku.dk/research/drill_analysing/history_drilling/central_ice_cores/ https://spicecore.org/about/%3C/nowiki%3E https://www.iceandclimate.nbi.ku.dk/research/drill_analysing/history_drilling/central_ice_cores/%3C/nowiki%3E https://www.nipr.ac.jp/arcs/blog/en/2017/12/EGRIP2017-2.html%3C/nowiki%3E https://www.global.hokudai.ac.jp/blog/greenland-ice-sheet-may-halve-in-volume-by-year-3000/%3C/nowiki%3E http://www.nerc-bas.ac.uk/icd/grip/griplist.html https://doi.org/10.1029/2004JD005575%3C/nowiki%3E https://doi.org/10.1073/pnas.2021442118%3C/nowiki%3E https://doi.org/10.1126/science.1157707%3C/nowiki%3E https://doi.org/10.3189/002214309790152483%3C/nowiki%3E https://doi.org/10.5194/tc-15-3655-2021%3C/nowiki%3E https://web.archive.org/web/20120207150245/http:/www.esf.org/activities/research-networking-programmes/life-earth-and-environmental-sciences-lesc/completed-esf-research-networking-programmes-in-life-earth-and-environmental-sciences/greenland-icecore-project-grip/more-information.html%3C/nowiki%3E https://www.carbonbrief.org/new-climate-models-suggest-faster-melting-of-the-greenland-ice-sheet/%3C/nowiki%3E http://www.ncdc.noaa.gov/paleo/icecore/greenland/summit/document/gripinfo.htm |
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| rdfs:comment | Il Greenland Ice Core Project (GRIP) era un progetto di ricerca multinazionale europeo, condotto in Groenlandia sotto la supervisione della Fondazione europea per la scienza. Il progetto era finanziato da otto nazioni europee: Belgio, Danimarca, Francia, Germania, Islanda, Italia, Svizzera e Regno Unito, oltre all'Unione europea. (it) Das Greenland Ice Core Project (abgekürzt: GRIP) war ein multinationales europäisches Projekt zur Erforschung des grönländischen Inlandseises. In den Jahren 1989 bis 1992 wurde der Eisschild in Zentralgrönland 73° N, 38° W nahe Summit, dem höchsten Punkt des Eisschilds, bis in eine Tiefe von 3029 Metern erbohrt, wo man auf felsigen Grund stieß. Die ältesten Teile des Eisbohrkerns kommen aus einer Tiefe, in der das Eis ein Alter von mehr als 200.000 Jahren erreicht hat. Der Bohrkern kann Aufschluss über die Ökologie und Klimageschichte der letzten rund 100.000 Jahre geben, das ist der Bereich, in dem der Kern ungestört und eindeutig datierbar ist. (de) The Greenland Ice Core Project (GRIP) was a multinational European research project, organised through the European Science Foundation (ESF). The project ran from 1989 to 1995, with drilling seasons from 1990 to 1992. In 1988, the project was first accepted as an ESF associated program, and in the summer of 1989, the fieldwork was started in Greenland. GRIP aimed to collect and investigate 3000-metre-long ice cores drilled at the apex of the Greenland ice sheet, also known as Summit Camp. The Greenland ice sheet occupies more than 90% of the total ice sheet and glacier ice on the Earth, excluding the Antarctic ice sheet. The project was managed by the Steering Committee called Physikalisches Institut der Universität Bern, Switzerland, chaired by Professor Bernhard Stauffer. Funding came fr (en) El Proyecto de muestras de hielo de Groenlandia (acrónimo en inglés GRIP,Greenland ice core project) fue un proyecto multinacional europeo de investigación, organizado por la Fundación europea de la Ciencia, con fondos de 8 naciones: Bélgica, Dinamarca, Francia, Alemania, Islandia, Italia, Suiza, RU), y de la Unión Europea. GRIP perforó exitosamente hasta una profundidad de 3.028 m de muestras de hielo hasta la base de la Capa de hielo de Groenlandia en Summit, Groenlandia Central de 1989 a 1992, en 72°35′N 37°38′O / 72.583, -37.633. (es) |
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