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PINGO – Peer Instruction for large groups – uni-due.de

https://www.uni-due.de/zim/services/pingo.php

[email protected] Campus Essen Schützenbahn 70 45127 Essen. Campus Duisburg Forsthausweg 2 47048 Duisburg Adressen & Orientierung. Organisationsstruktur. Hotline. Für technische Fragen und … Tel (Du) +49 203 379-2221 Tel (E) +49 201 183-4444 E-Mail [email protected] Formular zur Störungsmeldung. Feedback. Beratungszentrum e-Point. Mo-Fr 09:00 – 19:00 Uhr Tel (Du) +49 203 379 …

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You have collected data on the average weekly amount of … – uni …

https://www.be.msm.uni-due.de/fileadmin/Dateien/Behavioral_Economics/Pingo_Questions.pdf

B) is something that certain undergraduate majors at your university/college other than economics seem to have an ∞ amount of. C) are (n-2) when replacing the population mean by the sample mean. ANSWER: A A large p-value implies A) rejection of the null hypothesis. B) a large t-statistic. C) a large Ybar_act.

PINGO

https://pingo.coactum.de/

[email protected] PINGO is an open-source class room system, made by the University of Paderborn.

Pingo – Wikipedia

https://en.wikipedia.org/wiki/Pingos

Pingos are intrapermafrost ice-cored hills, ranging in height from 3 to 70 m and 30 to 1,000 m in diameter. They are typically conical in shape and grow and persist only in permafrost environments, such as the Arctic and subarctic. A pingo is a periglacial landform, which is defined as a non-glacial landform or process linked to colder climates. It is estimated that there are more than 11,000 pingos on Earth. The …

Pingo | Encyclopedia.com

https://www.encyclopedia.com/earth-and-environment/ecology-and-environmentalism/environmental-studies/pingo

08/05/2018  · pingo Ice-cored, dome-shaped hill, oval in plan, standing 2–50 m high, and 30–600 m in diameter, developed in an area of permafrost. The larger examples have breached crests in which ice may be exposed. They are probably due to local freezing of water that has migrated from adjacent uplands, or to the late freezing of the ground beneath a lake.

Pingo – an overview | ScienceDirect Topics

https://www.sciencedirect.com/topics/earth-and-planetary-sciences/pingo

Pingo-like features on Mars The size of this mound (ca. 100 m diameter) and cracking pattern seems similar to Terrestrial pingos. This mound is located at the bottom of an impact crater where an ideally developed artesian condition could occur, if groundwater is presence. Thus, if this is a pingo, it would be of the open system type.

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Three‐dimensional investigation of an open‐ and a closed‐system …

https://onlinelibrary.wiley.com/doi/10.1002/ppp.2115?af=R

13/05/2021  · University of Wuerzburg, Institute of Geography and Geology, Wuerzburg, Germany. Correspondence. … the shape and the location of the detected structures do not fit ideally to the general models. 66 Due to the morphological shape of the pingo, the massive ice core would be expected in a central position below the elevated surface. In contrast, the adjacent talik would be expected to be …

Growth of a young pingo in the Canadian Arctic observed by …

https://tc.copernicus.org/articles/10/799/2016/tc-10-799-2016.pdf

Growth of a young pingo in the Canadian Arctic observed by RADARSAT-2 interferometric satellite radar Sergey V … 2School of Environmental Studies, University of Victoria, Victoria, BC, Canada 3Northwest Territories Geological Survey, Government of the Northwest Territories, Yellowknife, NWT, Canada Correspondence to: Sergey V. Samsonov ([email protected] … If the water pressure drops …

Growth of pingo observed by RADARSAT-2 InSAR

https://tc.copernicus.org/preprints/9/6395/2015/tcd-9-6395-2015.pdf

initiate pingo growth. If the addition of water to this location exceeds the rate of down-ward freezing, then a pressurized, sub-pingo water lens forms and heaves the pingo 10 upward. Freezing of the pressurized water forms intrusive ice. If the water pressure drops due to escape of water through a hydraulic fracture or a change in the ground

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People Also Ask – pingo uni due login

Who is the creator of the Pingo system?

Please enter the access number: PINGO Help Intro video Info PINGO Info-Website Blog Facebook Legal Imprint Privacy policy (German) University of Paderborn [email protected] PINGO is an open-source class room system, made by the University of Paderborn.

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Where does a pingo form in a open system?

Northwest Territory, Canada. In an open system, a pingo forms as a result of artesian pressure induced from locally higher topographies. Open system pingos commonly occur at the base of a hillslope where hydraulic pressures are high, allowing the groundwater to inject into the pingo.

How does the degradation of a pingo occur?

Pingo degradation is normally initiated by the development of radial dilation cracks and concentric cracks caused by tensional stresses arising from bending and extension of the frozen overburden during pingo growth (Figures 4 and 6; Mackay, 1988 ).

How did the name Pingo get its name?

However, it was in 1938 that the term pingo was first borrowed from the Inuvialuit by the Arctic botanist Alf Erling Porsild in his paper on Earth mounds of the western Arctic coast of Canada and Alaska. Porsild Pingo in Tuktoyaktuk is named in his honour.

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