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Permafrost - Science topic

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Is there an index that integrates ground temperature, ground temperature change rate, active layer thickness, and active layer thickness change rate to comprehensively evaluate the thermal state and trend of permafrost over the years?
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The Permafrost Thermal State Index (PTSI) is a metric used to assess the thermal condition of permafrost, which is crucial for understanding climate change impacts in cold regions. While specific literature on PTSI is limited, several studies have examined permafrost thermal dynamics and related indices.
One notable study is "New high-resolution estimates of the permafrost thermal state and..." published in Earth System Science Data. This research provides novel datasets for the Northern Hemisphere, including predictions of mean annual ground temperature (MAGT), offering insights into permafrost thermal conditions. (https://essd.copernicus.org/articles/14/865/2022/)
Another relevant work is "Investigating the thermal state of permafrost with Bayesian inverse..." from The Cryosphere. This study analyzes trends in observed air and permafrost temperatures at multiple sites within the continuous permafrost zone, highlighting variations in permafrost temperature changes over time. ( )
Additionally, the International Permafrost Association (IPA) coordinated the Thermal State of Permafrost (TSP) project during the International Polar Year (IPY) 2007–2009. The project aimed to acquire standardized temperature measurements from permafrost regions globally, preparing a comprehensive dataset and developing maps of contemporary permafrost temperatures. (https://cmr.earthdata.nasa.gov/search/concepts/C1386206521-NSIDCV0.html)
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How to use matlab to model permafrost priority flow and predict permafrost degradation using the dual permeability model, lattice Boltzmann model or other numerical models of priority flow
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Dear friend Xuan Yangru
Modeling permafrost degradation under the action of preferential flow can be a complex process and requires a good understanding of the physics involved in the system. The dual permeability model and lattice Boltzmann models are commonly used to model preferential flow in permafrost. The following steps can be taken to consider the prediction of permafrost degradation under the action of preferential flow:
  1. Define the geometry of the permafrost system: This includes defining the size and shape of the permafrost region, and any other features that may impact the flow of water or heat through the system.
  2. Develop a numerical model: Using a numerical model, you can simulate the preferential flow of water through the permafrost. The dual permeability model or lattice Boltzmann models can be used to simulate the flow of water through the system. These models consider the different flow characteristics of the soil matrix and preferential flow channels.
  3. Input parameters: Input parameters such as temperature, water content, and soil properties are necessary to run the numerical model. These parameters can be obtained from field measurements or laboratory experiments.
  4. Run the model: After inputting the necessary parameters, you can run the numerical model and obtain results on how preferential flow impacts permafrost degradation.
  5. Analyze results: Analyze the results obtained from the model to understand the impact of preferential flow on permafrost degradation. This information can be used to better understand the system and develop strategies to mitigate permafrost degradation.
Matlab is a powerful tool that can be used for numerical modeling. It has various built-in functions and toolboxes that can be used to model permafrost degradation. Some toolboxes that can be used for this purpose include the Partial Differential Equation Toolbox, the Optimization Toolbox, and the Image Processing Toolbox.
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During the thawing of the subpolar permafrost, triggered by accelerating global warming, could viruses and bacteria from many thousands of years ago, which are dangerous to humans, emerge and cause another pandemic?
The thawing of permafrost, which has been present for thousands and millions of years in areas near the Arctic Circle, mainly in the Arctic, caused by the accelerating process of global warming, will result in the release into the atmosphere of thousands and possibly millions of tonnes of hitherto frozen methane, a gas that is many times more greenhouse-generating than CO2, which will result in a significant acceleration of the already rapid process of global warming. However, this is not the only very dangerous effect for human civilisation and for the state of the planet's biosphere of the progressing process of global warming, a process which has been taking place since the first industrial revolution, i.e. since the 18th century. Among the significant negative consequences of the increasingly rapid global warming process triggered by the industrial revolution based on the dirty energy of burning fossil fuels is the increase in the risk of a future pandemic caused by viruses emerging from the thawing of the permafrost in areas near the planet's Arctic Circle. These viruses emerged and were frozen many thousands and perhaps millions of years ago, i.e. when there was not yet a modern species of homo sapiens on planet Earth. Therefore, humans may not be immune at all to these strains of different types of viruses that functioned on the planet many thousands of years ago. In addition, the existence of many species of both wild animals and farmed livestock may also be threatened if thawing viruses from many thousands of years ago prove to be completely unfamiliar to the immune systems of said animals. According to CNN media reports, there are virological research laboratories currently working on revived viruses taken from thawing permafrost. These revived viruses are referred to in the media as "zombie viruses". In addition, high summer temperatures have thawed the corpses of people who died and were buried in cemeteries many years ago, as well as animals, from whose thawing bodies pathogenic strains of viruses and bacteria have emerged. The thawing of the permafrost in recent years, for example, has been identified as a major source factor in the occurrence of the anthrax epidemic in Siberia, because the high temperatures experienced in Siberia for the first time in many thousands of years allow viruses and bacteria to be released from human cemeteries and animal corpses, i.e. micro-organisms that functioned thousands of years ago and which may be particularly dangerous to humans and animals living on the planet today.
In view of the above, I address the following question to the esteemed community of scientists and researchers:
In the course of the rapid thawing of the sub-polar permafrost, caused by the progressive process of global warming, could viruses and bacteria from many thousands of years ago, which are dangerous to humans, come to light and cause another pandemic?
What is your opinion on this subject?
Please respond,
I invite you all to discuss,
Thank you very much,
Best regards,
Dariusz Prokopowicz
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Dariusz Prokopowicz There are many recent works published for this subject. The risk was always present, but now it will be more significant.
Wu, Ruonan, Gareth Trubl, Neslihan Taş, and Janet K. Jansson. "Permafrost as a potential pathogen reservoir." One Earth 5, no. 4 (2022): 351-360.
Alempic, J.M., Lartigue, A., Goncharov, A.E., Grosse, G., Strauss, J., Tikhonov, A.N., Fedorov, A.N., Poirot, O., Legendre, M., Santini, S. and Abergel, C., 2023. An Update on Eukaryotic Viruses Revived from Ancient Permafrost. Viruses, 15(2), p.564.
Christie, Alec. "Blast from the Past: Pathogen Release from Thawing Permafrost could lead to Future Pandemics." (2021).
Hueffer, K., Drown, D., Romanovsky, V., & Hennessy, T. (2020). Factors contributing to anthrax outbreaks in the circumpolar north. EcoHealth, 17, 174-180.
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Hello, collegues,
I'm trying to estimate the distribution of a certain kind of microorganism (eg Methanobacterium) in a certain environment (permafrost) from metagenomic data presented on various online services (NCBI, MG-RAST, https://microbeatlas.org). Such an analysis can be done on MG-RAST, but data are scarce. The service https://microbeatlas.org gives good data, but they do not correspond to the entire genus, but only to selected reference genomes. The situation is complicated by the fact that my computer is not very powerful and I cannot download 10,000 metagenomes and analyze them myself. Can you please tell me if it is possible to carry out such an analysis online, at least partially, with post-processing on a computer?
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Hello Vladimir,
I agree with Dr. Abhijeet. Working with 10000 genomes requires a lot of planning and very powerful servers.
However for smaller and more modest projects you could try working with cyverse servers, or with usegalaxy servers.
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Dear colleagues and esteemed professors,
While searching global permafrost distribution I have come across several terms, which are synonymous and confusing.
It would be awesome to know the differences between; Permafrost Region, Permafrost Zone and Permafrost Area.
While going through the topic myself, I have come across some remarkable commentary (Obu, 2021) and articles (Zhang et al., 1999 and 2000; Gruber, 2012). Still, I would appreciate knowing the difference from the experts themselves.
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Dear Sir, Thanks for the clarification sir.
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This kind of bedform occurs in the Gulf of Mexico, Where the water depth varies from about 500m to 2000m, I'm not sure if there's methane or other gases in the ground here, or if there's a permafrost.
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Hongxin Bai I think the interaction between a flow and cohesion less sediment on a bed is the cause of bed form formation.
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Dear colleagues,
I have a CT scan of a permafrost core. I assume that this core consists of air, ice, organic and mineral parts. I have threshold values for all constituents.
I need to build a 3D model and I want to define the threshold range for each constituent (i.e. let's say air's threshold values are from 0 to 80, ice from 81 to 150, organic from 151 to 190 and mineral from 191 to 255). I have several cores and threshold values are different for them.
On the screenshot, you can see the desired result.
It is possible to do it with Avizo but at the moment I don't have a license and it is quite expensive.
Is there any free alternative that I may use?
I already tried the ITK Python package and Huygens Professional and also several other programs but unfortunately, I did not reach my goal.
Update: another satisfying result can be four different images for each constituent respectively.
Thank you.
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Dear Reuben Reyes thank you for your comment, I must say that even the first sentence was already super helpful. I started to look for available volume rendering software.
I especially liked 3D Slicer. Using it I was able to visualize my core.
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While I'm working on a project about landslides on the Tibet Plateau, I encountered many large and valley-filling deposits that seem to be some kind of mass movement but cannot find their source areas.
The phenomenon is usually observed at 4000 - 5000 m elevation and many areas have permafrost. I attached two screenshots to show one of them which dammed the river (the only one that dammed river in the region). Many other cases can be seen around this area in the google earth kmz file.
I was told it might be slow sliding caused by underlain ice melt or remaining glacier tills. Can someone who has working experience in high-elevation areas identify what kind of phenomenon is it?
Thanks in advance
Chenxiao Tang
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This type of very old landslides (undated) / rock slides / glacier avalanches are also present in Hunza valley along Hunza river in Central Karakoram north Pakistan.
Regards
Ijaz
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What is the impact on lake ecology with permafrost thawing in Qinghai-Tibet Plateau ?
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See also a general discussion on permofrost elsewhere:
In my opinion, there is no need for a change of this zonal soil type with has a morphoclimatic component similar to other exogenic features, e.g., laterite or many duricrusts. It exists in a glacial to periglacial climate zone to a depth as much as 200 m with a shallow zone of as many as 4 to 5 meters deep affected by thawing processes. It is characterized by cryoturbation (pattern grounds), solifluction on gently dipping slopes and contains water/ H2O as its stabilizing pore-filling agent. Even if climatic changes may be conducive to a degradation or erosive disappearance and H2O is changing its physical state from solid to liquid, the well-defined character of it does not change along with that; there is no need for a re-definition it may alter into a relic or paleosol as many other pedological features subjected to climatic alteration and erosive/ sedimentological processes. It is the fate of surface features on the Earth to be under constant physical reworking/ redeposition and chemical modification as a consequence of morpho-climatic processes and should not succumb to mainstream political and medial influences.
Geoscientists think in different temporal and regional scales.
With kind regards H.G.Dill
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While working in the Subarctic of Western Siberia, we noticed that in places of active thermokarst the biological productivity of vegetation increases. Plants that are absent in nearby ecosystems with stable permafrost grow in thermokarst-affected ecosystems. Thermokarst is usually associated with human influence. What are the typical responses of productivity and biodiversity to the effects of thermokarst in your research area? Why does thermokarst increase vegetation productivity? Is this a thermal effect? Is this the effect of increasing soil fertility? Is this the effect of reducing competition from indigenous zonal flora? Or is it a complex of the listed reasons?
I am attaching a photograph of the community on the thermokarst slope and a photograph of a typical tundra (latitude N70 °).
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I am trying to calculate the LST of three land types existing in permafrost regions of NWT, I am using Landsat-8.
Is the thermal imagery of Landsat-8 a good source for deriving LST of a local scale?
And,
I was wondering,
which time of year is the best time for this process?
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It would be a good idea to compare the interpretations based on different seasons of the year. Winter would give you an idea of where areas with limited snow cover occur, and so the ground is likely to be very cold. Areas with large amounts of snow would be possible areas of discontinuous permafrost or where if might be absent. In summer, the topography would give you a good idea of where palsas/lithalsas might be present and the vegetation tell you where peat plateaus may occur. Look up the appearance of these on aerial photography. Do not forget to carry out a thorough literature search and incorporate the results of prior field studies by others to guide your interpretations. Otherwise you my end up clashing with the results of good field and laboratory studies. Check with the appropriate Territorial government bodies who carry out these studies as well as the GSC. Also check your interpretations against the available climate data, especially mean annual freezing and thawing indices based on seasons.
Stuart.
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There are many contaminated sites around the circumpolar Arctic, from DEW line sites to a variety of other historic hazardous waste, municipal waste, and mixed dumping sites. I am interested in any publications or data that could shed light on whether and how contaminated sites are changing as a result of permafrost thaw. Permafrost is often assumed to be an effective barrier to the spread of contamination from such sites, but thawing is likely to change this and may already be having effects on the containment of contaminants, particularly in coastal areas or other areas that are experiencing slumping or erosion. The effects may be highly site-specific but any information on particular sites or wider analysis of potential trends related to this question would be greatly appreciated. Thank you!
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I found the following pertaining to your query:
Subsidence risk from thawing permafrost
Analysis of flooding effects on a landfill permafrost containment system
Rethinking Landfill Development and Operation in Permafrost Regions ( Please note that you'll have to pay or request access for this one)
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Hi all,
I'm looking for climate change projection data in raster format. Something like is shown in the IPCC 5th report chapter 12.
In particular I'm interested in the Arctic, temperature, precipitation and permafrost. I've had a look at the IPCC data centre and a couple of other online data portals, but without much joy.
Does anyone have any suggestions?
Cheers,
Matt
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Dear Matthew,
The raster format is pretty uncommon in the meteorological and climate community. They usually use either GRIB (common among meteorological centers) or NetCDF (popular in climate science) for there vast data sets.
Therefore you may have to get the data in NetCDF and convert the data into an appropriate format (wouldn't tiff also work?). Maybe your data analysis tool might even import NetCDF?
Good luck
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Dear friends. Your theme is very interesting. We are engaged in mapping research topics based on methods of text analysis. Although we do not understand anything in the climate, we decided to map one of the directions of your research. Usually this is about a dozen articles with basic information on the topic, about a dozen articles potentially with novelty, subtopics and terms. We limited ourselves to the latter, because the number of articles is not enough, in the hope that this will be useful for one of you. We invite to intellectual cooperation: each of you can send initial data on any topic and will receive a map in return. We really appreciate the feedback and accumulate the experience of analyzing the research topics.
Results are in the topic_report.doc file. The analysis is performed using the Web of Science. Depending on the request of the scientist, we also apply scopus.com and the patent lens.org database. We look forward to collaborating.
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pl look after self organizing maps . there is a chance of getting clue.
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I could not see that file become attached in previous question
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Hi! IIn my recent monographs ("Global hydrology" and " Global changes in the river runoff" - both available on my page within ResearchGate free here, on my page within Research Gate, I give global forecasts of changes in the river runof for the 21th century, including Lena, Kolyma, Yenissey etc. and their basins. Anomalies of the river runoff changes within "Prilenskoe plato" are also examined.
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Dear Researchers,
I would like to ask that between Water Flow and Balance Simulation Model (WaSiM) and Cold Regions Hydrological Model (CRHM) which is good model in permafrost hydrology prespectve. I have to choose anyone between these two models. I am confused and not yet finally decided.
Expert opinion is highly appriciated and valuable.
Thanks in anticipation.
Regards
Naveed.
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Hi Marcos,
First of all thanks for your detailed comment.
I have contacted with the developers of CRHM and they have provided me required information which was very helpful for me to select the most appropriate model for my research scope. As long as concern about my research work, i will mainly focus on the runoff generations under changing climate from the permafrost zones due to dynamics of the Active Layer Thickness (ALT). The CRHM is better to use in the cold environments have mainly covered with snow and CRHM is applicable to the tundra or other like this environments found in Arctic, Canada and Alaska's regions.
WaSiM model simulate the dynamics of the active layer thickness more better as compared to CRHM and also gave three dimentional variations in the soil temperatures.
Therefore after review some articles and some other literature, I finally selected WaSiM. I can use CRHM if I found that I have enough time to simulate using it as well. By comparing both the model's results, I will conclude the application efficiency as well as I will be able to write some good articles.
Thanks a lot for you precios time and detailed comment.
Regards
Naveed.
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Hello Everyone,
I want to use VIC model for permafrost regions to simulate runoff under changing climatic and vegetation cover. Any guide / information may be very supportive and helpful for me. So please share if you have any kind of support / guide /help etc.
Regards
Naveed
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Interested
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Hi,
Anybody used Variable Inflitration Capacity Model (VIC) Model?
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its very interesting. have a look at attached file.
best regards
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I want to know that SWAT model can be used permaforst hydrology (focusing on surface water flow and ground water recharge) under changing climate and vegetation cover.
If yes, then what are the controling factors / parameters which shows the permafrost conditions in SWAT Model?
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Please find attached the SI of this paper including S1, S2, S3 and S4.
Regards,
Martijn
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For my research work, I want to know which model is best for permaforst hydrology (focusing on surface water flow and ground water recharge) under changing climate and vegetation cover.
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Dear Abrar,
I am using WEAP Model since last 5 years and also delivered many lecturers and trainings. It is almost impossible to use WEAP-SWAT-Hydrus 2D combination and also not fulfill the required targets as per my knowledge. If you have any idea, welcome to share.
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The conditions required for the formation of natural gas hydrates occur frequently on the Earth’s continental margins (apart from a smart fraction associated with the Artic Permafrost): - Is there any specific reason associated with these kind of occurrence?
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Depth (isolation and pressure), volcanic activities (quick temperature changes and released materials), and seismic activities (releasing liquid from different layers) are all common on the Earth's continental margins. These phenomena and the caused changes can result in the accumulation of gas hydrates in a long period.
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I recently read an article about the melting of permafrost soils that have been frozen for thousands of years, and as they melt, they are releasing ancient viruses and bacteria that seem to be springing back to life. For example, in August 2016, in the Yamal Peninsula, a 12-year-old boy died and at least twenty people were hospitalized after being infected by anthrax. It was assumed that a reindeer infected with anthrax died 75 years ago and its frozen carcass became trapped under permafrost. Many other diseases are also found to have been released due of this, and they are multiplying. I am concerned about what great impact this could have on the human population, and if there are ways this could be controlled or prevented. 
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Microbes have existed for billions of years because they mutate, reorganize and adapt to specific and supporting environments. Microbes in permafrost remain inactive as long as possible and could be revived under appropriate supporting environment and conditions. Human interactions (inter-regional and geotransfer of wildlife and domesticated animals) may facilitate or encapsulate transfer to populations.
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I’m wondering if you know catchment hydrological models that simulate hydrological response of watersheds located in permafrost or freezing soil areas with taking into account the soil freezing and thawing dynamics ?
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Thank you for your valuable comments.
In fact, concerning Canada, the university of Saskatchewan has developed the CRHM model to conduct such simulations. Also, the U.S. Army Corps of Engineers model GSSHA could be used. But, I'm curious to know the other models that could be used for this kind of studies.
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3 out of 4 extinction events were caused by a build-up of methane hydrates in the atmosphere.  We are seeing an increase of methane with the melting of permafrost.  With the continued increase of warming and the admission by climate scientists that the warming event is accelerating this should be a huge concern.
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Karyl,
You say three out of four extinctions were caused by methane hydrates. Could you itemise them, please. As far as I know only the PETM event has been blamed on methane hydrates, and now the cause is thought to be the up welling during the opening of the Atlantic Ocean which cooked the fossil fuel deposits.
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Class 1 hydrates are considered as the best type of hydrates compared to Class 2 and Class 3 hydrates as energy source. Above free gas section of Class 1 hydrate, hydrate section might contain hydrate+free water (Class 1W) or hydrate+free gas (Class 1G). According to the result of the modelling studies, Class 1G is preferred compared to Class 1W. My question is that in nature which type is common, whether Class 1G or Class 1W? I could not obtain any articles or reference about it. Just I know Messoyakha field (permafrost) in Russia is Class 1G type.
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Gas Hydrates: Immense Energy Potential and Environmental Challenges
By Carlo Giavarini, Keith Hester
Go through this google book; if it is helpful. I think Class 1G is common.
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I want to date gas emitted from soil (permafrost) and determine where this carbon comes from (what depth).
From what I saw in the literature, the only way to do this is to do incubations and then link the results with the field values. 
Are there other ways?
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I don't know the answer, but this seems like a challenging question because the gases emitted to the atmosphere are presumably produced at multiple depths. It seems that one approach would be to measure the age of CO2/CH4 that are produced at various depths, the rate of CO2/CH4 production at those depths, and then do some modeling of vertical gas transport through the soil. Then you could figure out the sources of the CO2 and CH4 at any depth throughout the soil column, including at the soil surface.
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I only know the paper of Boereboom et al. (2013) in The Cryosphere but I am sure there is more (unpublished?) data available.
Thanks
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Hi Daniel. Thank you, I will contact you shortly! Cheers, Thomas
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I am looking for alternative methods for the preservation of permafrost, especially in ice-rich discontinuous regions. I have reviewed the studies for woods chips, however, I am looking for results of different materials (i.e., geotextiles, vegetation mats, sod, etc.) or new technologies. I appreciate any direction or research that can will be cited.
Thanks!
Michelle
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By no means a scientific answer but one of observation coming from a cold climate , plain old ordinary saw dust seems to be one of the best mechanisms to maintain a permafrost situation .  I have no data but have experienced it first hand , as a side note when old time ice saving techniques were used in the northern US and all of Canada sawdust was the choice insulation so much so that it ice was packed onto to ships and surrounded by sawdust and sent to the Caribbean islands fully intact
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Papers, references, databases? Quaternary deposits of Beringia region (from Taymir to Alaska) are interest for me....
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We have ground ice content (intrasedimental + ice wedge + buried ice) for Canadian Arctic, Yukon, Nunavik and Alaska. Have a look at the papers + scientific report on my profile.
PS: several papers to come (09-2015) with tota ground ice for the Canadian Pmf conference.
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Current research suggests the possible existence of sporadic permafrost in relation to several buried ice patches of Picos de Europa, with mean annual temperatures close to 0ºC in the debris that cover these relict ice bodies. But so far it has not been demostrated to 100%.
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BTS  measuremets, ground temperatures monitoring at different depths at least 2 years, conducting geophysical investigations (Electrical Resistivity Tomography, GPR).
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For my study I have six different DEMs of a glacier. The DEMs are all from different years and I want to calculate the volume changes over a timeperiod. Including the six DEMs I have one subglacial DEM with low resolution (100 meter). In ArcMap, I use raster calculator to subtract the DEMs from the subglacial DEMs to get the volume results. The problem is that the DEMs with high resolution gets converted to 100 meter resolution. Is there any way to derive results with better resolution? 
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Another thought I have.
Do you roughly know the thickness of the ice sheet? And how rough is the subglacial DEM and the surface of the ice?
Maybe it would be useful to take the 3D surface into account. There are tools available in ArcMap (or extensions) to calculate first the surface of each cell based on the topography. During the volume calculation you multiply then the surface of the cell by the thickness of the ice instead of using 100x100m. 
This approach could be more accurate depending of the terrain roughness and the relation between thickness and cell size.
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I am working on a white paper for buried chilled pipelines in discontinuous permafrost. Topics that are covered are frost bulb, thermokarst, slope instability, thaw settlement, subsidence, permafrost disturbance in right-a-way, reclamation, and revegetation strategies. In addition, lessons learned and BPM for trenching methodologies. I appreciate any assistance!
Thanks!
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Cold Regions Research and Engineering Laboratory in Hanover is good. Maybe this report will help:
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I have had some luck with the USPTO database searching on "permafrost" but that will not lead, I think, to ship/boats/ etc. technologies.  I think what I really need is to know what the classification numbers might be.  Looked at the 2013 WIPO Indicators publication. I have not gone looking via the Intl Maritime Organization.
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Yes, the broad ways that something could be ice capable was the problem when I looked at the database.  Ice capable fixed structures in the Arctic would be a good category, but that, too, is a giant set of potential technologies.  I'm working on a little paper where I've taken 5 'factors' that two energy experts used in a 2009 article to assess how likely it is the Arctic will get exploited as environmental change moves along. I'm looking at whether any of the factors are further along now than then. I thought the article's factors were general enough to cover lots in the Arctic and they were not specific to energy production.  New technologies might also prove useful for adapting things for those who live there all the time.  Stands to reason that technological adaptation to change would grow fast there.  But it is hard to show that. Any suggestion are welcome.  I have a former student who works North Slope, he's a field engineer.  He's trying to help me think about it, too.  But, I see you have a lot on this.  I'm not an engineer.  Any suggestions would be welcome.
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We are looking for convective heat transfer coefficient values to compare with our field experimental results
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There is a phase change for ice melting as well as the force convection in the flowing water. If the ice surface is rough, and/or has some holes, it will be more complex. There is an review paper you might be interested in:
"Melting and Freezing" L.S. Yao ,J. Prusa "Advances in Heat Transfer, Volume 19, 1989, Pages 1–95
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I'm looking for convective heat transfer coefficient that were derived from experiments involving heat advection by flowing water over ice or permafrost.
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The followin literature may be useful for your research
Ref: Efffect of ice surface orientation on intensity of water-ice heat transfer under free convection condtions
E.S.Gogolev and A.N. Krasavin
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Unfrozen water effects.
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I meant methane gas hydrates. Thus the topics can be added: methane, Arctic Ocean.