On the public citation graph
Seasonal growth bands in pingo ice
0 signed · 73 inferred · view as graph
Inferred edges come from two machine sources: sweeps of open repository metadata (mostly SSRN and Zenodo), and a bulk OpenAlex citation snapshot. Every row below is labelled with the one it came from. Neither is a complete citation index — absence here is not evidence of absence.
Is this your work? Sign in with ORCID and put your name on the
claims that are yours.
Reference health. See whether every reference in this work resolves to a
known work and none has been retracted — and get a dated CiteStamped
badge you can embed.
What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1007/bf00861063openalex-snapshot
Distribution of dissolved gas in water and bubbles in ice upon movement of a crystallization front
inferredcites →https://doi.org/10.1016/0022-0248(86)90114-4openalex-snapshot
Orientation textures in ice sheets of quietly frozen lakes
inferredcites →https://doi.org/10.1017/s0022143000006249openalex-snapshot
On the Isotopic Composition in δD and δ18O of Water and Ice During Freezing
inferredcites →https://doi.org/10.1017/s0022143000006547openalex-snapshot
δD – δ18O Relationships in Ice Formed by Subglacial Freezing: Paleoclimatic Implications
inferredcites →https://doi.org/10.1017/s0022143000006997openalex-snapshot
δD-δ18O Relationships and the Thermal History of Basal Ice Near the margins of two Glaciers in Lyngen, North Norway
inferredcites →https://doi.org/10.1017/s0022143000008911openalex-snapshot
Stable Isotopes and Debris in Basal Glacier Ice, South Georgia, Southern Ocean
inferredcites →https://doi.org/10.1017/s0022143000011771openalex-snapshot
Melting–Refreezing at the Glacier Sole and the Isotopic Composition of the Ice
inferredcites →https://doi.org/10.1017/s0022143000020967openalex-snapshot
Fabrics of Icing-Mound and Pingo Ice in Permafrost
inferredcites →https://doi.org/10.1017/s0022143000023248openalex-snapshot
Nucleation and Growth of Bubbles at an Ice–Water Interface
inferredcites →https://doi.org/10.1029/ar033p0131openalex-snapshot
Oxygen isotope ratios of antarctic permafrost and glacier ice
inferredcites →https://doi.org/10.1080/00040851.1985.12004451openalex-snapshot
Isotopic Evidence for Relic Pleistocene Glacier Ice on Victoria Island, Canadian Arctic Archipelago
inferredcites →https://doi.org/10.1139/e76-096openalex-snapshot
Pingo investigations, north-central Banks Island, Canadian Arctic
inferredcites →https://doi.org/10.1139/e77-023openalex-snapshot
Pulsating pingos, Tuktoyaktuk Peninsula, N.W.T.
inferredcites →https://doi.org/10.14430/arctic2324openalex-snapshot
Frost Blisters of the Bear Rock Spring Area near Fort Norman, N.W.T.
inferredcites →https://doi.org/10.21236/ada126334openalex-snapshot
Ice Growth on Post Pond, 1973-1982
inferredcites →https://doi.org/10.4095/126937openalex-snapshot
Quaternary Geology of the Tuktoyaktuk Coastlands, Northwest Territories
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.1002/esp.4302openalex-snapshot
Composition and origin of a lithalsa related to lake‐level recession and Holocene terrestrial emergence, Northwest Territories, Canada
inferred← citeshttps://doi.org/10.1002/ppp.1734openalex-snapshot
Internal Structure of a Lithalsa in the Akkol Valley, Russian Altai Mountains
inferred← citeshttps://doi.org/10.1002/ppp.1773openalex-snapshot
Groundwater Hydrology and Stable Isotope Analysis of an Open‐System Pingo in Northwestern Mongolia
inferred← citeshttps://doi.org/10.1002/ppp.2124openalex-snapshot
Pingo drilling reveals sodium–chloride‐dominated massive ice in Grøndalen, Spitsbergen
inferred← citeshttps://doi.org/10.1002/ppp.2261openalex-snapshot
Developments in Permafrost Science and Engineering in Response to Climate Warming in Circumpolar and High Mountain Regions, 2019–2024
inferred← citeshttps://doi.org/10.1002/ppp.3430040405openalex-snapshot
Notes on open‐system pingo ice, Adventdalen, Spitsbergen
inferred← citeshttps://doi.org/10.1002/ppp.3430060407openalex-snapshot
Observations on nearshore pingo growth, Adventdalen, Spitsbergen
inferred← citeshttps://doi.org/10.1002/ppp.455openalex-snapshot
Massive ground ice body of glacial origin at Yugorski Peninsula, arctic Russia
inferred← citeshttps://doi.org/10.1002/ppp.712openalex-snapshot
On the δ18O, δD and D‐excess relations in meteoric precipitation and during equilibrium freezing: theoretical approach and field examples
inferred← citeshttps://doi.org/10.1007/0-306-48051-4_17openalex-snapshot
The Effects of Global Warming on Mountain Regions: a Summary of the 1995 Report of the Intergovernmental Panel on Climate Change
inferred← citeshttps://doi.org/10.1016/0165-232x(95)00027-9openalex-snapshot
Electrical freezing potentials measured in a pingo growing in the western Canadian Arctic
inferred← citeshttps://doi.org/10.1016/b978-0-12-374739-6.00206-2openalex-snapshot
8.14 Ground Ice and Cryostratigraphy
inferred← citeshttps://doi.org/10.1016/b978-0-12-409548-9.12423-6openalex-snapshot
Permafrost Landscape Features
inferred← citeshttps://doi.org/10.1016/b978-0-12-818234-5.00126-7openalex-snapshot
Landforms of the Periglacial Environment: Pingos
inferred← citeshttps://doi.org/10.1016/b978-0-323-99931-1.00038-6openalex-snapshot
Frost mounds: Active and relict forms
inferred← citeshttps://doi.org/10.1016/j.catena.2025.109070openalex-snapshot
The surface features and internal structure of an integrated open system pingo in the source area of the Yangtze River on the Qinghai-Tibet Plateau
inferred← citeshttps://doi.org/10.1016/j.coldregions.2016.05.001openalex-snapshot
Stable isotopes in the closed-system Weather Pingo, Alaska and Pestsovoye Pingo, northwestern Siberia
inferred← citeshttps://doi.org/10.1016/j.geomorph.2022.108326openalex-snapshot
Distribution of pingos on Svalbard
inferred← citeshttps://doi.org/10.1016/j.icarus.2008.05.017openalex-snapshot
Distinguishing between vapor- and liquid-formed ground ice in the northern martian regolith and potential for biosignatures preserved in ice bodies
inferred← citeshttps://doi.org/10.1016/j.icarus.2012.06.003openalex-snapshot
Sub-kilometre (intra-crater) mounds in Utopia Planitia, Mars: character, occurrence and possible formation hypotheses
inferred← citeshttps://doi.org/10.1016/j.rcar.2026.10.001openalex-snapshot
Isotopic Signatures of Pingo and Palsa Ice Cores, Western Siberia: Implications for Formation Mechanisms
inferred← citeshttps://doi.org/10.1016/s1571-0866(03)01007-8openalex-snapshot
Permafrost process research in the United States since 1960
inferred← citeshttps://doi.org/10.1017/9781108552172.009openalex-snapshot
Essays: Inspiring Fieldwork
inferred← citeshttps://doi.org/10.1017/9781108552172.015openalex-snapshot
The Illisarvik Drained-Lake Field Experiment: a Legacy of J. Ross Mackay
inferred← citeshttps://doi.org/10.1017/s0954102020000619openalex-snapshot
Cryostratigraphy of mid-Miocene permafrost at Friis Hills, McMurdo Dry Valleys of Antarctica
inferred← citeshttps://doi.org/10.1017/s095410202100002xopenalex-snapshot
Cryostratigraphy of mid-Miocene permafrost at Friis Hills, McMurdo Dry Valleys of Antarctica – ERRATUM
inferred← citeshttps://doi.org/10.1029/163gm06openalex-snapshot
Satellite Remote Sensing of Permafrost and Seasonally Frozen Ground
inferred← citeshttps://doi.org/10.1029/2009je003398openalex-snapshot
Reconciling channel formation processes with the nature of elevated outflow systems at Ophir and Aurorae Plana, Mars
inferred← citeshttps://doi.org/10.1080/00291950510020600openalex-snapshot
Ground penetrating radar investigations of open system pingos, Adventdalen, Svalbard
inferred← citeshttps://doi.org/10.1080/24694452.2017.1314166openalex-snapshot
J. Ross Mackay, 1915–2014
inferred← citeshttps://doi.org/10.1111/sed.12537openalex-snapshot
Experimental soft‐sediment deformation caused by fluidization and intrusive ice melt in sand
inferred← citeshttps://doi.org/10.1134/s1028334x17020064openalex-snapshot
New data on variations of stable isotopes in the pingo ice core in the southern part of the Tazovsky Peninsula
inferred← citeshttps://doi.org/10.1134/s1028334x26600854openalex-snapshot
The First Evidence of Hydrogeological Transformation during the Formation of the Pingo Ice Core in the West Siberian Permafrost
inferred← citeshttps://doi.org/10.1139/e92-099openalex-snapshot
Massive ice of the Tuktoyaktuk area, western Arctic coast, Canada
inferred← citeshttps://doi.org/10.1177/030913339301700204openalex-snapshot
Issues in Canadian permafrost research
inferred← citeshttps://doi.org/10.1177/030913339802200301openalex-snapshot
Aspects of the genesis and geomorphology of pingos: perennial permafrost mounds
inferred← citeshttps://doi.org/10.15356/2076-6734-2018-4-507-523openalex-snapshot
Use of stable water isotopes to identify stages of the pingo ice core formation
inferred← citeshttps://doi.org/10.22215/etd/2018-12635openalex-snapshot
On characteristics and dynamics of water-rock glacier interactions in mountain areas (Western Italian Alps)
inferred← citeshttps://doi.org/10.22215/etd/2018-12697openalex-snapshot
Towards improved monitoring of changing permafrost by estimating soil characteristics from ground temperature time-series
inferred← citeshttps://doi.org/10.4157/grj.77.276openalex-snapshot
Present-Day Periglacial Environments in Central Spitsbergen, Svalbard
inferred← citeshttps://doi.org/10.5194/tc-10-799-2016openalex-snapshot
Growth of a young pingo in the Canadian Arctic observed by RADARSAT-2 interferometric satellite radar
inferred← citeshttps://doi.org/10.52381/icop2024.232.1openalex-snapshot
Intrusive origin of a 4.8 meter thick ground ice body within a polygonal peatland along the Inuvik-Tuktoyaktuk Highway, NWT
inferred← citeshttps://doi.org/10.70675/b5a45ad4z9b5az4c50zbd27z794dd6ea97deopenalex-snapshot
Influence of ice degradation on planetary landscapes
inferred← citeshttps://doi.org/10.7202/004847aropenalex-snapshot
Pingo Growth and collapse, Tuktoyaktuk Peninsula Area, Western Arctic Coast, Canada: a long-term field study
inferred← citeshttps://doi.org/10.7256/2453-8922.2025.2.74286openalex-snapshot
The concentration of major soluble ions in the ice core of the pingo at the Pestsovoye gas field, in the Evoyakha River valley of southern Tazovsky Peninsula, Northwestern Siberia
Editorial review for independent work. ICSAC — the Institute for Complexity
Science and Advanced Computing — runs a structured editorial panel for researchers
publishing outside journals, and publishes on CiteStamp rails. Submission is free
and goes through ORCID: icsacinstitute.org/submit.