Suffusion: Terminology and Phenomenology

Khomenko, V. M.; Moscow, Niu Mgsu

doi:10.22227/978-5-7264-1933-6.2019.6-15

Cited by 1 publication

(2 citation statements)

References 2 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…Suffusion is an internal erosion process that occurs when finer soil particles detach due to seepage flow and start moving within the pore space of larger particles [43,44]. Geomorphologically, suffusion is involved in the formation of various subsidence landforms.…”

Section: Climate Change and Changes In The Suffusion (Internal Erosion)mentioning

confidence: 99%

“…Internal erosion is a phenomenon that has not been studied enough [44,45]. Internal erosion has been noted in Salekhard city and near the coast in the Marresale weather station in the YaNAO, and an estimation of suffusion risk was made for the Sabetta area (eastern coast of Yamal Peninsula).…”

Section: Climate Change and Changes In The Suffusion (Internal Erosion)mentioning

confidence: 99%

See 1 more Smart Citation

A Spatially Detailed Projection of Environmental Conditions in the Arctic Initiated by Climate Change

et al. 2023

View full text Add to dashboard Cite

The environmental conditions of the Arctic are vulnerable to the effects of climate change. We focus on the territory of the Yamalo-Nenets Autonomous Okrug (YaNAO). The objective of this study is to project mid-21st century climate-driven changes in the state of climate and the natural environment in the YaNAO. For this purpose, the CMIP6 data models with the climate change scenario SSP5-8.5 were used. Climate change directly affects the statistics of extreme events and climatically driven phenomena, such as frosts and thaws, as well as avalanches and slush flows. Climate change causes changes in the Arctic environment, primarily due to permafrost degradation, leading to important modifications in events such as mudflows, cryogenic landslides, abrasion, erosion, suffusion, frost heave, solifluction, thermokarst, and others. In some cases, the intensity and area of these processes increase, such as heaving processes and thermokarst becoming more active by 2050. In other cases, the solifluction processes decrease in the south part of the YaNAO due to the discontinuous or sporadic permafrost distribution. Projected climatic changes will inevitably lead to the restructuring of the geosystems in YaNAO, creating risks for infrastructure in economically active territories.

show abstract

Section: Climate Change and Changes In The Suffusion (Internal Erosion)mentioning

confidence: 99%

Section: Climate Change and Changes In The Suffusion (Internal Erosion)mentioning

confidence: 99%

A Spatially Detailed Projection of Environmental Conditions in the Arctic Initiated by Climate Change

et al. 2023

View full text Add to dashboard Cite

show abstract

Suffusion: Terminology and Phenomenology

Cited by 1 publication

References 2 publications

A Spatially Detailed Projection of Environmental Conditions in the Arctic Initiated by Climate Change

A Spatially Detailed Projection of Environmental Conditions in the Arctic Initiated by Climate Change

Contact Info

Product

Resources

About