FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2602410306> ?p ?o ?g. }

• W2602410306 abstract "Permafrost regions have been identified to host a soil organic carbon (C) pool of global importance, storing more than 1500 PgC. A large portion of this C pool is currently frozen in deep soils and permafrost deposits. Permafrost thaw hence may result in mobilization of large amounts of C as greenhouse gases, dissolved organic C, or particulate organic matter, with substantial impacts on C cycling and C pool distribution. Understanding potential consequences and feedbacks of permafrost degradation therefore requires better quantification of processes and landforms related to thaw. While many predictive land surface models so far consider a gradual increase in the average active layer thickness across the permafrost domain, rapid shifts in landscape topography and surface hydrology caused by thaw of ice-rich permafrost are much more difficult to project. Field studies of thermokarst and thermo-erosion indicate highly complex and rapid landscape-ecosystem feedbacks. Contrary to top-down permafrost thaw that may affect any permafrost type at the surface, both thermokarst and thermo-erosion are considered pulse disturbances that are closely linked to presence of near-surface ice-rich permafrost, are active on short sub-annual to decadal time scales, and may affect C stores tens of meters deep.Here we present a comprehensive review synthesizing measured and modeled rates of thermokarst and thermo-erosion processes from the scientific literature and own observations across the northern Hemisphere permafrost regions. The goal of our synthesis is (1) to provide an overview on the range of thermokarst and thermo-erosion rates that may be used for parameterization of thermokarst and thermo-erosion in ecosystem and landscape models; and (2) to assess simple back-of-the-envelope scenarios of the magnitude of C thaw due to thermokarst and thermo-erosion versus projected active layer thickening. Example scenarios considering thermokarst lake expansion and talik growth indicate that rapid thaw processes have a high possibility to contribute substantially to permafrost C mobilization over the coming century." @default.
• W2602410306 created "2017-04-07" @default.
• W2602410306 creator A5002062365 @default.
• W2602410306 creator A5006241333 @default.
• W2602410306 creator A5016083236 @default.
• W2602410306 creator A5021045182 @default.
• W2602410306 creator A5021212455 @default.
• W2602410306 creator A5036160087 @default.
• W2602410306 creator A5040494023 @default.
• W2602410306 creator A5040647242 @default.
• W2602410306 creator A5043824604 @default.
• W2602410306 creator A5045007233 @default.
• W2602410306 creator A5045565461 @default.
• W2602410306 creator A5046520181 @default.
• W2602410306 creator A5048116619 @default.
• W2602410306 creator A5049458763 @default.
• W2602410306 creator A5049920825 @default.
• W2602410306 creator A5052769176 @default.
• W2602410306 creator A5053492826 @default.
• W2602410306 creator A5071464620 @default.
• W2602410306 creator A5071653812 @default.
• W2602410306 creator A5072303385 @default.
• W2602410306 creator A5077504737 @default.
• W2602410306 creator A5078716623 @default.
• W2602410306 creator A5078777449 @default.
• W2602410306 creator A5081906243 @default.
• W2602410306 creator A5085085011 @default.
• W2602410306 date "2016-12-15" @default.
• W2602410306 modified "2023-09-23" @default.
• W2602410306 title "A synthesis of thermokarst and thermo-erosion rates in northern permafrost regions" @default.
• W2602410306 hasPublicationYear "2016" @default.
• W2602410306 type Work @default.
• W2602410306 sameAs 2602410306 @default.
• W2602410306 citedByCount "0" @default.
• W2602410306 crossrefType "journal-article" @default.
• W2602410306 hasAuthorship W2602410306A5002062365 @default.
• W2602410306 hasAuthorship W2602410306A5006241333 @default.
• W2602410306 hasAuthorship W2602410306A5016083236 @default.
• W2602410306 hasAuthorship W2602410306A5021045182 @default.
• W2602410306 hasAuthorship W2602410306A5021212455 @default.
• W2602410306 hasAuthorship W2602410306A5036160087 @default.
• W2602410306 hasAuthorship W2602410306A5040494023 @default.
• W2602410306 hasAuthorship W2602410306A5040647242 @default.
• W2602410306 hasAuthorship W2602410306A5043824604 @default.
• W2602410306 hasAuthorship W2602410306A5045007233 @default.
• W2602410306 hasAuthorship W2602410306A5045565461 @default.
• W2602410306 hasAuthorship W2602410306A5046520181 @default.
• W2602410306 hasAuthorship W2602410306A5048116619 @default.
• W2602410306 hasAuthorship W2602410306A5049458763 @default.
• W2602410306 hasAuthorship W2602410306A5049920825 @default.
• W2602410306 hasAuthorship W2602410306A5052769176 @default.
• W2602410306 hasAuthorship W2602410306A5053492826 @default.
• W2602410306 hasAuthorship W2602410306A5071464620 @default.
• W2602410306 hasAuthorship W2602410306A5071653812 @default.
• W2602410306 hasAuthorship W2602410306A5072303385 @default.
• W2602410306 hasAuthorship W2602410306A5077504737 @default.
• W2602410306 hasAuthorship W2602410306A5078716623 @default.
• W2602410306 hasAuthorship W2602410306A5078777449 @default.
• W2602410306 hasAuthorship W2602410306A5081906243 @default.
• W2602410306 hasAuthorship W2602410306A5085085011 @default.
• W2602410306 hasConcept C100970517 @default.
• W2602410306 hasConcept C111368507 @default.
• W2602410306 hasConcept C114793014 @default.
• W2602410306 hasConcept C123157820 @default.
• W2602410306 hasConcept C127313418 @default.
• W2602410306 hasConcept C15098985 @default.
• W2602410306 hasConcept C159390177 @default.
• W2602410306 hasConcept C159750122 @default.
• W2602410306 hasConcept C178790620 @default.
• W2602410306 hasConcept C185592680 @default.
• W2602410306 hasConcept C187320778 @default.
• W2602410306 hasConcept C1965285 @default.
• W2602410306 hasConcept C205649164 @default.
• W2602410306 hasConcept C2776026197 @default.
• W2602410306 hasConcept C2779227376 @default.
• W2602410306 hasConcept C2780155556 @default.
• W2602410306 hasConcept C39432304 @default.
• W2602410306 hasConcept C39464130 @default.
• W2602410306 hasConcept C76886044 @default.
• W2602410306 hasConcept C87359718 @default.
• W2602410306 hasConceptScore W2602410306C100970517 @default.
• W2602410306 hasConceptScore W2602410306C111368507 @default.
• W2602410306 hasConceptScore W2602410306C114793014 @default.
• W2602410306 hasConceptScore W2602410306C123157820 @default.
• W2602410306 hasConceptScore W2602410306C127313418 @default.
• W2602410306 hasConceptScore W2602410306C15098985 @default.
• W2602410306 hasConceptScore W2602410306C159390177 @default.
• W2602410306 hasConceptScore W2602410306C159750122 @default.
• W2602410306 hasConceptScore W2602410306C178790620 @default.
• W2602410306 hasConceptScore W2602410306C185592680 @default.
• W2602410306 hasConceptScore W2602410306C187320778 @default.
• W2602410306 hasConceptScore W2602410306C1965285 @default.
• W2602410306 hasConceptScore W2602410306C205649164 @default.
• W2602410306 hasConceptScore W2602410306C2776026197 @default.
• W2602410306 hasConceptScore W2602410306C2779227376 @default.
• W2602410306 hasConceptScore W2602410306C2780155556 @default.
• W2602410306 hasConceptScore W2602410306C39432304 @default.
• W2602410306 hasConceptScore W2602410306C39464130 @default.
• W2602410306 hasConceptScore W2602410306C76886044 @default.
• W2602410306 hasConceptScore W2602410306C87359718 @default.

• next