FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4285388584> ?p ?o ?g. }

• W4285388584 endingPage "2792" @default.
• W4285388584 startingPage "2769" @default.
• W4285388584 abstract "Abstract. Rock glaciers are landforms related to permafrost creep that are sensitive to climate variability and change. Their spatial distribution and kinematic behaviour can be critical for managing water resources and geohazards in periglacial areas. Rock glaciers have been inventoried for decades worldwide, often without assessment of their kinematics. The availability of remote sensing data however makes the inclusion of kinematic information potentially feasible, but requires a common methodology in order to create homogeneous inventories. In this context, the International Permafrost Association (IPA) Action Group on rock glacier inventories and kinematics (2018–2023), with the support of the European Space Agency (ESA) Permafrost Climate Change Initiative (CCI) project, is defining standard guidelines for the inclusion of kinematic information within inventories. Here, we demonstrate the feasibility of applying common rules proposed by the Action Group in 11 regions worldwide. Spaceborne interferometric synthetic aperture radar (InSAR) was used to characterise identifiable moving areas related to rock glaciers, applying a manual and a semi-automated approach. Subsequently, these areas were used to assign kinematic information to rock glaciers in existing or newly compiled inventories. More than 5000 moving areas and more than 3600 rock glaciers were classified according to their kinematics. The method and the preliminary results were analysed. We identified drawbacks related to the intrinsic limitations of InSAR and to various applied strategies regarding the integration of non-moving rock glaciers in some investigated regions. This is the first internationally coordinated work that incorporates kinematic attributes within rock glacier inventories at a global scale. The results show the value of designing standardised inventorying procedures for periglacial geomorphology." @default.
• W4285388584 created "2022-07-14" @default.
• W4285388584 creator A5003563913 @default.
• W4285388584 creator A5006412580 @default.
• W4285388584 creator A5012660711 @default.
• W4285388584 creator A5016892222 @default.
• W4285388584 creator A5018150515 @default.
• W4285388584 creator A5021121825 @default.
• W4285388584 creator A5028676354 @default.
• W4285388584 creator A5034743566 @default.
• W4285388584 creator A5038503083 @default.
• W4285388584 creator A5042632167 @default.
• W4285388584 creator A5045376401 @default.
• W4285388584 creator A5046825713 @default.
• W4285388584 creator A5068645374 @default.
• W4285388584 creator A5072109365 @default.
• W4285388584 creator A5072209764 @default.
• W4285388584 creator A5077175130 @default.
• W4285388584 creator A5078768469 @default.
• W4285388584 creator A5083199921 @default.
• W4285388584 date "2022-07-14" @default.
• W4285388584 modified "2023-10-13" @default.
• W4285388584 title "Incorporating InSAR kinematics into rock glacier inventories: insights from 11 regions worldwide" @default.
• W4285388584 cites W126541936 @default.
• W4285388584 cites W1601896124 @default.
• W4285388584 cites W1606141550 @default.
• W4285388584 cites W1789935643 @default.
• W4285388584 cites W1895065985 @default.
• W4285388584 cites W1922445317 @default.
• W4285388584 cites W1950002147 @default.
• W4285388584 cites W1966053921 @default.
• W4285388584 cites W1994704913 @default.
• W4285388584 cites W1995652380 @default.
• W4285388584 cites W2016992419 @default.
• W4285388584 cites W2022402716 @default.
• W4285388584 cites W2047029664 @default.
• W4285388584 cites W2065989874 @default.
• W4285388584 cites W2070358034 @default.
• W4285388584 cites W2074762674 @default.
• W4285388584 cites W2079105346 @default.
• W4285388584 cites W2082663320 @default.
• W4285388584 cites W2099417215 @default.
• W4285388584 cites W2100359724 @default.
• W4285388584 cites W2102632939 @default.
• W4285388584 cites W2112200923 @default.
• W4285388584 cites W2118046132 @default.
• W4285388584 cites W2128261119 @default.
• W4285388584 cites W2139330078 @default.
• W4285388584 cites W2142505589 @default.
• W4285388584 cites W2143716001 @default.
• W4285388584 cites W2150310489 @default.
• W4285388584 cites W2150407424 @default.
• W4285388584 cites W2163351872 @default.
• W4285388584 cites W2166808849 @default.
• W4285388584 cites W2174009612 @default.
• W4285388584 cites W2192249243 @default.
• W4285388584 cites W2266207265 @default.
• W4285388584 cites W2278720811 @default.
• W4285388584 cites W2291532431 @default.
• W4285388584 cites W2302872967 @default.
• W4285388584 cites W2312546335 @default.
• W4285388584 cites W2329562006 @default.
• W4285388584 cites W2340673858 @default.
• W4285388584 cites W2409021404 @default.
• W4285388584 cites W2468284306 @default.
• W4285388584 cites W2474090142 @default.
• W4285388584 cites W2529854346 @default.
• W4285388584 cites W2542020478 @default.
• W4285388584 cites W2549856320 @default.
• W4285388584 cites W2616988067 @default.
• W4285388584 cites W2763671509 @default.
• W4285388584 cites W2766314745 @default.
• W4285388584 cites W2767362755 @default.
• W4285388584 cites W2774713322 @default.
• W4285388584 cites W2774752002 @default.
• W4285388584 cites W2787511792 @default.
• W4285388584 cites W2792995900 @default.
• W4285388584 cites W2807312034 @default.
• W4285388584 cites W2884220732 @default.
• W4285388584 cites W2885384010 @default.
• W4285388584 cites W2888670335 @default.
• W4285388584 cites W2895633339 @default.
• W4285388584 cites W2896704949 @default.
• W4285388584 cites W2909581233 @default.
• W4285388584 cites W2947561989 @default.
• W4285388584 cites W2949440094 @default.
• W4285388584 cites W2954163087 @default.
• W4285388584 cites W2963800186 @default.
• W4285388584 cites W2979546489 @default.
• W4285388584 cites W2982058479 @default.
• W4285388584 cites W3005241160 @default.
• W4285388584 cites W3008823460 @default.
• W4285388584 cites W3021715820 @default.
• W4285388584 cites W3031220429 @default.
• W4285388584 cites W3036448344 @default.
• W4285388584 cites W3061415658 @default.
• W4285388584 cites W3084408795 @default.
• W4285388584 cites W3108583344 @default.

• next