[HTML][HTML] Deglaciation of the Eurasian ice sheet complex
The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Glacial geomorphological mapping: A review of approaches and frameworks for best practice
Geomorphological mapping is a well-established method for examining earth surface
processes and landscape evolution in a range of environmental contexts. In glacial …
processes and landscape evolution in a range of environmental contexts. In glacial …
[HTML][HTML] Late Quaternary dynamics of Arctic biota from ancient environmental genomics
During the last glacial–interglacial cycle, Arctic biotas experienced substantial climatic
changes, yet the nature, extent and rate of their responses are not fully understood …
changes, yet the nature, extent and rate of their responses are not fully understood …
[HTML][HTML] CHELSA-TraCE21k–high-resolution (1 km) downscaled transient temperature and precipitation data since the Last Glacial Maximum
High-resolution, downscaled climate model data are used in a wide variety of applications
across environmental sciences. Here we introduce a new, high-resolution dataset, CHELSA …
across environmental sciences. Here we introduce a new, high-resolution dataset, CHELSA …
Massive blow-out craters formed by hydrate-controlled methane expulsion from the Arctic seafloor
Widespread methane release from thawing Arctic gas hydrates is a major concern, yet the
processes, sources, and fluxes involved remain unconstrained. We present geophysical …
processes, sources, and fluxes involved remain unconstrained. We present geophysical …
[HTML][HTML] Population genomics of Mesolithic Scandinavia: Investigating early postglacial migration routes and high-latitude adaptation
T Günther, H Malmström, EM Svensson, A Omrak… - PLoS …, 2018 - journals.plos.org
Scandinavia was one of the last geographic areas in Europe to become habitable for
humans after the Last Glacial Maximum (LGM). However, the routes and genetic …
humans after the Last Glacial Maximum (LGM). However, the routes and genetic …
Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE‐CHRONO reconstruction
The BRITICE‐CHRONO consortium of researchers undertook a dating programme to
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …
[HTML][HTML] The build-up, configuration, and dynamical sensitivity of the Eurasian ice-sheet complex to Late Weichselian climatic and oceanic forcing
The Eurasian ice-sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …
Northern landscapes in transition: Evidence, approach and ways forward using the Krycklan Catchment Study
Improving our ability to detect changes in terrestrial and aquatic systems is a grand
challenge in the environmental sciences. In a world experiencing increasingly rapid rates of …
challenge in the environmental sciences. In a world experiencing increasingly rapid rates of …
[HTML][HTML] Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming
Methane seepage from the upper continental slopes of Western Svalbard has previously
been attributed to gas hydrate dissociation induced by anthropogenic warming of ambient …
been attributed to gas hydrate dissociation induced by anthropogenic warming of ambient …