Friday, January 25, 2013

European Geosciences Union

  • Speedup and fracturing of George VI Ice Shelf, Antarctic Peninsula
  • Surface motion of active rock glaciers in the Sierra Nevada, California, USA: inventory and a case study using InSAR
  • Glacier changes and climate trends derived from multiple sources in the data scarce Cordillera Vilcanota region, southern Peruvian Andes
  • Radar stratigraphy connecting Lake Vostok and Dome C, East Antarctica, constrains the EPICA/DMC ice core time scale
  • Current state of glaciers in the tropical Andes: a multi-century perspective on glacier evolution and climate change
  • An analysis of present and future seasonal Northern Hemisphere land snow cover simulated by CMIP5 coupled climate models
  • Area and volume loss of the glaciers in the Ortles-Cevedale group (Eastern Italian Alps): controls and imbalance of the remaining glaciers
  • North Atlantic warming and declining volume of arctic sea ice
  • Climatic drivers of seasonal glacier mass balances: an analysis of 6 decades at Glacier de Sarennes (French Alps)
  • Density assumptions for converting geodetic glacier volume change to mass change
  • Hoar crystal development and disappearance at Dome C, Antarctica: observation by near-infrared photography and passive microwave satellite
  • Numerical simulations of Gurenhekou Glacier on the Tibetan Plateau using a full-Stokes ice dynamical model
  • High-resolution interactive modelling of the mountain glacier–atmosphere interface: an application over the Karakoram
  • Sensitivity of alpine glacial change detection and mass balance to sampling and datum inconsistencies
  • New estimates of Arctic and Antarctic sea ice extent during September 1964 from recovered Nimbus I satellite imagery
  • Spatial and temporal variations of glacier extent across the Southern Patagonian Icefield since the 1970s
  • Glacier volume estimation as an ill-posed boundary value problem
  • Transient thermal modeling of permafrost conditions in Southern Norway
  • The Arctic Sea ice in the CMIP3 climate model ensemble – variability and anthropogenic change
  • Net accumulation rates derived from ice core stable isotope records of Pío XI glacier, Southern Patagonia Icefield
  • Snow specific surface area simulation using the one-layer snow model in the Canadian LAnd Surface Scheme (CLASS)
  • A balanced water layer concept for subglacial hydrology in large scale ice sheet models
  • Micrometeorological conditions and surface mass and energy fluxes on Lewis glacier, Mt Kenya, in relation to other tropical glaciers
  • Global glacier volumes and sea level – effects of ice below the surface of the ocean and of new local lakes on land
  • Snow spectral albedo at Summit, Greenland: comparison between in situ measurements and numerical simulations using measured physical and chemical properties of the snowpack
  • Mass balance, runoff and surges of the Bering Glacier, Alaska
  • Hindcasting to measure ice sheet model sensitivity to initial states
  • Ikaite crystal distribution in Arctic winter sea ice and implications for CO2 system dynamics
  • The role of cornice fall avalanche sedimentation in the valley Longyeardalen, Central Svalbard
  • Gravity effect of glacial ablation in the Eastern Alps – observation and modeling
  • Evidence and analysis of 2012 Greenland records from spaceborne observations, a regional climate model and reanalysis data
  • Influence of ablation-related processes in the built-up of simulated Northern Hemisphere ice sheets during the last glacial cycle
  • Sea ice thickness, freeboard, and snow depth products from Operation IceBridge airborne data
  • Modelling and mapping climate change impacts on permafrost at high spatial resolution for a region with complex terrain
  • Quantifying present and future glacier melt-water contribution to runoff in a Central Himalayan river basin
  • Recent changes in spring snowmelt timing in the Yukon River Basin detected by passive microwave satellite data
  • Surface mass balance model intercomparison for the Greenland ice sheet
  • The influence of climate and hydrological variables on opposite anomaly in active layer thickness between Eurasian and North American watersheds

1 comment:

  1. The Cryosphere Discussions (TCD) - Papers in Open Discussion

    http://www.the-cryosphere-discuss.net/papers_in_open_discussion.html

    The Cryosphere (TC) - An Interactive Open Access Journal of the European Geosciences Union

    http://www.the-cryosphere.net/

    The Cryosphere (TC) is an international scientific journal dedicated to the publication and discussion of research articles, short communications and review papers on all aspects of frozen water and ground on Earth and on other planetary bodies.

    The main subject areas are:
    ・ ice sheets and glaciers;
    ・ planetary ice bodies;
    ・ permafrost, river and lake ice;
    ・ seasonal snowcover;
    ・ sea ice;
    ・ remote sensing, numerical modelling, in-situ and laboratory studies of the above and including studies of the interaction of the cryosphere with the rest of the climate system.

    The Cryosphere has an innovative two-stage publication process which involves a scientific discussion forum and exploits the full potential of the Internet to:
    ・ foster scientific discussion;
    ・ enhance the effectiveness and transparency of scientific quality assurance;
    ・ enable rapid publication;
    ・ make scientific publications freely accessible.

    In the first stage, papers that pass a rapid access-review by one of the editors are immediately published on the The Cryosphere Discussions (TCD) website. They are then subject to Interactive Public Discussion, during which the referee’s comments (anonymous or attributed), additional short comments by other members of the scientific community (attributed) and the author’s replies are also published in TCD. In the second stage, the peer-review process is completed and, if accepted, the final revised papers are published in TC. To ensure publication precedence for authors, and to provide a lasting record of scientific discussion, TCD and TC are both ISSN-registered, permanently archived and fully citable.

    _________________________________
    The Cryosphere (TC) and The Cryosphere Discussions (TCD) are published by the Copernicus GmbH (Copernicus Publications) on behalf of the European Geosciences Union (EGU).

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