Davos Atmosphere and Cryosphere Assembly DACA-13

Ice and Climate News nr. 10

5. Atmosphere-Ocean General Circulation Models 7. Global Prediction: Permafrost 8. Predicting Lake and River Ice 10. Operational Sea-Ice Analysis and Forecasting at met.no 11. Arctic Council Climate and Cryosphere Project 12. Seasonal Forecast of Antarctic Sea Ice 13. The Global Cryosphere Watch 14. Towards a Community Arctic System Model 16. Simulation of Glacier Mass and Energey Balance 18. T...

Seismic Wave Interactions Between the Atmosphere - Ocean - Cryosphere System and the Geosphere in Polar Regions

Surface Contribution to Planetary Albedo Variability in Cryosphere Regions

Climatological planetary albedo obtained from the International Satellite Cloud Climatology Project (ISCCP) D-series flux dataset is broken down into contributions from the surface and atmosphere in cryosphere regions. The atmosphere accounts for much more of climatological planetary albedo ( 75%) than the surface at all times of the year. The insignificance of the surface contribution over hig...

Production and characterization of monoclonal antibodies raised against the membrane ecdysone receptor from the anterior silk gland of the silkworm, Bombyx mori

Several evidences for nongenomic action of ecdysteroids through membrane receptor (mEcR) in programmed cell death (PCD) of the Bombyx mori anterior silk glands (ASGs) have been reported. The isolation, characterization and sequencing of mEcR still remain elusive. In the present work, monoclonal antibodies against mEcR has been raised, for the first time, and expected to facilitate any further m...

Anthropogenic warming of Earth's climate system.

We compared the temporal variability of the heat content of the world ocean, of the global atmosphere, and of components of Earth's cryosphere during the latter half of the 20th century. Each component has increased its heat content (the atmosphere and the ocean) or exhibited melting (the cryosphere). The estimated increase of observed global ocean heat content (over the depth range from 0 to 3...