Improved Surface Mass Balance Closure in Ocean Hindcast Simulations

Improved GRACE regional mass balance estimates

Introduction Conclusions References

High-resolution simulations of the surface mass balance of Greenland at the end of this century

Introduction Conclusions References Tables Figures ◭ ◮ ◭ ◮ Back Close Full Screen / Esc Abstract Introduction Conclusions References Tables Figures ◭ ◮ ◭ ◮ Back Close Full Screen / Esc Printer-friendly Version Interactive Discussion EGU Abstract We present atmospheric general circulation model simulations of the present (1981– 2005) and future (2081–2100) climate according to the SRES A1B green...

Improved fold closure in mass-spring low-dimensional glottal models

This work presents a low-dimensional physical model of the glottis in which a 2-D fold displacement representation allows to represent both the vertical and longitudinal displacements of the folds. We use a one-mass mechanical model, coupled to aerodynamic driving forces, and we use a delay line representation to account for the propagation of the displacement on the body-cover. The waveform is...

Conventional versus reference-surface mass balance

Glacier surface mass balance evaluated over the actual glacier geometry depends not only on climatic variations, but also on the dynamic adjustment of glacier geometry. Therefore, it has been proposed that reference-surface balances calculated over a constant glacier hypsometry are better suited for climatic interpretation. Here we present a comparison of 82 year modelled time series (1926– 200...

Mass Balance Constraints on the Elemental Composition of the Ocean