Addition à Travers la Forêt Hantée (Addition Trois-Chiffres) (A)

Indeed, this assumption may not be unrealistic, because the region of the particle injections that occurred in association with the Pi 2 onset was reported to span 5 h of local

The zonal ¯ow associated with the unperturbed east±west component (which includes the corotation ¯ow) then adds a weak eastward ¯ow in the dusk sector which reverses to a weak

Simulated 9-member ensemble mean time-series left axis together with TSI anomalies red curves, right axis for the period 3000–2000 BP: a global annual atmospheric surface

Ice thinning, upstream advection, and non-climatic biases for the upper 89% of the EDML ice core from a nested model of the Antarctic ice sheet... This work is licensed under a

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Thus independent regional climate records are provided by speleothem oxygen isotope records and marine alkenone records; lake sediment analyses and archaeological studies of

For low magnetic Prandtl number P m fluids, the upper bound of energy dissipation is that of classical turbulence (i.e. proportional to the cubic power of the shear velocity)

At low porosity and small wave number (k&•, •b0 < < 1) the porosity waves and the melt packets travel roughly twice as fast as the background extraction