La Commutativité de l’Addition avec Quatre Termes (A)

We have observed a number of strong short-lived echoes with the EISCAT UHF radar at angles 83.5° and 78.6° with the geomagnetic field and at about 100-km altitude north in the

Despite the diculties in determining the exact variation in ¯ow angle across the ®eld of view, even an approximate estimate allows the ¯ow-angle dependence of the

On the other hand, deep into the magnetosphere, upstream waves are also expected to trigger eigenos- cillations of the local ®eld lines (Yumoto and Saito, 1983), if the source

Taniguchi, M., Shimada, J., Tanaka, T., Kayane, I., Sakura, Y., Shimano, Y., Dapaah-Siakwan, S., and Kawashima, S.: Disturbances of temperature-depth profiles due to surface

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

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events, impulsive events, non-flare associated particle events); (2) analysis of samples of solar atmospheric ma- terial (large solar particle events, elemental abundances,

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)