Addition et Soustraction des Nombres à 3, 4 et 5 Chiffres (A)

(a) Wavelet spectra of thermocline displacement at Cape Struga (thick full line), sea level at Dubrovnik (thin full line) and NE wind component at Dubrovnik (dotted line), for

The plasma convection velocities determined independently by the two radars are shown to agree very closely and the combined three-dimensional velocity data used to test the

Solar cycle evolution of active regions and coronal holes From an analysis of the 10 IGSs that occurred between 1978 and 1979, combining interplanetary scintillation (IPS) tracking

The turbulence refractivity structure constant (C 2 n ) is one of the basic parameters of atmospheric turbulence which can be determined using the radar measurements of the

Based on the different forms of entropy balance between exact and anelastic models, we find that a necessary condition for convergence of the anelastic results to the exact solutions

Simulating nitrogen budgets in complex farming systems using INCA: calibration and scenario analyses for the Kervidy catchment but, in terms of nitrate flux, the result is almost

Ozone vertical profiles derived from nadir mea- surements of the GOME instrument on board the ERS-2 satellite, by means of the FURM algorithm of the Univer- sity of Bremen,

(4) and (5), the values of kx and kz are chosen to be the dominant horizontal and vertical wave numbers at each integer hour (shown in Fig. 2), respectively; the values u; w and ma