Wind and waves in the Northern Adriatic Sea

Observations of neutral depletion and plasma acceleration in a flowing high-power argon helicon plasma

“…34 We therefore use in =1/ ͑n n in ͒ as a lower bound to evaluate collisionality, with corresponding en values being an order of magnitude larger. 34 We therefore use in =1/ ͑n n in ͒ as a lower bound to evaluate collisionality, with corresponding en values being an order of magnitude larger.…”

e± Ar scattering in the energy range 1 eV ≤ E i ≤ 0.5 GeV

“…where U=E i /I is the reduced energy. It is observed in a number of experiments [7,[52][53][54], that the value of R(E i ) rises steadily as the energy increases above the threshold, and approaches unity at very high energies. All the above adjustable parameters A, B and C are, therefore, determined using the following three simple conditions…”

“…Since the first electron-atom scattering experiments in 1931 [5], many theoretical and experimental studies on e ± -Ar have been available in the literature [6][7][8]. Apart from these investigations, the experimental works of Ranković et al [9], Zecca et al [10], Jones et al [11], Kurokawa et al [12], Cho and Park [13], Hargreaves et al [14], Milosavljević et al [15], Mielewska et al [16] and Gilbert et al [17], and the theoretical calculations of Ranković et al [9], Bartschat et al [18], Green et al [19], Fursa and Bray [20], Jones et al [11], Mohan et al [21], McEachran and Stauffer [22], Bote et al [23], Gargioni and Grosswendt [4], Adibzadeh and Theodosiou [24], Yousif Al-Mulla [25], Jablonski et al [26], Salvat [27], Stepanek [28], Blanco and García [29,30], Paikeday and Alexander [31], Kelemen [32], Bartlett and Stelbovics [33], Sienkiewicz et al [34] and Pandya and Shah [35], are worth mentioning among the important works.…”

Shore grykes along the western Istrian coast

“…The winds of t�e Sout�west and t�e Nort�west quadrant raise it, t�us leading to "�ig�water" p�enomena. Mean significant wave �eig�t during t�e year is lower t�an 0.5 m (Dal Cin & Simeoni 1994), w�ile t�e �ig�est offs�ore wave �eig�t, bot� for Bora and Scirocco storms, is about 5 m (Cavaleri et al 1996). The �ig�est mean �ourly speed for sout�east wind in t�e period 1958-1987 was 27.3 m/s.…”