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Sodium Moon Spot (SMS) lake-ye sodiomi-ye Mâng Fr.: tache de sodium de la Lune The → sodium tail of the Moon as it appears in the sky opposite the Sun. The SMS undergoes changes in shape and brightness. It is brighter when the → new moon occurs at → perigee, when the new moon is north of the → ecliptic, and approximately five hours after the new moon. |
sodium tail of the Moon donbâle-ye sodiomi-ye Mâng Fr.: queue de sodium de la Lune A comet-like tail of the Moon comprised of → sodium (Na) atoms and invisible to the naked eye. The lunar surface is constantly bombarded by the → solar wind, → photons, and → meteoroids, which can liberate Na atoms from the → regolith. These atoms are subsequently accelerated by solar → radiation pressure to form a long comet-like tail opposite the Sun. Near → new moon, this diffuse cloud of Na atoms encounters the Earth's gravity and is "pinched" into a beam of enhanced density. This beam appears as the ~3° diameter Sodium Moon Spot (SMS) seen in the sky opposite the Sun. The spot is about five times the diameter of the → full moon, and is 50 times fainter than can be seen with the unaided eye. The spot is reflected light from millions of Na atoms that two days earlier were on the surface of the Moon. This spot is visible to sensitive cameras equipped with filters tuned to the orange light emitted by Na atoms near 589.3 nm (Baumgardner et al., 2021 Journal of Geophysical Research: Planets DOI: 10.1029/2020je006671). |
soft iron âhan-e narm Fr.: fer doux Iron that has a low carbon content, in contrast to → steel. Because it is easily magnetized and demagnetized, it is used to make the cores of → solenoids and other electrical equipment. |
solar constant pâypa-ye xoršidi (#) Fr.: constante solaire The amount of solar radiation in all wavelengths received per unit of time per unit of area on a theoretical surface perpendicular to the Sun's rays and at Earth's mean distance from the Sun. Its mean value is 1367.7 W m-2 or 1.37 × 106 erg sec-1 cm-2. In other words, the solar constant is the mean → solar irradiance on the outer atmosphere when the Sun and Earth are spaced at 1 → astronomical unit. See also: → solar luminosity. |
solar corona hurtâj, tâj-e xoršid (#) Fr.: couronne solaire The outermost atmosphere of the Sun immediately above the → chromosphere, which can be seen during a total solar eclipse. It consists of hot (1-2 × 106 K), extremely tenuous gas (about 10-16 g cm-3) extending for millions of kilometer from the Sun's surface. |
solar depression nešib-e xoršid Fr.: dépression solaire The → angle between the → sea horizon, the → center of → Earth, and the center of the → solar disk. → solar; → depression. |
solar equation hamugeš-e xoršidi Fr.: équation solaire In ancient astronomy, the difference between the Sun's mean and actual position. The ancients observed that, although the motion of the Sun in the ecliptic is almost uniform, it is subject to a small annual variation. |
solar longitude derežnâ-ye xoršidi Fr.: longitude du Soleil The ecliptic longitude of the Sun. It varies from 0° (at the vernal equinox) to 360° during the year. By Kepler's Second Law, the rate of change of the solar longitude is such that the Earth sweeps out equal areas on the ecliptic plane in equal times. |
solar radiation tâbeš-e xoršidi Fr.: rayonnement solaire All the constituents making up the Sun's emission: photons, electrons, protons, neutrinos, and atomic nuclei. |
solar radiation pressure fešâr-e tâbeš xoršid (#) Fr.: pression du rayonnement solaire The → radiation pressure of solar photons, which pushes a comet's dust outward to form a → dust tail. |
solar rotation carxeš-e xoršid (#) Fr.: rotation du Soleil The motion of the Sun around an axis which is roughly perpendicular to the plane of the → ecliptic; the Sun's rotational axis is tilted by 7.25° from perpendicular to the ecliptic. It rotates in the → counterclockwise direction (when viewed from the north), the same direction that the planets rotate (and orbit around the Sun). The Sun's rotation is differential, i.e. the period varies with latitude on the Sun (→ differential rotation). Equatorial regions rotate in about 25.6 days. The regions at 60 degrees latitude rotate more slowly, in about 30.9 days. |
Solberg-Hoiland criterion sanjidâr-e Solberg-Høiland Fr.: critère de Solberg-Høiland A criterion for → convective stability in → massive stars. The Solberg-Høiland stability criterion corresponds to the inclusion of the effect of → rotation (variation of → centrifugal force) in the convective stability criterion. It is a combination of → Ledoux's criterion (or possibly → Schwarzschild's criterion) and → Rayleigh's criterion. Both the dynamical shear and Solberg-Høiland instabilities occur in the case of a very large → angular velocity decrease outwards. Therefore, in a → rotating star the Ledoux or Schwarzschild criteria for convective instability should be replaced by the Solberg-Høiland criterion. More specifically, this criterion accounts for the difference of the centrifugal force for an adiabatically displaced fluid element. It is also known as the axisymmetric baroclinic instability. It arises when the net force (gravity + buoyancy + centrifugal force) applied to a fluid parcel in an adiabatical displacement has components only in the direction of the displacement (A. Maeder, Physics, Formation and Evolution of Rotating Stars, 2009, Springer). E. Høiland, 1939, On the Interpretation and Application of the
Circulation Theorems of V. Bjerknes. Archiv for mathematik og
naturvidenskab. B. XLII. Nr. 5. Oslo. |
solidification dafzeš; dafzâneš Fr.: solidification 1) To become or make solid, hard, or firm. |
soliton soliton Fr.: soliton Math., Physics: A solution of a certain type of partial differential equation that represents a solitary wave. A soliton is a self-reinforcing wave that maintains its shape while it travels at constant speed. Solitons are caused by a cancellation of nonlinear and dispersive effects in the medium. From solit(ary) + → -on. |
solution luyeš Fr.: solution 1) The act of solving a problem, question. The state of being solved. Verbal noun of → solve. |
solvation luyé Fr.: solvation Any of a class of chemical reactions in which solute and solvent molecules combine. From solv(ent), → solvent + -ation. Luyé, from luy- the stem of luyidé→ solute and luyandé→ solvent + -é nuance suffix. |
sonde gomâné Fr.: sonde A rocket or balloon carrying instruments to probe conditions in the upper atmosphere. From Fr. sonde "ounding line; plumb line." Gomâné "a shaft sunk in order to ascertain the depth of the water when making a subterraneous canal," from Proto-Iranian *vi-mā-, from vi- "apart, away from, out" (cf. Av. vi-; O.Pers. viy- "apart, away;" Skt. vi- "apart, asunder, away, out;" L. vitare "to avoid, turn aside") + mā- "to measure" (cf. O.Pers./Av. mā(y)- "to measure;" Mod.Pers. mâ/mun/mân "measure," as in Pers. terms âzmâ- "to test;" pirâmun "perimeter," âzmun "test, trial," peymân "measuring, agreement," peymâné "a measure; a cup, bowl;" PIE base *me- "to measure;" cf. Skt. mati "measures," matra- "measure;" Gk. metron "measure;" L. metrum). |
sonic sedâyi (#) Fr.: sonique Of, relating to, or being the speed of sound in a medium. From L. sonus, → sound. Sedâyi, pertaining to sedâ, → sound. |
sonic boom qariv-e sedâ (#) Fr.: bang sonique A noise caused by a shock wave that emanates from an object traveling at or above the speed of sound. → sonic; boom, M.E. bombon, bummyn "to buzz;" cf. Du. bommen, Ger. bummen, word made by sound imitation. Qariv "shout, clamour, cry;" sedâyi, → sonic. |
sonic point noqte-ye sedâyi Fr.: point sonique The point where the → stellar wind makes a transition from → subsonic to → supersonic flow. In the particular case of a spherically symmetric wind (thus with no magnetic field), the distance from star, at which the sonic point occurs, is given by: rs = (GM*)/2cs2, where G is the → gravitational constant, M* is the stellar mass, and cs the → sound speed at the sonic point. |
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