TERMIUM Plus^®

Record 1,  Textual support,  English

Record 1,  Textual support,  French

Record number: 1, Textual support number: 1 CONT

Les mesures d’angles verticaux sont effectuées en général cercle à droite et cercle à gauche; la moyenne est alors affranchie de la collimation verticale(défaut de calage de la graduation zéro au site zéro ou à la distance zénithale zéro).  2, record 1, French, - cercle%20%C3%A0%20gauche

Record 1,  Textual support,  Spanish

Record 2,  Textual support,  English

Record 2,  Textual support,  French

Record number: 2, Textual support number: 1 CONT

Les mesures d’angles verticaux sont effectuées en général cercle à droite et cercle à gauche; la moyenne est alors affranchie de la collimation verticale(défaut de calage de la graduation zéro au site zéro ou à la distance zénithale zéro).  2, record 2, French, - cercle%20%C3%A0%20droite

Record 2,  Textual support,  Spanish

Record 3,  Textual support,  English

Record 3,  Textual support,  French

Record 3,  Textual support,  Spanish

Record number: 3, Textual support number: 1 DEF

Cero, usado como carácter de relleno, que aparece como el dígito de mayor significado (más a la izquierda) en un valor numérico visualizado en un medio legible por el hombre.  2, record 3, Spanish, - cero%20a%20la%20izquierda

Record 4,  Textual support,  English

Record number: 4, Textual support number: 1 OBS

A quantity which rigorously assumes the value of zero is said to be identically zero. The "identically" is used for emphasis when simply stating that a quantity is (or appears to be) zero is not considered sufficiently strong. A quantity that is identically zero is said to be vanishing, or sometimes (again for emphasis) to vanish identically.  1, record 4, English, - identically%20zero

Record number: 4, Textual support number: 1 CONT

Although there is no missing data within the reanalysis dataset, there are a few cases where relative humidity values are identically zero, even in the lower levels. These values are not physically realistic and are excluded from the analysis.  2, record 4, English, - identically%20zero

Record 4,  Textual support,  French

Record number: 4, Textual support number: 1 CONT

[...] calculons le membre de gauche de cette équation, qui devrait donner identiquement zéro [...]  2, record 4, French, - identiquement%20z%C3%A9ro

Record number: 4, Textual support number: 1 PHR

Donner identiquement zéro, valoir identiquement zéro.  3, record 4, French, - identiquement%20z%C3%A9ro

Record 4,  Textual support,  Spanish

Record 5,  Textual support,  English

Record number: 5, Textual support number: 1 DEF

That value of wind speed which is exceeded half the time.  2, record 5, English, - median%20wind%20speed

Record number: 5, Textual support number: 1 CONT

The description of wind speeds is an example of the use of the Weibull distribution to describe natural phenomena. Each part of the planet has it's own parameters for a Weibull distribution to describe the wind speed pattern in that place. On the basis of that you can calculate the number of days a year, or hours a day, with wind speeds above a certain force, or the mean wind speed, or the median wind speed, halve the days in a year have a wind speed below the median force, halve the days above. The Weibull distribution is very practical in this area because the distribution doesn't allow for negative value's and it is easy to appropriately consider the fact that on most days there will be a bit of wind, on some days a lot and you have those days that there is way too much wind speed.  3, record 5, English, - median%20wind%20speed

Record number: 5, Textual support number: 1 OBS

median: When a series of 'n' observations is arranged in order of magnitude, the central value (n odd), or the mean of the two central values (n even), is termed the "median". The median may differ appreciably from the "mean", in which case the frequency distribution is said to be "skew".  4, record 5, English, - median%20wind%20speed

Record 5,  Textual support,  French

Record number: 5, Textual support number: 1 OBS

La distribution de Weibull - vitesse utilisable. On s’est aperçu que la vitesse du vent à un endroit donné dessinait une courbe statistique nommé distribution de Weibull. On peut donc déduire, par des méthodes mathématiques connues la vitesse médiane, la vitesse moyenne, etc.  2, record 5, French, - vitesse%20m%C3%A9diane%20du%20vent

Record number: 5, Textual support number: 2 OBS

Description statistique des vitesses du vent. [...] le graphe, ci-dessus représenté, est une distribution de probabilité(distribution fréquentielle). La probabilité que le vent souffle à une vitesse quelconque(zéro inclus) étant obligatoirement égale à 100 % [...]. La moitié de la zone bleue se trouve à gauche de la ligne verticale noire située à 6, 6 m/s. On dit alors que 6, 6 m/s est la médiane de la distribution. Cela signifie que le vent souffle à moins de 6, 6 m/s la moitié du temps, et à plus de 6, 6 m/s pendant l'autre. [...] nous avons alors fixé la vitesse moyenne à 7 m/s.  3, record 5, French, - vitesse%20m%C3%A9diane%20du%20vent

Record 5,  Textual support,  Spanish

Record 6,  Textual support,  English

Record 6,  Textual support,  French

Record number: 6, Textual support number: 1 OBS

à gauche du zéro(du limbe du sextant) à droite de l'index(voir cotter p. 344)(Deux façons différentes d’exprimer la même chose)  1, record 6, French, - %C3%A0%20droite%20de%20l%26rsquo%3Bindex

Record 6,  Textual support,  Spanish