• Aucun résultat trouvé

Temps Écoulé Jusqu'à 5 Heures, à Intervalle de 15 Minutes (A)

N/A
N/A
Protected

Academic year: 2021

Partager "Temps Écoulé Jusqu'à 5 Heures, à Intervalle de 15 Minutes (A)"

Copied!
2
0
0

Texte intégral

(1)

Calcul Temps Écoulé (A)

Calculez le temps écoulé entre la 1ère et la 2ème heures.

1ère heure 2ème heure Temps écoulé

20h30m 21h0m 23h0m 2h15m 6h45m 7h30m 2h0m 6h30m 20h0m 22h0m 0h15m 1h15m 2h0m 3h45m 21h45m 1h15m 8h45m 10h15m 15h15m 17h15m Mathslibres.com

(2)

Calcul Temps Écoulé (A) Réponses

Calculez le temps écoulé entre la 1ère et la 2ème heures.

1ère heure 2ème heure Temps écoulé

20h30m 21h0m 0 heures, 30 minutes. 23h0m 2h15m 3 heures, 15 minutes. 6h45m 7h30m 0 heures, 45 minutes. 2h0m 6h30m 4 heures, 30 minutes. 20h0m 22h0m 2 heures, 0 minutes. 0h15m 1h15m 1 heures, 0 minutes. 2h0m 3h45m 1 heures, 45 minutes. 21h45m 1h15m 3 heures, 30 minutes. 8h45m 10h15m 1 heures, 30 minutes. 15h15m 17h15m 2 heures, 0 minutes. Mathslibres.com

Références

Documents relatifs

Columnar aerosol size distribution parameters at night- time retrieved by GRASP using different schemes (see Ta- ble 2) show a good coherence and smooth variation when they are

From the analysis of stress distribution, the highest measured stresses are inferred to represent the actual deviatoric stress t whose maximum value gives an estimate of the

This hypothesis was justified for previous magnetospheric missions (Peder- sen, 1995), showing that the potential difference between the spacecraft body and a floating probe (i.e.

Après 4, 5 ou 6 jours de culture, le nombre des cellules germinales est toujours plus élevé dans les ovaires cultivés dans du milieu supplémenté en thymuline, ou en présence. de

Below, we employ these radar measurements of the convection flow, in conjunction with our knowledge of the motion of the OCB, to estimate the dayside reconnection voltage during

Here we report measurements of a suite of nine elemental ratios (Li/Ca, B/Ca, Na/Ca, Mg/Ca, Zn/Ca, Sr/Ca, Cd/Ca, Ba/Ca, and U/Ca) in 18 species of benthic marine invertebrates

We model atmospheric and non-tidal oceanic loading effects on surface gravity variations, us- ing global surface pressure field provided by the European Centre for Medium-range

1.5d, Figure 10b), the averaged TC-driven flux anomaly is negative in the North West Atlantic, North West Pacific, North East Pacific, Arabian Sea and South West Indian, and is