Nghĩa của từ potential temperature bằng Tiếng Việt

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Đặt câu có từ "potential temperature"

Dưới đây là những mẫu câu có chứa từ "potential temperature", trong bộ từ điển Từ điển Anh - Việt. Chúng ta có thể tham khảo những mẫu câu này để đặt câu trong tình huống cần đặt câu với từ potential temperature, hoặc tham khảo ngữ cảnh sử dụng từ potential temperature trong bộ từ điển Từ điển Anh - Việt

1. T0820 Thetagram Aerological diagram whose co-ordinates are the equivalent potential temperature (or pseudo-potential temperature) and the pressure.

2. E0950 Equivalent potential temperature The potential temperature corresponding to the adiabatic equivalent temperature. qE = Tae(100/p)0.286, where qE is the equivalent potential temperature; Tae, the adiabatic equivalent temperature; and p, the pressure in hPa.

3. I1210 Isentropic surface Surface of constant entropy or of constant potential temperature.

4. P1270 Potential temperature Temperature (q) that an air parcel would have if brought dry adiabatically to a pressure of 1000 hPa.

5. M1720 Moist adiabaic Saturated adiabatic, Wet adiabatic A line representing a constant value of wet-bulb potential temperature on a thermodynamic diagram.

6. Formation of frontal zones in the mid troposphere is simulated with an adiabatic inviscid primitive equation model using potential temperature as vertical coordinate.

7. W0750 Wet-bulb pseudo-potential temperature Pseudo-wet-bulb potential temperature Fictitious temperature which would be assumed by an air parcel raised adiabatically to the condensation level, and then brought down to the 1000-hPa level by a pseudo-adiabatic process, the parcel being continuously supplied with the amount of water required to remain saturated in spite of evaporation.

8. Sigma-theta is computed as follows: Salinity is combined with potential temperature computed from the World Ocean Atlas temperature Climatology to compute the potential density anomaly (sigma-theta) defined as

9. Adiabatic processes of moist (but unsaturated) air are described elsewhere in this encyclopedia (see Thermodynamics: Moist (Unsaturated) Air), and it is shown that potential temperature remains constant during such processes as long as condensation does not occur

10. Ocean island Basaltic magmas are enriched in H 2 O relative to depleted MORB, giving rise to the possibility that the excess magmatism associated with mantle plumes is caused, at least in part, by the effect of higher H 2 O on mantle melting rather than solely being due to high mantle potential temperature (Schilling et al., 1980; Bonatti, 1990).