Nghĩa của từ lapse rate bằng Tiếng Việt

@lapse rate
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Đặt câu có từ "lapse rate"

1. S3470 Superadiabatic lapse rate Temperature lapse rate with a magnitude greater than the dry adiabatic lapse rate.

2. A0560 Adiabatic lapse rate Theoretical temperature lapse rate of a parcel of air which moves adiabatically in the vertical.

3. S0260 Saturation adiabatic lapse rate Adiabatic lapse rate of saturated air whose magnitude is less than that of the adiabatic lapse rate of dry air owing to the release of latent heat.

4. D1270 Dry adiabatic lapse rate Adiabatic lapse rate (about 1°C/100 m) of dry air, and also, approximately, of moist unsaturated air.

5. The actual lapse rate, called the environmental lapse rate, is not constant (it can fluctuate throughout the day or seasonally and also regionally), but a normal lapse rate is 5.5 °C per 1,000 m (3.57 °F per 1,000 ft).

6. A0090 Absolute stability The state of a column of air in the atmosphere which has a temperature lapse rate less than the saturation-adiabatic lapse rate.

7. A3230 Autoconvective lapse rate Autoconvection gradient Largely hypothetical temperature lapse rate (3.4°C per 100 m in dry air) in an atmosphere whose density is constant with height (homogeneous atmosphere).

8. The saturated adiabatic lapse rate (SALR) is about half the DALR or 5°C/km.

9. FRAME: 116 While the dry adiabatic lapse rate is constant at about 10°C/ km, the saturated adiabatic lapse rate shows considerable variation because the amount of heat released varies according to how much water vapour condenses.

10. P1260 Potential instability Convective instability State of a column or layer of unsaturated air which becomes unstable if lifted bodily until completely saturated and if its lapse rate is then greater than the saturated-adiabatic lapse rate.

11. Before condensation, the air will be cooled at the dry adiabatic lapse rate, 10°C / km.

12. Above a heated surface, the vertical temperature gradient sometimes exceeds the dry Adiabatic lapse rate (i.e

13. FRAME: 170 A shallow lapse rate, an isothermal layer, or an inversion, is an indication of stable air.

14. FRAME: 113 This reduced rate of 5°C/ km, is known as the SATURATED ADIABATIC LAPSE RATE (SALR).

15. The change in temperature optimum with elevation was similar to the adiabatic lapse rate, suggesting a precise adaptation to temperature through natural selection.

16. The dry Adiabatic lapse rate has a value of about 10°C per 1000 m (5.5°F per 1000 ft) of vertical rise

17. From there on, follow the moist adiabatic lapse rate until the temperature of the parcel reaches the air mass temperature, at the equilibrium level (EL).

18. In the ICAO Standard Atmosphere, designed according to the adiabatic process, the temperature lapse rate is 6.5 oC per 1000 m (1.98 oC per 1000 feet).

19. A3220 Autoconvection gradient (A3230) Largely hypothetical temperature lapse rate (3.4°C per 100 m in dry air) in an atmosphere whose density is constant with height (homogeneous atmosphere).

20. Over large oceans, the changes in tropospheric moisture content appear to be closely linked to changes in SSTs and lower tropospheric air temperatures (consistent with a moist adiabatic lapse rate).

21. Meteorology Self Instructions Module 2 - Weather Determinants ANSWERS TO SELF-TEST Part D - Adiabatic Lapse Rate 1. adiabatic 2. approximately 5°C, about 10°C 3. condensation 4. heat 5. saturated; dry 6.

22. P1960 Pseudo-adiabatic lapse rate The rate of change of temperature with height in a rising air parcel when, under the most simplified conditions, the condensate (assumed to be water) immediately precipitates out.

23. D1370 Dry stage Phase of an adiabatic expansion process of moist air, in the absence of condensed water, in which the rising non-saturated air cools at the dry-adiabatic lapse rate, i.e. about 1°C/100 m.

24. An energy generator capable of transferring heat from a cold region to a hot region, which utilizes the adiabatic temperature difference called lapse rate generated in gas or gas-like particles when a field or an energy potential gradient is applied to the particles.

25. These changes allow TAMDAR data to be applied directly at the pressure they are observed at, remove the assumption that the atmosphere is following a standard lapse rate, remove the assumption that wind is constant with height, and permit the TAMDAR moisture fields to be Assimilated.Note that the Obsgrid modifications were included in the standard releases of Obsgrid starting in V3.8, while