potential temperature वाक्य
उदाहरण वाक्य
मोबाइल
- The comparison of the equivalent potential temperature of parcels of air at different pressures thus provides a measure of the instability of the column of air.
- The occurrence of mafic dike swarms in Archean and Paleoproterozoic terrains is often cited as evidence for mantle plume activity associated with abnormally high mantle potential temperatures.
- :The melting point of gold ( ~ 1000 C ) is significantly lower than the potential temperature of a charcoal fire ( ~ 2700 C ).
- Suitable boundary conditions have to be imposed for the wind velocity components u, v and w, the potential temperature \ theta and pressure p at all boundaries.
- The air around the mountain is stable because the air at the top, due to its lower pressure, has a higher potential temperature than the warmer air below.
- Each of these coefficients are functions of the known variables, such as the average wind speed at 10m, and average potential temperature and moisture at the surface and 10m.
- These equations along with the ideal gas law are used to evolve the density, pressure, and potential temperature scalar fields and the velocity vector field of the atmosphere through time.
- Things like the temperature ( potential temperature ), precipitable water, and to an extent the pressure thickness simply move from one spot on the grid to another with the wind.
- Since potential temperature is conserved under adiabatic or isentropic air motions, in steady, adiabatic flow lines or surfaces of constant potential temperature act as streamlines or flow surfaces, respectively.
- Since potential temperature is conserved under adiabatic or isentropic air motions, in steady, adiabatic flow lines or surfaces of constant potential temperature act as streamlines or flow surfaces, respectively.
- Common examples include potential temperature, salinity, and concentration of CFCs, tritium ( introduced to the ocean surface by atomic bomb tests ), oxygen, and many other compounds.
- Potential temperature is conserved for all dry adiabatic processes, and as such is an important quantity in the planetary boundary layer ( which is often very close to being dry adiabatic ).
- Forecast files are organized by level type ( single level, pressure level, potential vorticity level, and potential temperature level ), and forecast time-step for a specified model.
- For saturated air, or for air which is likely to be lifted high enough to reach saturation, it is the equivalent potential temperature which must increase with height in order to ensure stability.
- Fire endurance tests for this application must be run under 50Pa positive furnace pressure in order to adequately simulate the effect of potential temperature differences between indoor and outdoor temperatures in Canada's winters.
- (2 ) The "'Mixed layer "'composing the middle 35 to 80 % of CBL is characterized by conserved variables such as potential temperature, wind speed and moisture.
- These equations along with the ideal gas law are used to evolve the density, pressure, and potential temperature scalar fields and the air velocity ( wind ) vector field of the atmosphere through time.
- Once the CCL is determined, the surface temperature necessary to raise a mass of air to that height can be found by using the Dry Adiabatic Lapse Rate ( DALR ) to determine the potential temperature.
- The mixed layer, the major part of CBL, has a nearly constant distribution of quantities such as potential temperature, wind speed, moisture and pollutant concentration because of strong buoyancy generated convective turbulent mixing.
- Since convection acts to quickly mix the atmosphere and return to a stably stratified state, observations of decreasing potential temperature with height are uncommon, except while vigorous convection is underway or during periods of strong insolation.
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