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With increasing height, temperature, pressure, atmospheric humidity, and dust content decrease.
Fig. 6 Monthly-mean 3-hourly GMS cloud-top height (temperature) distributions in 1999.
Spatio-temporal monitoring of the tropopause height, temperature and pressure is an appropriate tool to show the running processes in the atmosphere.
Based on sea-surface height, temperature, and velocity from a 17-year model run, we quantify the footprint of existing moorings to identify the extent to which the shelf circulation is likely to be represented by those moorings.
It has also been established that height-latitude distribution amplitudes and phases significantly differ for geopotential height, temperature, zonal and meridional wind and depend on wave number and hemisphere.
Experimental observations on adatom position, height, temperature clustering and Ostwald ripening, p- or n-doping, or the electronic configuration can be rationalized by present calculations, which deliver a solid theoretical ground from which experimental features can be interpreted and discussed.
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Both the time-average and the dynamic flame structure, including flame height, peak temperature, and flicker frequency, are found to be influenced by chemical kinetics.
However, when dry air is found at the same height, temperatures at 500 hPa need to be even colder as dry atmospheres require a greater lapse rate for instability than moist atmospheres.
Experimental measurements of visible flame heights, temperatures, and pollutant emission indices in partially premixed swirling flames with a broad range of central fuel tube equivalence ratios (ΦF) are reported.
Instruments of the unmanned spacecraft, engineered to penetrate cloud cover, provided data on a wide array of oceanographic conditions and features, including wave height, water temperature, currents, winds, icebergs, and coastal characteristics.
Figure 10 shows the curve of barrier height vs temperature.
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