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The degree of atmospheric instability depends on the temperature gradient (i.e., the rate at which air temperature changes with altitude).
Correlation coefficients show that the analysed fissures react to the air temperature changes with different intensities.
Two types of radiation adjustment were applied in order to evaluate the effect of air temperature changes on photosynthesis.
The variation of spatial soil moisture pattern is more sensitive to change in ground temperature rather than air temperature changes.
Furthermore, air temperature changes the pressure of the gas and makes it difficult to predict the flight of the pellet or BB, particularly at longer ranges.
Fig. 6 Left: Surface air temperature changes in the northern winter hemisphere from model calculation including energetic electron precipitation and NOx production (Rozanov et al. 2005).
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The changes are plotted as functions of the surface air temperature change.
In this study, we relate simulated surface air temperature change to canyon albedo change.
Similarly, Fig. 5b displays the millennial scale of the ocean temperature change with respect to the surface air temperature change.
This work assesses whether a neighborhood-scale cool roof demonstration could yield an observable air temperature change.
Figure 5a displays the relation between the surface air temperature change and the temperature changes for four oceanic layers of different depths.
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CEO of Professional Science Editing for Scientists @ prosciediting.com