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Evolution of temperature field and streamlines has been examined.
Here, the nonlinear trend may be defined as a component of global warming because it represents the evolution of temperature at the century scale since 1889.
However, to age fossilized samples in relevant Martian conditions, modeling the evolution of temperature and pressure in the Martian subsurface is required.
The strain recorded follows the logical evolution of temperature with no abnormal behaviour being detected.
A mathematical model is built to analyze the evolution of temperature.
It also predicts the evolution of temperature inside the material samples.
The evolution of temperature and the heater thermal output were also reasonably well predicted by the model.
The evolution of temperature, H2 partial pressure and reaction of Mg powder through the charging process are analysed.
The dynamically changing activity profiles reflect the evolution of temperature profiles and product compositions with only minor deviations.
A transient 1D thermal model of a pavement section was developed to simulate the temporal evolution of temperature within PCM-containing pavement sections exposed to realistic climate conditions.
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For instance, the contemporary evolution of temperature-dependent development has been shown for salmonid fish populations introduced to new thermal environments (e.g., Haugen and Vøllestad 2000) and for amphibian populations subject to pond warming as a result of beaver activity (Skelly and Freidenburg 2000).
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