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In atmospheric sciences (meteorology, climatology and related fields), the temperature gradient (typically of air, more generally of any fluid) is a physical quantity that describes in which direction and at what rate the temperature changes the most rapidly around a particular location. The temperature gradient is a dimensional quantity expressed in units of degrees (on a particular temperature scale) per unit length. The SI unit is kelvin per metre (K/m).

Contents 1 Mathematical description 2 Weather and climate relevance 3 Day to day experiences and health issues 4 See also 5 References 6 External links

Assuming that the temperature T is an intensive quantity, i.e., a single-valued, continuous and differentiable function of three-dimensional space (often called a scalar field), i.e., that

T = T(x,y,z)

where x, y and z are the coordinates of the location of interest, then the temperature gradient is the vector quantity defined as

Differences in air temperature between different locations are critical in weather forecasting and climate. The absorption of solar light at or near the planetary surface increases the temperature gradient and may result in convection (a major process of cloud formation, often associated with precipitation). Similarly, on a global and annual basis, the dynamics of the atmosphere (and the oceans) can be understood as attempting to reduce the large difference of temperature between the poles and the equator by redistributing masses of warm and cold air (and water).

Meteorological fronts are regions where the horizontal temperature gradient may reach relatively high values, as these are boundaries between air masses with rather distinct properties.

Clearly, the temperature gradient may change substantially in time, as a result of diurnal or seasonal heating and cooling for instance.

Other places where noticeable temperature gradients can be experienced include the entrance (or exits) of air conditioned shops in the summer, or the entrance of caves and other protected or poorly ventilated areas.

Rapid changes in temperature (in space or time) may cause discomfort and, in extreme cases, heat or cold stresses.

• Gradient
• Adiabatic lapse rate

• Edward N. Lorenz (1967) The nature and theory of the general circulation of atmosphere, World Meteorological Organization, Publication No. 218, Geneva, Switzerland.

• M. I. Budyko (1978) Climate and Life, Academic Press, International Geophysics Series, Volume 18, ISBN 0-12-139450-6.

• Robert G. Fleagle and Joost A. Businger (1980) An Introduction to Atmospheric Physics, Second Edition, Academic Press, International Geophysics Series, Volume 25, ISBN 0-12-260355-9.

• David Miller (1981) Energy at the Surface of the Earth: An Introduction to the Energetics of Ecosystems, Academic Press, International Geophysics Series, Volume 29.

• John M. Wallace and Peter V. Hobbs (2006) Atmospheric Science: An Introductory Survey, Second Edition, Academic Press, International Geophysics Series, ISBN 0-12-732951-X.

• IPCC Third Assessment Report