Answer: Adiabatic temperature gradient is the rate of change in temperature due to pressure under adiabatic conditions.
Explanation:
The rate of change of temperature due to pressure under adiabatic conditions is referred to as adiabatic temperature gradient.
In practice, since in the sea the pressure changes can be considered proportional to depth changes, the adiabatic temperature gradient is usually given as rate of change per unit depth, instead of per unit pressure and for practical purposes and calculations, the unit of depth is often chosen as 1000 m.
The natural and non-natural heat transfer influence the process of adiabatic temperature gradient.
Answer:
1991, because that is when the Soviet Union began producing fewer nuclear weapons.
Explanation:
OR C
<h2>
Answer: Average temperatures would increase.</h2>
Explanation:
Radiative forcing refers to the <u>change in the net flow of radiative energy towards the surface of the Earth</u>. This is due to internal changes in the composition of the atmosphere, or changes in the external contribution of the energy that comes from the Sun.
To determine this, measurements are taken at the upper edge of the troposphere, in order to obtain the difference between the radiation absorbed by the Earth and the energy radiated back into space.
It should be noted that a positive value of radiative forcing contributes to heating the Earth's surface, while a negative value contributes to its cooling.
Therefore, if the radiative forcing increases <u>the average temperature will increase as well.</u>