Vertical distributions

inner structure of the planet Earth, consisting of several concentric spherical layers

result of a scientific drilling project of the Soviet Union on the Kola Peninsula

variation of temperature of Earth at different depths

mass per unit volume of earths atmosphere

formula used to model how air pressure varies with altitude

separation of water in a lake into distinct layers

Vertical rate of change of temperature in atmosphere

layering of a body of water due to density variations

layer in a fluid where there is a force balance between pressure gradient force, Coriolis force and turbulent drag

vertical arrangement of vegetation in layers

wind model

vibration measurement using boreholes

the temperatures of the Earth’s oceans across depth, location and seasons