Current
In hydrology, throughflow is the horizontal movement of water in the soil zone.
Surface current
Through flow is the horizontal movement of water through the soil zone. Groundwater flow is the movement of water through the bedrock, which is typically an aquifer
Atmospheric transport is the process by which land sinks with little or no horizontal movement.
A sliding hanger is used when thermal horizontal movement is a factor. This type of hanger allows for horizontal movement as the pipe expands or contracts due to temperature changes. It helps prevent excessive stress on the piping system and supports its movement.
The antonym for convection is advection. Advection refers to the transfer of heat through horizontal movement of air or water, while convection involves the vertical movement of fluids.
Currents, tides, and waves are horizontal water movements.
Alfred Wegener named his theory of the horizontal movement of the Earth's crust "continental drift."
Percolation (vertical movement), throughflow (horizontal movement)
The sideways movement of air is called lateral movement or horizontal airflow.
As energy from waves moves through the water, the water itself also moves in a circular motion. This circular motion involves the transfer of energy through the water column, causing a vertical and horizontal movement of water particles in the direction of the wave propagation.
updraught