Molecule movement in the atmosphere primarily involves the processes of diffusion, convection, and turbulence. Gas molecules move randomly and spread out to fill the available space due to diffusion, while convection involves the vertical movement of air caused by temperature differences, leading to rising warm air and descending cool air. Turbulence occurs when wind flows disrupts the orderly movement of air molecules, causing chaotic and irregular patterns. Together, these movements contribute to weather patterns and the distribution of gases in the atmosphere.
The sun
Evaporation.
The earth is on a constant rotation and coincides with patterns of other stars as well as the sun and moon. Movement is natural in our atmosphere and always occurs.
The air in the Troposphere heats up as it absorbs sunlight, causing it to expand and become less dense. This leads to vertical movement of air, creating convection currents that drive weather patterns and circulation in the atmosphere.
The upward and downward movement of air in the atmosphere is called convection. Warm air rises because it is less dense, while cooler air sinks due to its higher density. This process plays a crucial role in weather patterns and the formation of clouds. Additionally, convection helps distribute heat throughout the atmosphere.
Carbon dioxide (CO2) is the molecule in which carbon is found in the Earth's atmosphere.
Carbon dioxide (CO2) is the molecule that enters a leaf from the atmosphere during photosynthesis.
Carbon dioxide (CO2) is the molecule that carries most of the carbon in the atmosphere.
Carbon is stored in the atmosphere primarily as carbon dioxide (CO2) molecule.
convection
Gas movement is greater.
actin myosin and cell movement
reabsorption
In warmer temperatures, that space can/will expand, molecule movement will increase and collisions will occur. In cooler temperatures, that space can/will decrease & molecule movement will slow down.
h2
Carbon Dioxide (two oxygen molecules and one carbon molecule)
No molecule movement at all.