Solar radiation is redistributed around Earth through atmospheric circulation, and the direction in which Earth is spinning is counterclockwise when viewed from above the North Pole. Let's explore how these processes are interconnected:

In summary, solar radiation drives atmospheric circulation by creating temperature and pressure gradients on Earth's surface. The rotation of the Earth, with a counterclockwise spin when viewed from above the North Pole, introduces the Coriolis effect, which influences the direction of air movement and contributes to the organization of global wind patterns and circulation cells. These interconnected processes are crucial for redistributing heat and moisture around the planet, shaping weather patterns and climate.

Dr Gaurav H Tandon thank you for your contribution to the discussion

Energy radiated from Earth's surface as heat, or infrared radiation, is absorbed and re-radiated by greenhouse gases, impeding the loss of heat from our atmosphere to space. Earth's spin causes the Coriolis force which deflects the direction of air moving towards or away from the poles.Most heat is transferred in the atmosphere by radiation and convection. Sunlight absorbed by Earth's surfaces is re-radiated as heat, warming the atmosphere from the bottom up. This heat is absorbed and re-radiated by greenhouse gases in the atmosphere, resulting in the greenhouse effect. However, air moves from warm to cold regions and redistributes all of the incoming solar energy. The moving air creates the atmosphere's general circulation patterns. These general circulation patterns redistribute incoming solar radiation and they play a role in determining the climate of certain regions. Winds and ocean currents play a major role in moving the surplus heat from the equatorial regions to the Polar Regions. Without this heat transfer, the polar regions of Earth would get colder every year and regions between ~ 35 N and 35 S would get warmer every year. The difference in solar energy received at different latitudes drives atmospheric circulation. Places that get more solar energy have more heat. Places that get less solar energy have less heat. Warm air rise and cool air sinks. Warm moist air from the tropics gets fed north by the surface winds of the Ferrel cell. This then meets cool dry air moving south in the Polar cell. The polar front forms where these two contrasting air mass meet, leading to ascending air and low pressure at the surface, often around the latitude of the UK. The Earth spins on its axis from west to east. The Coriolis force, therefore, acts in a north-south direction. The Coriolis force is zero at the Equator. Though the Coriolis force is useful in mathematical equations, there is actually no physical force involved. The Earth is a sphere, and if you were floating in space above the North Pole the Earth appears to spin counterclockwise. From above the South Pole it spins clockwise. Whether it roates clockwise or counter clockwise depends on your perspective. If you are looking down on our solar system from the North Pole’s side, the planet spins on its axis in a counter-clockwise direction. If you're looking at our solar system from the other side, it rotates in a clockwise direction.