Wind Chill is the scale you need.
In the late 1930s a Boy Scout was invited to travel to the Antarctic with Byrd's expedition, and this person was Paul Siple.
One of the experiments he devised was to measure the rate of cooling in various wind strengths and temperatures, of water filled bottles. From such simple beginnings, Wind Chill measurement was started.
It is a thing called the Coriolis effect. The Coriolis effect is an observed reversal in spin of "things" like water, storm systems, etc. (Toilets in the Northern Hemisphere spin in the opposite direction of those in the Southern) To better understand this effect, observe global weather patterns. High and Low pressure systems in the Northern hemisphere spin Clockwise and Counterclockwise, respectively. It is the opposite in the Southern Hemisphere, because of Earth's direction of rotation. This is the Coriolis Effect.
the Coriolis force, which is produced by earth's rotation.
Because jet streams are above the friction layer, they have a negligible effect. The wind is balanced by the Coriolis effect and the pressure gradient so that the winds flow parallel to isobars.
1. Differential warming 2. Transfer of Wind Energy 3. Coriolis Effect 4. Presence of Continents
Wrapping a bottle in a wet cloth at a picnic can produce a cooler temperature due to the process of evaporative cooling. As the water in the cloth evaporates, it absorbs heat from the bottle, lowering its temperature. In contrast, a bucket of cold water may not facilitate as much heat loss from the bottle since the water does not evaporate, resulting in less effective cooling. The increased surface area of the wet cloth also enhances the cooling effect through increased evaporation.
No, the increased cooling caused by wind is not due to the Coriolis effect. The Coriolis effect is a phenomenon that describes the apparent deflection of moving objects caused by the Earth's rotation. The cooling effect of wind is mainly due to the process of convection and the transfer of heat away from a surface.
Wind Chill Factor
Wind Chill Factor
true
the Coriolis effect
Increased cooling by wind from body heat is called convective cooling. This process occurs when heat is transferred from the body to the air through convection, resulting in a cooling effect due to the movement of air.
the Coriolis effect
It's called the 'Coriolis effect'. In the northern hemisphere, they rotate clockwise. South of the equator, they rotate counter-clockwise.
yes they are =^_^=
The Coriolis effect
The Coriolis effect
Coriolis effect