AASI SNOWBOARD TECHNICAL MANUAL Physics of Snowboarding
Tis chapter introduces basic physics concepts that are central to understanding snowboarding. It illustrates and clearly explains how those general physics concepts relate directly to snowboard instruction.
Objectives
■ Describe basic physics concepts and how they apply to snowboarding. ■ Understand and explain the forces that affect the board-to-snow interaction and how a board turns.
■ Apply your knowledge of physics to better assess your students’ riding, and create a plan for changing their riding.
INTRODUCTION Te principles of physics can be found in all areas of snowboarding, and relate to the constant array of dynamic movements encountered during a lesson. People, equipment, snow conditions, and students’ desires are all subject to dramatic change. Physics, on the other hand, is fixed. Regardless of a rider’s ability, physics defines what movements can be performed on a snowboard. More importantly, physics provides insight into how to interact with these constants to be more efficient and effective. Once you appreciate what is really happening on or off the snow, you are in a position to enter into a mutually beneficial relationship with these forces.
Virtually everything done in snowboarding can be described with physics. Leonardo da Vinci said, “To understand motion is to understand nature.” Even the Greek word “physis” (physics) means “nature.” Physics not only explains motion, but can be used to describe it and help you understand motion. Sliding downhill or, more accurately, the sensations derived from gliding downhill are a large part of the thrill enjoyed by snowboarders. For these reasons and others, it is imperative to start with the following concepts, as they define the medium for enjoying riding.
SNOW
Te two main things that allow snowboarding to exist are snow (or other slippery surfaces) and a sloping topography. Snow forms when water vapor condenses in below-freezing clouds in the atmosphere. Tese condensed vapors, from either fog or water vapors, are transformed into ice crystals. Te crystals contain particles of salt, dust, or minerals that allow each of them to be able to bond – or nucleate. As they bond, they also increase in mass and begin to fall from the sky. Te same basic principles are at work with machine-made snow, except that the crystals do not fall as far from the sky so they are more consistent in size and shape.
Snow’s crystalline, frozen state is uniquely different from ice in that it has a much lower melting point. Tis low melting point, when combined with heat from the friction created by a snowboard sliding across the snow, forms a thin layer of water to slide upon.
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