By defining a relationship between angle and radius.
A protein's structure is determined by its polarity. Sub-units have polar and non-polar parts. No-polar go in the inside and polar on the outside of the protein. They are attracted to each other and this is what causes the protein's complex patterns.
The northern polar jet stream is a fast-flowing, narrow air current located in the upper troposphere. It forms at the boundary of cold polar air and warmer air masses to the south. Its path meanders due to the temperature differences, guiding weather systems and influencing patterns of high and low-pressure systems.
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The names of the climate zones are tropical, subtropical, temperate, and polar. These zones are based on factors like temperature, precipitation, and vegetation patterns.
The sun in Antarctica is the same sun that shines all over the earth. It's rise and set patterns, however, are polar, which makes those patterns different from the sunset/sunrise patterns that most humans are familiar with.
The health of men has been affected as work patterns have shifted. Physical labor has been replaced by machines and office work.
Antarctica is the continent that experiences all seven climate patterns, including polar, dry, tropical, temperate, continental, arctic, and subarctic climates.
The belt of winds that carries the polar storm track is called the polar jet stream. It is a high-altitude, fast-flowing air current that influences weather patterns in the mid-latitudes.
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The major ground-level wind patterns include trade winds, westerlies, and polar easterlies. Trade winds blow from east to west in the tropics, westerlies blow from west to east in the mid-latitudes, and polar easterlies blow from east to west near the poles. These wind patterns are influenced by the Earth's rotation and pressure systems.
The three main wind patterns in each hemisphere - trade winds, westerlies, and polar easterlies - are the result of the Earth's rotation, the distribution of temperature, and pressure differences in the atmosphere. These unique wind patterns are formed due to the Coriolis effect, which deflects winds to the right in the northern hemisphere and to the left in the southern hemisphere, creating distinct circulation systems.
It changes precipitation patterns, causes strong storms, and transfers warm and cold air.