A continental jet-stream travels parallel to the equator - a polar jet-stream travels in a north/south direction.
The bond would be considered polar if the electronegativity difference between the two atoms is 0.5. This is because a difference in electronegativity values between 0.5 and 1.7 indicates a polar covalent bond.
Polar covalent. There is a significant difference in electronegativity between C and F.
continental polar
The S-Cl bond is polar. The electronegativity difference between S and Cl is 0.58, which means it is polar.
The difference in electronegativity between S and N is only .5, so it's slightly polar. However, it's not very polar.
A. The subtropical jet stream lies between the westerlies and polar easterlies; this statement is true. B. The polar jet stream typically flows to the east, while the subtropical jet stream flows towards the west.
Continental polar and continental tropical are alike in that they are dry air masses. The different between the two is that the continental polar is a cool air mass while the tropical is a very hot mass of air.
The temperature difference between the polar region and the mid-latitudes is greater in winter, leading to a stronger temperature gradient. This increased temperature gradient results in a stronger polar front jet stream during the winter months.
The temperature difference between the cold polar regions and the warmer lower latitudes increases in the winter, intensifying the pressure gradient and causing the jet stream to move faster. Additionally, shorter days and longer nights in the winter result in a more pronounced temperature gradient, further accelerating the jet stream.
Continental polar and continental tropical are alike in that they are dry air masses. The different between the two is that the continental polar is a cool air mass while the tropical is a very hot mass of air.
Maritime polar air masses are characterized by cool, moist air that forms over oceans in polar regions, leading to cloudy and rainy weather. In contrast, continental tropical air masses develop over warm land areas, resulting in hot, dry conditions. The primary difference lies in their moisture content and temperature, with maritime polar being cooler and wetter, while continental tropical is warmer and drier. These distinct properties influence local weather patterns significantly.
Wind doesn't control the jet stream; this is controlled by something much more complex. It has to do with the mass balance of the atmosphere, vertically propagating waves, and the earth's rotation.
The bond would be considered polar if the electronegativity difference between the two atoms is 0.5. This is because a difference in electronegativity values between 0.5 and 1.7 indicates a polar covalent bond.
Four types of air masses that can affect the United States are continental polar (cP), maritime polar (mP), continental tropical (cT), and maritime tropical (mT). These air masses vary in temperature and moisture content, influencing the weather patterns when they move across the region.
The jet stream is typically faster in the winter due to greater temperature contrasts between polar and tropical regions. This temperature difference creates stronger winds that drive the jet stream at higher speeds during the winter months.
The Difference of CT and MTContinental Tropicalair mass is more hot and dry, and forms over water. Maritime Tropical is more warm and moist and forms over land.
The polar jet stream is generally stronger than the subtropical jet stream. The subtropical jet stream lies between the westerlies and trade winds.