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.
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 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.
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 polar jet stream is generally stronger than the subtropical jet stream. The subtropical jet stream lies between the westerlies and trade winds.
The polar jet stream is generally stronger and faster-moving than the subtropical jet stream. The polar jet stream forms at higher latitudes and is located closer to the poles, while the subtropical jet stream is located at lower latitudes. The polar jet stream is associated with larger temperature contrasts and stronger pressure gradients, resulting in stronger winds compared to the subtropical jet stream.
the polar one is less stable than the non-polar one