occluded
Surface winds have to flow around such things as buildings and mountains. Upper-level winds have no 'obstructions' to alter their path.
Upper level winds blow along the contours of the land due to the influence of pressure gradients, Coriolis effect, and frictional forces. This creates a flow pattern that follows the shape of the landscape, leading to the characteristic meandering of upper level winds around the globe.
Upper-level winds in the middle-latitudes blow from the west due to the combination of the Coriolis effect and pressure gradients. The Coriolis effect causes winds to deflect to the right in the Northern Hemisphere, which, combined with pressure gradients created by the temperature difference between the equator and poles, results in westerly winds at the upper levels of the atmosphere.
Winds associated with a cold front are strongest just before the front passes through an area. This is due to the sharp temperature contrast between the cold air behind the front and the warmer air ahead of it, creating a steep pressure gradient that leads to strong winds.
Yes, upper level winds can create wind shear that disrupts the structure of a front, causing it to break up or weaken. This is particularly common with stationary fronts, where conflicting winds at different levels can prevent the front from maintaining its organization.
stationary
occluded
The upper level winds can cause a stationary front to break up, leading to the dispersal of clouds and an end to days of gray skies. This change in weather pattern typically results in clearer skies and improved weather conditions.
Yes, upper-level winds can disrupt and break apart weather fronts, resulting in changes in weather patterns. When a front breaks up due to these winds, it can bring an end to prolonged periods of gray skies and potentially lead to clearer conditions or a shift in weather systems.
Surface winds have to flow around such things as buildings and mountains. Upper-level winds have no 'obstructions' to alter their path.
stationary fronts
Upper level winds blow along the contours of the land due to the influence of pressure gradients, Coriolis effect, and frictional forces. This creates a flow pattern that follows the shape of the landscape, leading to the characteristic meandering of upper level winds around the globe.
The upper-level center of low pressure would be to the west of you. In the Northern Hemisphere, winds move counterclockwise around low-pressure systems, which means that the winds at the surface would be coming from the north and the upper-level center would be to the west.
Upper-level winds in the middle-latitudes blow from the west due to the combination of the Coriolis effect and pressure gradients. The Coriolis effect causes winds to deflect to the right in the Northern Hemisphere, which, combined with pressure gradients created by the temperature difference between the equator and poles, results in westerly winds at the upper levels of the atmosphere.
Cirrus clouds form by the uplift of warm, moist air along an incline of cooler air ahead of the front, for example a warm front. They are so wispy because they are actually ice crystal clouds that form at high altitudes in the upper troposphere. There are 3 types of cirrus clouds: 1. Warm Front Cirrus - Form out ahead of an approaching warm front and are blown around by upper level winds that give them their wispy appearance. 2. Anvil Cirrus - Form off of thunderstorm anvils and can signal that a thunderstorm is nearby. 3. Mares Tail Cirrus - Cirrus clouds that are blown around by upper level winds such that they look like mares tails. Hope this helps! :)
Winds associated with a cold front are strongest just before the front passes through an area. This is due to the sharp temperature contrast between the cold air behind the front and the warmer air ahead of it, creating a steep pressure gradient that leads to strong winds.