winds that are at an upper level of land, like a large hill, or mountian
The winds above 15,000 ft. above sea level are referred to as upper level winds. The upper level winds extend upward to the outer limits of the atmosphere. Some of these winds are as high as 200 MPH.
N.E winds or S.E. winds
Monsoons are pulsating in nature while trade winds are steady winds.
The Answer is Local Winds
This means the normal direction of the wind. Here are some sentences.The prevailing winds are from the southwest.This gale is opposite of the prevailing winds.
Christopher Columbus repeatedly crossed the Atlantic Ocean by utilizing the prevailing winds.
Surface winds have to flow around such things as buildings and mountains. Upper-level winds have no 'obstructions' to alter their path.
stationary fronts
stationary
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.
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.
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.
occluded
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.
Radiosonde is the general term.
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.
There are two reasons. First, hurricanes need warm ocean water to form. The water is generally not warm enough in January to support the formation of hurricanes. Second, upper level winds are strongest in the winter. Strong upper level winds mean strong wind shear, which prevents hurricanes form organizing.