Berg winds are likely to occur during winter due to the combination of high-pressure systems and temperature inversions typical of this season. In winter, colder air settles in valleys, while warmer air aloft can create a pressure gradient that drives winds down mountain slopes. These winds warm adiabatically as they descend, leading to the characteristic dry and warm conditions associated with berg winds. Additionally, the lack of vegetation in winter can enhance the effects of these winds, making them more pronounced.
Difficult - it's only one word. But it could be used as a command on a sailing ship.
Convergence of winds at the surface and aloft is a major factor in cloud formation and cyclone development. When warm, moist air rises and cools, it condenses into clouds and releases latent heat, further intensifying the upward motion. This process, known as convergence and uplift, helps fuel the development of cyclones by creating a low-pressure system at the surface that draws in more air and moisture.
Loft, aloft, oft.
The general movement of low pressure centers across the United States is typically from west to east. This is due to the prevailing westerly winds aloft and the overall atmospheric circulation patterns in the region.
geostrophic
The winds above the equator are called "winds aloft". Below it, there are various ocean currents, but no winds.
A trough aloft is generally associated with unstable weather conditions, such as the potential for thunderstorms, heavy rain, and strong winds. This is because a trough aloft represents a region of lower pressure in the upper atmosphere, which can lead to the development of unsettled weather patterns.
Seven to eight hours depending on winds aloft.
Radiosonde is the general term.
actually,the quite says ''the winds of destiny carry you aloft to dance with the stars'' and means that you may be so lucky that you will have what you always loved, even if this is to dance with the stars
9900 and less than 5 knots.
When winds blow parallel to the isobars, this is known as geostrophic flow. Geostrophic winds occur at high altitudes where the Coriolis force balances the pressure gradient force. This results in straight, parallel wind lines with minimal curvature.
depending on the winds aloft- 8:40 to 10:00 Hrs
9900 and less than 5 knots.
R. A. Ebdon has written: 'Average temperatures, contour heights and winds at 50 millibars over the northern hemisphere' -- subject(s): Atmospheric temperature, Charts, diagrams, Winds aloft
Cold air aloft is associated with a surface low pressure system. The reverse is true for warm air aloft. In a baroclinic low pressure system, the upper-level low/trough is usually situated over the cold air, while upper level highs/ridges are around warm air aloft.