here are the dfinitions its not that hard to come up wih something.
Pressure gradient-n atmospheric sciences (meteorology, climaxtology and related fields), the pressure gradient (typically of air, more generally of any fluid) is a physical quantity that describes which direction and at what rate the pressure changes the most rapidly around a particular location. The pressure gradient is a dimensional quantity expressed in units of pressure per unit length. The SI unit ispascal per meter (Pa/m).
Isobars-A line on a map connecting points having the same atmospheric pressure at a given time or on average over a given period.
They become more tightly packed together.
the steeper the pressure gradient
On a field map, the winds are the strongest when the isobars are very close together, and the pressure gradient is high.
High pressure: The isobars will be far apart. Low pressure: The isobars will be very close together.
Closely spaced isobars indicate large pressure changes over a small area and suggest strengthening winds.Widely spaced isobars portray a "flat" or weak pressure gradient typical of light-wind situations.
Isobars show different pressure areas on a weather map.
the steeper the pressure gradient
On a weather map, the lines of equal pressure (isobars) also illustrate the pressure gradient or change of pressure per distance. The higher the pressure gradient, the higher the winds speed. Thus, when the isobars are close together, the gradient is high, and winds are higher than where the isobars are further apart. Wind can also be affected by local considerations, hills, valleys, and buildings can modify the gradient wind's direction and speed.
It means that there is a steep gradient, or pressure change, and strong winds.
Closely spaced isobars mean stronger winds, as it indicates a tight pressure gradient.
The isobars become concentric and sometimes, especially in cyclones, tightly packed with low pressure in the cyclones and high pressure in the anticyclones. In the more intense systems the isobars may be almost perfectly circular.
On a field map, the winds are the strongest when the isobars are very close together, and the pressure gradient is high.
Because jet streams are above the friction layer, they have a negligible effect. The wind is balanced by the Coriolis effect and the pressure gradient so that the winds flow parallel to isobars.
On a field map, the winds are the strongest when the isobars are very close together, and the pressure gradient is high.
False. Pressure decreases from the center to the outside.
high winds
High pressure: The isobars will be far apart. Low pressure: The isobars will be very close together.
A diagram of air pressure could be represented on a weather map. This map would use isobars - lines that connect areas with the same atmospheric pressure - to show areas of high and low pressure. The spacing of the isobars indicates the strength of the pressure gradient, which affects wind speed and direction.