Why don't winds simply flow down a pressure gradient?
The slope represents a change in velocity, or acceleration. The acceleration is the gradient (steepness) of the line. A larger gradient means faster acceleration. if the gradient points down and is negative then it represents deceleration.
because of global warming and increase of doldrums.
Wind at the surface is slower than the "winds aloft" The biggest effect is within a few inches of the ground.
Barometric pressure goes down in a tornado.
A concentration gradient is a difference in concentration across a space. It affects diffusion and osmosis because both of these passive transports move down their concentration gradients, or from an area of high concentration to low concentration.
Filtration
osmotic pressure
It may seem that winds are stronger at night, but scientifically, days tend to be windier. Nights do seem windy to us because as the world (traffic, people, television, etc) quiets down around us, we begin to hear the wind more. So why are the days windier, then? One thing that causes wind is a pressure gradient, which exists when pressure changes more in one place than in another. This happens mostly in the daytime, when the sun is out and warming different areas differently. After the sun sets, there is less of a chance of such a temperature change. ==In more detail...== In more detailed terms: as a generalization, winds tend to be weakest near dawn and strongest in late afternoon because the colder the ground is, the more of a local inversion you’re likely to have isolating surface winds from the faster winds above (conversely in the late afternoon surface heating allows for more mixing with the faster moving winds above). Winds are not caused by pressure change but by pressure gradient — that is, differences in pressure across space. So heating or cooling can cause winds, but only by changing pressure in one place more than in another, so that a gradient is formed (or strengthened). ==Other causes for wind== There are other wind-causing factors too, however, and these can hit at any time — day or night. For example, winds associated with cyclonic and related frontal circulation are independent of diurnal (daytime/nighttime) factors — you’ll feel those the strongest whenever the associated circulation feature reaches you.
Gravity will tend to pull the water down the "hill" or pile of water against the pressure gradient.
The pressure gradient decreases. The trade winds weaken, or even blow backwards.
Filtration is when fluids and solutes flow down their pressure gradient across a membrane such as in the glomerulus of the kidney.
Wind flows from areas of higher pressure to areas of lower pressure. The Coriolis effect influences wind direction by deflecting its path to the right in the Northern hemisphere and to the left in the Southern hemisphere.
the temp goes down, the winds go up, and the pressure goes up...
Do you mean "down the concentration gradient"?
If a substance moves down its concentration gradient, it means that it is moving from an area where it has a high concentration to an area where it has a low concentration. This is known as diffusion.
All small molecules can move down the concentration gradient as water O2, CO2 etc.
Down the concentration gradient